Danube

{{Short description|Second-longest river in Europe}}

{{About|the river}}

{{Redirect|Istrus|the Greek figure|Istrus (mythology)|the ancient city|Histria (ancient city)}}

{{Use dmy dates|date=November 2023}}

{{Use American English|date=June 2020}}

{{Infobox river

| name = Danube

| native_name = {{native name list |tag1=de |name1=Donau |tag2=sk |name2=Dunaj |tag3=hu |name3=Duna |tag4=hr |name4=Dunav |tag5=sr-Cyrl |name5=Дунав |tag6=bg |name6=Дунав |tag7=ro |name7=Dunărea |tag8=uk |name8=Дунай}}

| image = View from Gellért Hill to the Danube, Hungary - Budapest (28493220635).jpg

| image_caption = The Danube in Budapest

| mapframe = yes

| mapframe-wikidata = yes

| mapframe-stroke-color = #4287f5

| map_caption = Course of the Danube

| subdivision_type1 = Countries

| subdivision_name1 = {{hlist|Germany|Austria|Slovakia|Hungary|Croatia|Serbia|Bulgaria|Romania|Moldova|Ukraine}}

| subdivision_type5 = Cities

| subdivision_name5 = {{hlist|Ulm|Ingolstadt|Regensburg|Passau|Linz|Vienna|Bratislava|Győr|Komárno|Budapest|Dunaújváros||Mohács|Apatin|Vukovar||Ilok|Bačka Palanka||Novi Sad||Sremski Karlovci|Belgrade|Pančevo|Smederevo|Drobeta-Turnu Severin|Vidin|Giurgiu|Ruse| Silistra|Călărași|Brăila|Galați|Reni|Izmail|Kiliia|Tulcea|Sulina}}

| length_km = 2,850

| length_ref = {{cite encyclopedia|url=https://www.britannica.com/place/Danube-River|title=Danube River|encyclopedia=Encyclopædia Britannica |edition=Online |access-date=30 April 2022}}

| width_min = Middle Danube (Iron Gates) {{cvt|150|m|abbr=on}}; Lower Danube (Brăila) {{cvt|400|m|abbr=on}}

| width_avg = Upper Danube {{cvt|300|m|abbr=on}}; Middle Danube {{cvt|400-800|m|abbr=on}}; Lower Danube {{cvt|900-1,000|m|abbr=on}}{{cite web|url=https://www.osce.org/files/f/documents/0/8/32944.pdf |title=Hydromorphological balance of the Danube River Channel on the Sector between Bazias (km 1072.2) and Danube Delta Inlet (km 80.5) |last=Bondar |first=Constantin |publisher=osce.org |access-date=30 April 2022}}{{cite web|url=http://www.icpdr.org|title=ICPDR}}

| width_max = Middle Danube {{cvt|1,500|m|abbr=on}}; Lower Danube {{cvt|1,700|m|abbr=on}}{{cite web|url=https://www.interreg.eu|title=Long-term Morphological Development of the Danube in Relation to the Sediment Balance}}

| depth_min = {{cvt|1|m|abbr=on}} (Upper Danube)

| depth_avg = Upper Danube {{cvt|8|m|abbr=on}}; Middle Danube {{cvt|6-10|m|abbr=on}}, {{cvt|53|m|abbr=on}} (Iron Gates); Lower Danube {{cvt|9|m|abbr=on}}{{cite web|url=http://www.hidmet.gov.rs|title=Republic Hydrometeorological Service of Serbia}}

| depth_max = Middle Danube (Iron Gates) {{cvt|90|m|abbr=on}}; Lower Danube {{cvt|34|m|abbr=on}}

| river_system =Danube River

| progression =Black Sea

| discharge1_location=Danube Delta

| discharge1_min = {{convert|1,790|m3/s|cuft/s|abbr=on}}{{citation|url=https://www.limnology.ro/water2012/Proceedings/001.pdf |title=The Danube River in the Pontic Sector – Hidrologycal Regime |last1=Gâştescu |first1=Petre |last2=Țuchiu |first2=Elena |work=Water resources and wetlands: Conference Proceedings |location=Tulcea, Romania |editor-first1=Petre |editor-last1=Gâştescu |editor-first2=William |editor-last2=Lewis William Jr |editor-first3=Petre |editor-last3=Breţcan |date=2012 |isbn=978-606-605-038-8 |page=18}}{{cite web|url=https://www.limnology.ro/wrw2023/proceedings.html|title=THE DANUBE RIVER AND ITS DELTA, HYDROGEOGRAPHYC CHARACTERISTICS-ACTUAL SYNTHESIS}}

| discharge1_avg =(Period: 1931–2020){{cvt|6,452|m3/s|cuft/s|abbr=on}}{{cite web|url=https://unece.org/DAM/env/documents/2019/ece/Restart/Ukraine_S1/Points_of_view_expressed_by_the_Romanian_authorutues_and_scientific_research_institute.pdf |title=Points of view expressed by the Romanian authorities and scientific research on the Ukraine's document "Annotated Report on Scientific Research – Complex Environmental Monitoring for the Danube – Black Sea Deep Water Navigation Canal operation in 2017–2018. The Sea Approach Canal Zone" |publisher=unece.org |access-date=30 April 2022}}

| discharge1_max = {{convert|15,900|m3/s|cuft/s|abbr=on}}

| discharge5_location= Passau (Bavaria, 30 km before town)

| discharge5_avg =(Period: 1931–2020){{convert|580|m3/s|cuft/s|abbr=on}}

| discharge4_location= Vienna

| discharge4_avg =(Period: 1931–2020){{convert|1,920|m3/s|cuft/s|abbr=on}}

| discharge3_location= Budapest

| discharge3_avg =(Period: 1931–2020){{convert|2,350|m3/s|cuft/s|abbr=on}}

| discharge2_location= Belgrade

| discharge2_avg =(Period: 1931–2020){{convert|5,300|m3/s|cuft/s|abbr=on}}

| source1 = Breg

| source1_location = Furtwangen im Schwarzwald, Baden-Württemberg, Germany

| source1_coordinates= {{coord|48|05|44|N|08|09|18|E|display=inline}}

| source1_elevation = {{convert|1,078|m|abbr=on}}

| source2 = Brigach

| source2_location = St. Georgen im Schwarzwald, Baden-Württemberg, Germany

| source2_coordinates= {{coord|48|06|24|N|08|16|51|E|display=inline}}

| source2_elevation = {{convert|940|m|abbr=on}}

| source_confluence_location = Donaueschingen, Baden-Württemberg, Germany

| source_confluence_coordinates= {{coord|47|57|03|N|08|31|13|E|display=inline}}

| mouth = Danube Delta

| mouth_location = Romania

| mouth_coordinates = {{coord|45|13|3|N|29|45|41|E|display=inline,title}}

| basin_size_km2 = 801,463

| basin_size_ref =

}}

{{River Danube routemap}}

The Danube ({{IPAc-en|ˈ|d|æ|n|.|j|uː|b}} {{respell|DAN|yoob}}; see also other names) is the second-longest river in Europe, after the Volga in Russia. It flows through Central and Southeastern Europe, from the Black Forest south into the Black Sea. A large and historically important river, it was once a frontier of the Roman Empire. In the 21st century, it connects ten European countries, running through their territories or marking a border. Originating in Germany, the Danube flows southeast for {{convert|2850|km|mi|sp=us|abbr=on}}, passing through or bordering Austria, Slovakia, Hungary, Croatia, Serbia, Romania, Bulgaria, Moldova, and Ukraine. Among the many cities on the river are four national capitals: Vienna, Bratislava, Budapest, and Belgrade. Its drainage basin amounts to {{Convert|817000|km2|abbr=on}} and extends into nine more countries.

The Danube's longest headstream, the Breg, rises in Furtwangen im Schwarzwald, while the river carries its name from its source confluence in the palace park in Donaueschingen onwards. Since ancient times, the Danube has been a traditional trade route in Europe. Today, {{convert|2415|km|mi|abbr=on}} of its total length are navigable. The Danube is linked to the North Sea via the Rhine–Main–Danube Canal, connecting the Danube at Kelheim with the Main at Bamberg. The river is also an important source of hydropower and drinking water.

The Danube river basin is home to such fish species as pike, zander, huchen, Wels catfish, burbot and tench. It is also home to numerous diverse carp and sturgeon, as well as salmon and trout. A few species of euryhaline fish, such as European seabass, mullet, and eel, inhabit the Danube Delta and the lower portion of the river.

Names and etymology

Today the river carries its name from its source confluence in Donaueschingen, Germany, to its discharge into the Black Sea via the Danube Delta in Romania and Ukraine.

The river was known to the ancient Greeks as the {{lang|grc-Latn|Istros}} ({{lang|grc|Ἴστρος}}){{Cite web|url=https://www.perseus.tufts.edu/hopper/text?doc=urn:cts:greekLit:tlg0016.tlg001.perseus-grc1:4.48|title=Herodotus, The Histories, book 4, chapter 48|website=www.perseus.tufts.edu}} from a root possibly also encountered in the ancient name of the Dniester ({{lang|la|Danaster}} in Latin, {{lang|grc-Latn|Tiras}} in Greek) and akin to Iranic {{lang|ira|turos}} 'swift' and Sanskrit {{lang|sa-Latn|iṣiras}} ({{lang|sa|इषिरस्}}) 'swift', from the PIE {{PIE|*isro-}}, {{PIE|*sreu}} 'to flow'.{{cite journal |title=Straturi etimologice reflectate în hidronimia românească |first1=Oliviu |last1=Felecan |first2=Nicolae |last2=Felecan |page=254 |journal=Quaderns de Filologia: Estudis Lingüístics |volume=20 |year=2015 |issue=1 |publisher=Universitat de València |doi=10.7203/qfilologia.20.7521 |url=http://roderic.uv.es/bitstream/10550/49693/1/5283423.pdf |doi-access=free }}

In the Middle Ages, the Greek {{lang|grc-Latn|Tiras}} was borrowed into Italian as {{lang|it|Tyrlo}} and into Turkic languages as {{lang|trk|Tyrla}}; the latter was further borrowed into Romanian as a regionalism ({{lang|ro|Turlă}}).

The Thraco-Phrygian name was {{lang|xpg-Latn|Matoas}},{{cite journal |title=Matoas, the Thraco-Phrygian name for the Danube, and the IE root *madų |first=Robert |last=Dyer |journal=Glotta |volume=52 |year=1974 |issue=1/2 |pages=91–95 |publisher=Vandenhoeck & Ruprecht (GmbH & Co. KG) |jstor=40266286}} "the bringer of luck".{{cite book |first=Marjeta |last=Šašel Kos |language=sl, en |url=http://iza.zrc-sazu.si/pdf/Sasel_Kos_Ukrocena_lepotica.pdf |pages=42–50 |chapter=Reka kot božanstvo — Sava v antiki |trans-chapter=River as a Deity – The Sava in Antiquity |editor-first=Jožef |editor-last=Barachini |title=Ukročena lepotica: Sava in njene zgodbe |trans-title=The Tamed Beauty: The Sava and Its Stories |isbn=978-961-92735-0-0 |year=2009 |place=Sevnica |publisher=Javni zavod za kulturo, šport, turizem in mladinske dejavnosti |archive-url=https://web.archive.org/web/20160304041135/http://iza.zrc-sazu.si/pdf/Sasel_Kos_Ukrocena_lepotica.pdf |archive-date=4 March 2016 }}

The Middle Mongolian name for the Danube was transliterated as Tho-na in 1829 by Jean-Pierre Abel-Rémusat.{{cite book |last=Abel-Rémusat |first=Jean-Pierre |author-link=Jean-Pierre Abel-Rémusat |title=Nouveaus Mélanges Asiatiques |volume=2 |location=Paris |publisher=Schubart and Heidelhoff |year=1829 |pages=96–97}}

The modern languages spoken in the Danube basin all use names derived from the Latin name {{lang|la|Danubius}}:

class="wikitable sortable" style="border-collapse: collapse;"

!style="text-align:left"|Language

!style="text-align:left"|Name

!style="text-align:left"|Pronunciation (IPA)

!style="text-align:left" data-sort-type=text|Flow sequence{{efn|Flow sequence from the source confluence in Germany to final discharge into the Black Sea via the Danube Delta in Romania and Ukraine.
See also Contents > Geography.}}

Latin

|Danubius, Dānuvius

|

|N/A

German

|Donau

|{{IPA|de|ˈdoːnaʊ|IPA|de-Donau.ogg}}

| 1 Germany
2 Austria

Bavarian

|Doana

|

|N/A

Silesian

|Dōnaj

|

|N/A

Upper Sorbian

|Dunaj

|{{IPA|hsb|ˈdunaj|IPA}}

|N/A

Czech

|Dunaj

|{{IPA|cs|ˈdunaj|IPA}}

|N/A

Slovakian

|Dunaj

|{{IPA|sk|ˈdunaj|IPA}}

| 3 Slovakia

Polish

|Dunaj

|{{IPA|pl|ˈdunaj|IPA|pl-Dunaj.ogg}}

|N/A

Hungarian

|Duna

|{{IPA|hu|ˈdunɒ|IPA|hu-Duna.ogg}}

| 4 Hungary

Slovenian

|Donava

|{{IPA|sl|ˈdóːnaʋa|IPA}}

|N/A

Serbo–Croatian

|Dunav / Дунав

|{{IPA|sh|dǔna(ː)ʋ|IPA}}

| 5 Croatia
6 Serbia

Macedonian

|Дунав

|{{IPA|sh|dǔna(ː)ʋ|IPA}}

|N/A

Romanian

|Dunăre,
definite form Dunărea

|{{IPA|ro|ˈdunəre|IPA}}, definite form {{IPA|ro|ˈdunəre̯a|IPA}}{{Cite book |last=Vékony |first=Gábor |year=2000 |title=Dacians, Romans, Romanians |publisher=Matthias Corvinus Publishing |isbn=978-1-882785-13-1 |page=[https://archive.org/details/daciansromansrom0000veko/page/210 210] |url-access=registration |url=https://archive.org/details/daciansromansrom0000veko/page/210 }}

|7 Romania
9 Moldova

Bulgarian

|Дунав (Dúnav)

|{{IPA|bg|ˈdunɐf|IPA}}

| 8 Bulgaria

Ukrainian

|Дунай (Dunáy)

|{{IPA|uk|dʊˈnɑj|IPA}}

|10 Ukraine

Greek

|Δούναβης (Doúnavis)

|{{IPA|el|ˈðunavis|IPA}}

|N/A

French

|Danube

|{{IPA|fr|da.nyb|IPA}}

|N/A

Italian

|Danubio

|{{IPA|it|daˈnuːbjo|IPA}}

|N/A

Portuguese

|Danúbio

|{{IPA|pt|dɐˈnu.βju|IPA}}

|N/A

Spanish

|Danubio

|{{IPA|es|daˈnuβjo|IPA}}

|N/A

Russian

|Дунай (Dunáy)

|{{IPA|ru|dʊˈnaj|IPA}}

|N/A

Turkish

|Tuna / طونه

|{{IPA|tr|tuˈnɐ|IPA}}

|N/A

Romansh

|Danubi

|

|N/A

Albanian

|Danub,
definite form: Danubi{{citation |page=624 |publisher=Akademia e Shkencave e RPS te Shqiperise, Instituti i Kultures Popullore, Sektori i Prozes dhe Poezise |editor1=Kozma Vasili |editor2=Arsen Mustaqi |title=Lirika popullore |trans-title=Folk lyrics |series=Folklor Shqiptar |volume=4 |language=sq |issue=3 – Kenge per nizamet dhe kurbetin |year=1981 |location=Tirana |quote=Tunë-a lumi i Danubit }}

|

|N/A

=Etymology=

Danube is an Old European river name derived from the Celtic 'Danu' or 'Don'Triad 35. Bromwich, Trioedd Ynys Prydein, pp. 280–285. (both Celtic gods), which itself derived from the Proto-Indo-European {{PIE|*deh₂nu}}. Other European river names from the same root include the Dunaj, Dzvina/Daugava, Don, Donets, Dnieper, Dniestr, Dysna and Tana/Deatnu. In Rigvedic Sanskrit, danu (दनु) means "fluid, dewdrop" and danuja (दनु-ज) means "born from danu" or "born from dew-drops". In Avestan, the same word means "river". The Finnish word for Danube is {{wikt-lang|fi|Tonava}}, which is most likely derived from the name of the river in German, {{lang|de|Donau}}. Its Sámi name {{lang|smi|Deatnu}} means "Great River". It is possible that {{lang|xsc|dānu}} in Scythian as in Avestan was a generic word for "river": Dnieper and Dniestr, from Danapris and Danastius, are presumed to continue Scythian {{lang|xsc|*dānu apara}} "far river" and {{lang|xsc|*dānu nazdya-}} "near river", respectively.{{cite book |author-link1=J. P. Mallory |last1=Mallory |first1=J.P |author-link2=Victor H. Mair |first2=Victor H. |last2=Mair |title=The Tarim Mummies: Ancient China and the Mystery of the Earliest Peoples from the West |url=https://archive.org/details/tarimmummiesanci00mall |url-access=registration |location=London |publisher=Thames and Hudson |year=2000 |page=[https://archive.org/details/tarimmummiesanci00mall/page/106 106] |isbn=978-0-500-05101-6 }}. {{cite book |url=http://i.ironau.ru/pdf/osjazfolk1949.pdf |author=V. I. Adaev |script-title=ru:Осетинский язык и фольклор |trans-title=Ossetian language and folklore |location=Moscow |publisher=Publishing house of Soviet Academy of Sciences |year=1949 |page=236 |language=ru }}

In Latin, the Danube was variously known as {{lang|la|Danubius}}, {{lang|la|Danuvius}}, {{lang|la|Ister}}{{cite book|title=Ancient Languages of the Balkans, Part One|location=Paris|publisher=Mouton|year=1976|page=144}} or Hister. The Latin name is masculine, as are all its Slavic names, except Slovene (the name of the Rhine is also masculine in Latin, most of the Slavic languages, as well as in German). The German {{lang|de|Donau}} (Early Modern German {{lang|de|Donaw}}, {{lang|de|Tonaw}},{{lang|de|Tonaw}} in {{cite book|author=Sebastian Franck |title=Weltbuch |year=1542 |url=https://books.google.com/books?id=dk9QLBxWmxcC&q=tonach&pg=PT167 |page=81 |author-link=Sebastian Franck}} {{lang|de|Donaw}} e.g. in {{cite book |author=Leonhard Thurneisser zum Thurn |title=Pison |year=1572 |url=https://books.google.com/books?id=PWhWAAAAcAAJ&pg=PR186|page=186}} Spelling {{lang|de|Donau}} from the 17th century. Middle High German {{lang|gmh|Tuonowe}}){{cite book|author=Grimm|title=Deutsche Grammatik|page=[https://archive.org/details/bub_gb_VXTJ_C205t4C/page/n426 407]|title-link=Deutsche Grammatik}} is feminine, as it has been re-interpreted as containing the suffix -ouwe "wetland".

Romanian differs from other surrounding languages in designating the river with a feminine term, {{lang|ro|Dunărea}} ({{IPA|ro|ˈdunəre̯a|IPA}}). This form was not inherited from Latin, although Romanian is a Romance language. To explain the loss of the Latin name, scholars who suppose that Romanian developed near the large river propose that the Romanian name descends from a hypothetical Thracian {{lang|txh|*Donaris}}. The Proto-Indo-European root of this presumed name is related to the Iranic word "{{lang|ira|don-}}"/"{{lang|ira|dan-}}", while the supposed suffix {{lang|ira|-aris}} is encountered in the ancient name of the Ialomița River, Naparis, and in the unidentified Miliare river mentioned by Jordanes in his Getica. Gábor Vékony says that this hypothesis is not plausible, because the Greeks borrowed the Istros form from the native Thracians. He proposes that the Romanian name is a loanword from a Turkic language (Cuman or Pecheneg).

Geography

File:Danube basin.png]]

File:Bregquelle 01.jpg at St. Martin's Chapel in Furtwangen im Schwarzwald: the Bregquelle, the source of the Danube's longest headstream, the Breg, where the Danube is symbolized by the Roman allegory for the river, Danuvius.]]

File:Donauquelle Donaueschingen im Sommer.jpg: the source of the Donaubach (Danube Brook), which flows into the Brigach.]]

Classified as an international waterway, it originates in the town of Donaueschingen, in the Black Forest of Germany, at the confluence of the rivers Brigach and Breg. The Danube then flows southeast for about {{cvt|2730|km}}, passing through four capital cities (Vienna, Bratislava, Budapest, and Belgrade) before emptying into the Black Sea via the Danube Delta in Romania and Ukraine.

=International status=

Once a long-standing frontier of the Roman Empire, the river passes through or touches the borders of 10 countries. Its drainage basin extends into nine more (ten if Kosovo is included).{{cite web|url=http://www.icpdr.org/icpdr-pages/countries.htm|title=Countries of the Danube River Basin|publisher=International Commission for the protection of the Danube River|access-date=13 November 2010}}

class="wikitable sortable" style="border-collapse: collapse;

!style="text-align:left"|Flow
seq.

!style="text-align:left"|Country

!style="text-align:left"|Basin
area

!style="text-align:left"|Local
name

!style="text-align:left"|Points of interest

style="text-align:center"|1

|Germany

|style="text-align:right"|7.0%

|Donau

|Donaueschingen – source

style="text-align:center"|2

|Austria

|style="text-align:right"|10.0%

|Donau

|Vienna – capital

style="text-align:center"|3

|Slovakia

|style="text-align:right"|5.9%

|Dunaj

|Bratislava – capital

style="text-align:center"|4

|Hungary

|style="text-align:right"|11.6%

|Duna

|Budapest – capital

style="text-align:center"|5

|Croatia

|style="text-align:right"|4.4%

|Dunav

|

style="text-align:center"|6

|Serbia

|style="text-align:right"|10.2%

|Dunav

|Belgrade – capital

style="text-align:center"|7

|Romania

|style="text-align:right"|29.0%

|Dunărea

|Danube DeltaBlack Sea

style="text-align:center"|8

|Bulgaria{{efn|name="sequence_8"|Note that the port city of Vidin in Bulgaria is downstream from the town of Moldova Nouă in Romania.}}

|style="text-align:right"|5.9%

|Dunav

|

style="text-align:center"|9

|Moldova

|style="text-align:right"|1.6%

|Dunărea

|

style="text-align:center"|10

|Ukraine

|style="text-align:right"|3.8%

|Дунай

|Danube DeltaBlack Sea

=Drainage basin=

In addition to the bordering countries (see above), the drainage basin includes parts of nine more countries: Bosnia and Herzegovina (4.6% of the basin area), the Czech Republic (2.9%), Slovenia (2.0%), Montenegro (0.9%), Switzerland (0.2%), Italy (<0.15%), Poland (<0.1%), North Macedonia (<0.1%) and Albania (<0.1%). The total drainage basin is {{convert|801463|km2|abbr=on}} in area,{{GeoQuelle|DE-BY|GV}}{{GeoSource|Danube||12}} and is home to 83 million people. The highest point of the drainage basin is the summit of Piz Bernina at the Italy–Switzerland border, at {{convert|4049|m|sp=us|abbr=on}}.{{cite book|url=http://www.unece.org/fileadmin//DAM/env/water/publications/pub76.htm|title=Our Waters: Joining Hands Across Borders. First Assessment of Transboundary Rivers, Lakes and Groundwaters|year=2007|chapter=Drainage basin of the Black Sea |chapter-url=http://www.unece.org/fileadmin/DAM/env/water/blanks/assessment/black.pdf|publisher=United Nations Economic Commission for Europe}} The Danube River Basin is divided into three main parts, separated by "gates" where the river is forced to cut through mountainous sections:{{Cite web|url=https://www.icpdr.org/main/danube-basin/river-basin|title=River Basin | ICPDR – International Commission for the Protection of the Danube River|website=www.icpdr.org}}

=Discharge=

Mean annual discharge on the hydrological stations (period from 2000 to 2024);{{cite web|url=https://www.hidmet.gov.rs|title=Republički hidrometeorološki zavod}}{{cite web|url=https://www.icpdr.org/library/publications?f%5B0%5D=category%3A233|title=ICPDR-International Commission for the Protection of the Danube River}}{{cite web|url=https://www.hidro.ro/bulletin_type/diagnoza-si-prognoza-pentru-dunare|title=DIAGNOZA ŞI PROGNOZA PENTRU DUNĂRE}}

class="wikitable" style="text-align:center;"

! rowspan="2" |Year

! colspan="7" |Mean annual discharge in m3/s (cu ft/s)

Reni
Isaccea

!Silistra

!Pristol

!Batina
Bezdan

!Nagymaros Szob

!Bratislava
Wolfsthal

!Untergries-bach

2000

|{{convert|6,580.6|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|6,198.1|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,585.9|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,669.4|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,627.2|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,337.9|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,667.2|m3/s|cuft/s|sortable=on|abbr=values}}

2001

|{{convert|6,304.3|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,919.4|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,421.8|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,432.5|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,382.3|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,231.3|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,627.6|m3/s|cuft/s|sortable=on|abbr=values}}

2002

|{{convert|6,837.1|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|6,100.1|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,392|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,824.9|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,855.6|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,683|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,803.9|m3/s|cuft/s|sortable=on|abbr=values}}

2003

|{{convert|5,021|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|4,571|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|3,825|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,786|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,722|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,647|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,153|m3/s|cuft/s|sortable=on|abbr=values}}

2004

|{{convert|6,524|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|6,088|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,233|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,025|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,013|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,852|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,213|m3/s|cuft/s|sortable=on|abbr=values}}

2005

|{{convert|8,711|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|7,659|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|6,396|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,420|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,329|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,115|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,359|m3/s|cuft/s|sortable=on|abbr=values}}

2006

|{{convert|8,428|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|7,370|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|6,616|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,110|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,503|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,186|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,396|m3/s|cuft/s|sortable=on|abbr=values}}

2007

|{{convert|5,626|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,195|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|4,512|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,182|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,136|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,916|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,287|m3/s|cuft/s|sortable=on|abbr=values}}

2008

|{{convert|5,909|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,358|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|4,736|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,163|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,079|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,876|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,339|m3/s|cuft/s|sortable=on|abbr=values}}

2009

|{{convert|6,492|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,990|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,412|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,607|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,441|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,186|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,433|m3/s|cuft/s|sortable=on|abbr=values}}

2010

|{{convert|9,598|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|8,515|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|7,424|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,879|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,615|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,130|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,420|m3/s|cuft/s|sortable=on|abbr=values}}

2011

|{{convert|5,303|m3/s|cuft/s|sortable=on|abbr=values}}

|

|

|{{convert|2,000|m3/s|cuft/s|sortable=on|abbr=values}}

|

|

|

2012

|{{convert|5,053|m3/s|cuft/s|sortable=on|abbr=values}}

|

|

|{{convert|2,240|m3/s|cuft/s|sortable=on|abbr=values}}

|

|

|

2013

|{{convert|7,164|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|6,558|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,946|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,863|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,684|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,417|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,671|m3/s|cuft/s|sortable=on|abbr=values}}

2014

|{{convert|7,446|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|6,901|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,756|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,198|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,036|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,788|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,237|m3/s|cuft/s|sortable=on|abbr=values}}

2015

|{{convert|6,138|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,722|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|4,971|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,030|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,903|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,629|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,240|m3/s|cuft/s|sortable=on|abbr=values}}

2016

|{{convert|6,465|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,993|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,339|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,261|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,196|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,944|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,412|m3/s|cuft/s|sortable=on|abbr=values}}

2017

|{{convert|5,202|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|4,813|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|4,270|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,143|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,041|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,844|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,307|m3/s|cuft/s|sortable=on|abbr=values}}

2018

|{{convert|6,487.8|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,875.5|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|4,891|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,906.3|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,808.1|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,644.1|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,227.8|m3/s|cuft/s|sortable=on|abbr=values}}

2019

|{{convert|5,579|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,168|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|4,593|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,253|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,114|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,962|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,446|m3/s|cuft/s|sortable=on|abbr=values}}

2020

|{{convert|4,893.5|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|4,659|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|4,095|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,215|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,026|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,841|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,285|m3/s|cuft/s|sortable=on|abbr=values}}

2021

|{{convert|5,998|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|5,505|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|4,696|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,178|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|2,028|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,838|m3/s|cuft/s|sortable=on|abbr=values}}

|{{convert|1,304|m3/s|cuft/s|sortable=on|abbr=values}}

2022

|{{convert|5,753|m3/s|cuft/s|sortable=on|abbr=values}}

|

|

|{{convert|2,180|m3/s|cuft/s|sortable=on|abbr=values}}

|

|

|

2023

|{{convert|6,623.8|m3/s|cuft/s|sortable=on|abbr=values}}

|

|

|{{convert|2,240|m3/s|cuft/s|sortable=on|abbr=values}}

|

|

|

2024

|{{convert|5,776.4|m3/s|cuft/s|sortable=on|abbr=values}}

|

|

|

|

|

|

Multiannual average, minimum and maximum discharge (water period from 1876 to 2010){{cite book|title=Flood Regime of Rivers in the Danube River Basin|year=2019 |doi=10.31577/2019.9788089139460 |last1=Pekárová |first1=Pavla |last2=Miklánek |first2=Pavol |isbn=978-80-89139-46-0 |s2cid=131234947 }}

class="wikitable" style="text-align:center;"

! rowspan="2" |Station

! colspan="3" |Discharge (m3/s)

! colspan="3" |Discharge (cu ft/s)

Min

!Mean

!Max

!Min

!Mean

!Max

Ceatal Izmail

|1,889

|6,489

|14,673

|{{convert|1,889|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|6,489|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|14,673|m3/s|cuft/s|sortable=on|disp=number}}

Reni, Isaccea

|1,805

|6,564

|14,820

|{{convert|1,805|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|6,564|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|14,820|m3/s|cuft/s|sortable=on|disp=number}}

Zimnicea, Svishtov

|1,411

|6,018

|14,510

|{{convert|1,411|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|6,018|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|14,510|m3/s|cuft/s|sortable=on|disp=number}}

Orșova

|1,672

|5,572

|13,324

|{{convert|1,672|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|5,572|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|13,324|m3/s|cuft/s|sortable=on|disp=number}}

Veliko Gradište

|1,461

|5,550

|14,152

|{{convert|1,461|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|5,550|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|14,152|m3/s|cuft/s|sortable=on|disp=number}}

Pančevo

|1,454

|5,310

|13,080

|{{convert|1,454|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|5,310|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|13,080|m3/s|cuft/s|sortable=on|disp=number}}

Bogojevo

|959

|2,889

|8,153

|{{convert|959|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|2,889|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|8,153|m3/s|cuft/s|sortable=on|disp=number}}

Bezdan, Batina

|749

|2,353

|7,043

|{{convert|749|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|2,353|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|7,043|m3/s|cuft/s|sortable=on|disp=number}}

Mohács

|667

|2,336

|7,227

|{{convert|667|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|2,336|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|7,227|m3/s|cuft/s|sortable=on|disp=number}}

Nagymaros, Szob

|628

|2,333

|7,057

|{{convert|628|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|2,333|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|7,057|m3/s|cuft/s|sortable=on|disp=number}}

Bratislava

|633

|2,059

|7,324

|{{convert|633|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|2,059|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|7,324|m3/s|cuft/s|sortable=on|disp=number}}

Vienna

|506

|1,917

|6,062

|{{convert|506|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|1,917|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|6,062|m3/s|cuft/s|sortable=on|disp=number}}

Krems an der Donau

|596

|1,845

|5,986

|{{convert|596|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|1,845|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|5,986|m3/s|cuft/s|sortable=on|disp=number}}

Linz

|468

|1,451

|4,783

|{{convert|468|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|1,451|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|4,783|m3/s|cuft/s|sortable=on|disp=number}}

Hofkirchen

|211

|638

|1,943

|{{convert|211|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|638|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|1,943|m3/s|cuft/s|sortable=on|disp=number}}

Regensburg

|128

|444

|1,330

|{{convert|128|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|444|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|1,330|m3/s|cuft/s|sortable=on|disp=number}}

Ingolstadt

|83

|312

|965

|{{convert|83|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|312|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|965|m3/s|cuft/s|sortable=on|disp=number}}

Ulm

|6

|38

|153

|{{convert|6|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|38|m3/s|cuft/s|sortable=on|disp=number}}

|{{convert|153|m3/s|cuft/s|sortable=on|disp=number}}

Simulated water and suspended sediment results from climate-driven decadal study (with STD through specific decade):{{cite journal|title=Simulating fluvial fluxes in the Danube watershed: The "Little Ice Age" versus modern day|date=2021|doi=10.1177/0959683611409778 |last1=McCarney-Castle |first1=K. |last2=Voulgaris |first2=G. |last3=Kettner |first3=A.J. |last4=Giosan |first4=L. |journal=The Holocene |volume=22 |pages=91–105 |s2cid=129864432 }}

P – Simulated average precipitation in the Danube basin; T – Simulated average temperature in the Danube basin; Q – Simulated average discharge in the Danube River at delta; S – Simulated sediment load in the Danube River at delta;

class="wikitable" style="text-align:center;"

!rowspan=2|Period (CE)

!rowspan=2|Scenario

!colspan=2|P

!colspan=2|T

!colspan=2|Q

!colspan=2|S

mm

!in

!°C

!°F

!m3/s

!cu ft/s

!metric tons
(millions)

!short tons
(millions)

colspan="10" |LIA
1530–1540

|Cool/dry

|{{convert|794|mm|in|disp=table|sortable=on}}

|{{convert|9.0|C|F|disp=table|sortable=on}}

|{{convert|6,207|m3/s|cuft/s|disp=table|sortable=on}}

|{{convert|72.9|t|ST|disp=table|sortable=on}}

1650–1660

|Cool/wet

|{{convert|885|mm|in|disp=table|sortable=on}}

|{{convert|8.4|C|F|disp=table|sortable=on}}

|{{convert|7,929|m3/s|cuft/s|disp=table|sortable=on}}

|{{convert|67.3|t|ST|disp=table|sortable=on}}

1709–1719

|Warm/wet

|{{convert|861|mm|in|disp=table|sortable=on}}

|{{convert|8.3|C|F|disp=table|sortable=on}}

|{{convert|7,616|m3/s|cuft/s|disp=table|sortable=on}}

|{{convert|52.9|t|ST|disp=table|sortable=on}}

1770–1780

|Warm/dry

|{{convert|865|mm|in|disp=table|sortable=on}}

|{{convert|8.9|C|F|disp=table|sortable=on}}

|{{convert|7,728|m3/s|cuft/s|disp=table|sortable=on}}

|{{convert|74.1|t|ST|disp=table|sortable=on}}

colspan="10" |Modern
1940–1950

|Cool/dry

|{{convert|778|mm|in|disp=table|sortable=on}}

|{{convert|8.9|C|F|disp=table|sortable=on}}

|{{convert|7,209|m3/s|cuft/s|disp=table|sortable=on}}

|{{convert|55.0|t|ST|disp=table|sortable=on}}

1960–1970

|Cool/wet

|{{convert|850|mm|in|disp=table|sortable=on}}

|{{convert|8.8|C|F|disp=table|sortable=on}}

|{{convert|7,399|m3/s|cuft/s|disp=table|sortable=on}}

|{{convert|73.0|t|ST|disp=table|sortable=on}}

1975–1985

|Warm/wet

|{{convert|818|mm|in|disp=table|sortable=on}}

|{{convert|9.0|C|F|disp=table|sortable=on}}

|{{convert|7,186|m3/s|cuft/s|disp=table|sortable=on}}

|{{convert|77.8|t|ST|disp=table|sortable=on}}

1990–2000

|Warm/dry

|{{convert|790|mm|in|disp=table|sortable=on}}

|{{convert|9.5|C|F|disp=table|sortable=on}}

|{{convert|5,068|m3/s|cuft/s|disp=table|sortable=on}}

|{{convert|73.8|t|ST|disp=table|sortable=on}}

Discharge chronology

Historical average flow to the present day; Measured and reconstructed average water flows from 1742.

The reconstructed and observed streamflow (Q – m3/s) at Ceatal Izmail for the 1742 to 2022:{{cite journal|title=The first tree-ring reconstruction of streamflow variability over the last ~250 years in the Lower Danube|last1=Nagaviciuc|first1=Viorica|last2=Roibu|first2=Cătălin-Constantin|last3=Mursa|first3=Andrei|last4=Ştirbu|first4=Marian-Ionuţ|last5=Popa|first5=Ionel|last6=Ionita|first6=Monica|year=2023|doi=10.1016/j.jhydrol.2023.129150 |s2cid=256288140 |journal=Journal of Hydrology|doi-access=free}}{{cite web|url=https://www.hidro.ro|title=INHGA |url-status=live |archive-url=https://web.archive.org/web/20231216143728/https://www.hidro.ro/ |archive-date= Dec 16, 2023 }}{{cite web|url=https://www.icpdr.org/main/publications/annual-reports|title=Annual Reports |website=ICPDR |archive-url=https://web.archive.org/web/20230418005823/https://www.icpdr.org/main/publications/annual-reports |archive-date= Apr 18, 2023 }}{{cite web|url=https://www.ipcc.ch|title=IPCC |url-status=live |archive-url=https://web.archive.org/web/20231221145430/https://www.ipcc.ch/ |archive-date= Dec 21, 2023 }}

class="wikitable" style="text-align:center;"

!Year

!m3/s

!cu ft/s

!Year

!m3/s

!cu ft/s

!Year

!m3/s

!cu ft/s

!Year

!m3/s

!cu ft/s

!Year

!m3/s

!cu ft/s

!Year

!m3/s

!cu ft/s

colspan="18" |Reconstructed
1742

|{{convert|5,780|m3/s|cuft/s|disp=table}}

|1751

|{{convert|6,760|m3/s|cuft/s|disp=table}}

|1761

|{{convert|6,470|m3/s|cuft/s|disp=table}}

|1771

|{{convert|9,700|m3/s|cuft/s|disp=table}}

|1781

|{{convert|5,830|m3/s|cuft/s|disp=table}}

|1791

|{{convert|5,540|m3/s|cuft/s|disp=table}}

1743

|{{convert|5,355|m3/s|cuft/s|disp=table}}

|1752

|{{convert|7,090|m3/s|cuft/s|disp=table}}

|1762

|{{convert|6,510|m3/s|cuft/s|disp=table}}

|1772

|{{convert|6,050|m3/s|cuft/s|disp=table}}

|1782

|{{convert|6,470|m3/s|cuft/s|disp=table}}

|1792

|{{convert|6,930|m3/s|cuft/s|disp=table}}

1744

|{{convert|5,370|m3/s|cuft/s|disp=table}}

|1753

|{{convert|4,980|m3/s|cuft/s|disp=table}}

|1763

|{{convert|5,950|m3/s|cuft/s|disp=table}}

|1773

|{{convert|4,600|m3/s|cuft/s|disp=table}}

|1783

|{{convert|7,930|m3/s|cuft/s|disp=table}}

|1793

|{{convert|7,800|m3/s|cuft/s|disp=table}}

1745

|{{convert|4,940|m3/s|cuft/s|disp=table}}

|1754

|{{convert|6,330|m3/s|cuft/s|disp=table}}

|1764

|{{convert|6,280|m3/s|cuft/s|disp=table}}

|1774

|{{convert|6,150|m3/s|cuft/s|disp=table}}

|1784

|{{convert|8,400|m3/s|cuft/s|disp=table}}

|1794

|{{convert|5,230|m3/s|cuft/s|disp=table}}

1746

|{{convert|7,140|m3/s|cuft/s|disp=table}}

|1755

|{{convert|6,840|m3/s|cuft/s|disp=table}}

|1765

|{{convert|6,130|m3/s|cuft/s|disp=table}}

|1775

|{{convert|6,060|m3/s|cuft/s|disp=table}}

|1785

|{{convert|7,610|m3/s|cuft/s|disp=table}}

|1795

|{{convert|6,530|m3/s|cuft/s|disp=table}}

1747

|{{convert|5,850|m3/s|cuft/s|disp=table}}

|1756

|{{convert|6,370|m3/s|cuft/s|disp=table}}

|1766

|{{convert|8,530|m3/s|cuft/s|disp=table}}

|1776

|{{convert|6,320|m3/s|cuft/s|disp=table}}

|1786

|{{convert|6,570|m3/s|cuft/s|disp=table}}

|1796

|{{convert|6,460|m3/s|cuft/s|disp=table}}

1748

|{{convert|6,840|m3/s|cuft/s|disp=table}}

|1757

|{{convert|6,830|m3/s|cuft/s|disp=table}}

|1767

|{{convert|6,850|m3/s|cuft/s|disp=table}}

|1777

|{{convert|5,530|m3/s|cuft/s|disp=table}}

|1787

|{{convert|6,980|m3/s|cuft/s|disp=table}}

|1797

|{{convert|6,700|m3/s|cuft/s|disp=table}}

1749

|{{convert|6,690|m3/s|cuft/s|disp=table}}

|1758

|{{convert|8,410|m3/s|cuft/s|disp=table}}

|1768

|{{convert|8,400|m3/s|cuft/s|disp=table}}

|1778

|{{convert|7,470|m3/s|cuft/s|disp=table}}

|1788

|{{convert|5,860|m3/s|cuft/s|disp=table}}

|1798

|{{convert|6,560|m3/s|cuft/s|disp=table}}

1750

|{{convert|5,180|m3/s|cuft/s|disp=table}}

|1759

|{{convert|5,520|m3/s|cuft/s|disp=table}}

|1769

|{{convert|5,720|m3/s|cuft/s|disp=table}}

|1779

|{{convert|6,600|m3/s|cuft/s|disp=table}}

|1789

|{{convert|7,190|m3/s|cuft/s|disp=table}}

|1799

|{{convert|9,590|m3/s|cuft/s|disp=table}}

colspan="3" |

|1760

|{{convert|6,840|m3/s|cuft/s|disp=table}}

|1770

|{{convert|10,700|m3/s|cuft/s|disp=table}}

|1780

|{{convert|6,990|m3/s|cuft/s|disp=table}}

|1790

|{{convert|6,940|m3/s|cuft/s|disp=table}}

|1800

|{{convert|6,150|m3/s|cuft/s|disp=table}}

colspan="3" |{{convert|5,905|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,597|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|7,154|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,547|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,978|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,749|m3/s|cuft/s|abbr=values}}

1801

|{{convert|7,310|m3/s|cuft/s|disp=table}}

|1811

|{{convert|8,220|m3/s|cuft/s|disp=table}}

|1821

|{{convert|6,390|m3/s|cuft/s|disp=table}}

|1831

|{{convert|6,670|m3/s|cuft/s|disp=table}}

|1841

|{{convert|6,210|m3/s|cuft/s|disp=table}}

|1851

|{{convert|7,350|m3/s|cuft/s|disp=table}}

1802

|{{convert|6,590|m3/s|cuft/s|disp=table}}

|1812

|{{convert|5,230|m3/s|cuft/s|disp=table}}

|1822

|{{convert|5,700|m3/s|cuft/s|disp=table}}

|1832

|{{convert|4,820|m3/s|cuft/s|disp=table}}

|1842

|{{convert|5,340|m3/s|cuft/s|disp=table}}

|1852

|{{convert|6,550|m3/s|cuft/s|disp=table}}

1803

|{{convert|6,870|m3/s|cuft/s|disp=table}}

|1813

|{{convert|6,680|m3/s|cuft/s|disp=table}}

|1823

|{{convert|6,520|m3/s|cuft/s|disp=table}}

|1833

|{{convert|5,350|m3/s|cuft/s|disp=table}}

|1843

|{{convert|6,710|m3/s|cuft/s|disp=table}}

|1853

|{{convert|7,800|m3/s|cuft/s|disp=table}}

1804

|{{convert|6,220|m3/s|cuft/s|disp=table}}

|1814

|{{convert|7,290|m3/s|cuft/s|disp=table}}

|1824

|{{convert|6,420|m3/s|cuft/s|disp=table}}

|1834

|{{convert|6,470|m3/s|cuft/s|disp=table}}

|1844

|{{convert|6,960|m3/s|cuft/s|disp=table}}

|1854

|{{convert|5,060|m3/s|cuft/s|disp=table}}

1805

|{{convert|7,010|m3/s|cuft/s|disp=table}}

|1815

|{{convert|6,640|m3/s|cuft/s|disp=table}}

|1825

|{{convert|8,040|m3/s|cuft/s|disp=table}}

|1835

|{{convert|7,040|m3/s|cuft/s|disp=table}}

|1845

|{{convert|7,440|m3/s|cuft/s|disp=table}}

|1855

|{{convert|7,020|m3/s|cuft/s|disp=table}}

1806

|{{convert|6,830|m3/s|cuft/s|disp=table}}

|1816

|{{convert|8,090|m3/s|cuft/s|disp=table}}

|1826

|{{convert|5,800|m3/s|cuft/s|disp=table}}

|1836

|{{convert|9,740|m3/s|cuft/s|disp=table}}

|1846

|{{convert|6,750|m3/s|cuft/s|disp=table}}

|1856

|{{convert|5,390|m3/s|cuft/s|disp=table}}

1807

|{{convert|7,000|m3/s|cuft/s|disp=table}}

|1817

|{{convert|8,650|m3/s|cuft/s|disp=table}}

|1827

|{{convert|6,650|m3/s|cuft/s|disp=table}}

|1837

|{{convert|6,770|m3/s|cuft/s|disp=table}}

|1847

|{{convert|7,070|m3/s|cuft/s|disp=table}}

|1857

|{{convert|4,880|m3/s|cuft/s|disp=table}}

1808

|{{convert|5,600|m3/s|cuft/s|disp=table}}

|1818

|{{convert|6,920|m3/s|cuft/s|disp=table}}

|1828

|{{convert|8,140|m3/s|cuft/s|disp=table}}

|1838

|{{convert|10,440|m3/s|cuft/s|disp=table}}

|1848

|{{convert|5,620|m3/s|cuft/s|disp=table}}

|1858

|{{convert|5,580|m3/s|cuft/s|disp=table}}

1809

|{{convert|7,150|m3/s|cuft/s|disp=table}}

|1819

|{{convert|6,470|m3/s|cuft/s|disp=table}}

|1829

|{{convert|8,280|m3/s|cuft/s|disp=table}}

|1839

|{{convert|9,960|m3/s|cuft/s|disp=table}}

|1849

|{{convert|5,360|m3/s|cuft/s|disp=table}}

|1859

|{{convert|5,630|m3/s|cuft/s|disp=table}}

1810

|{{convert|8,430|m3/s|cuft/s|disp=table}}

|1820

|{{convert|6,560|m3/s|cuft/s|disp=table}}

|1830

|{{convert|7,790|m3/s|cuft/s|disp=table}}

|1840

|{{convert|5,560|m3/s|cuft/s|disp=table}}

|1850

|{{convert|7,360|m3/s|cuft/s|disp=table}}

|1860

|{{convert|7,220|m3/s|cuft/s|disp=table}}

colspan="3" |{{convert|6,901|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|7,075|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,973|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|7,282|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,482|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,248|m3/s|cuft/s|abbr=values}}

1861

|{{convert|5,980|m3/s|cuft/s|disp=table}}

|1871

|{{convert|8,860|m3/s|cuft/s|disp=table}}

|1881

|{{convert|8,320|m3/s|cuft/s|disp=table}}

|1891

|{{convert|5,440|m3/s|cuft/s|disp=table}}

|1901

|{{convert|5,570|m3/s|cuft/s|disp=table}}

|1911

|{{convert|5,120|m3/s|cuft/s|disp=table}}

1862

|{{convert|5,040|m3/s|cuft/s|disp=table}}

|1872

|{{convert|5,970|m3/s|cuft/s|disp=table}}

|1882

|{{convert|5,130|m3/s|cuft/s|disp=table}}

|1892

|{{convert|5,620|m3/s|cuft/s|disp=table}}

|1902

|{{convert|5,650|m3/s|cuft/s|disp=table}}

|1912

|{{convert|6,940|m3/s|cuft/s|disp=table}}

1863

|{{convert|3,340|m3/s|cuft/s|disp=table}}

|1873

|{{convert|5,150|m3/s|cuft/s|disp=table}}

|1883

|{{convert|7,590|m3/s|cuft/s|disp=table}}

|1893

|{{convert|5,710|m3/s|cuft/s|disp=table}}

|1903

|{{convert|5,490|m3/s|cuft/s|disp=table}}

|1913

|{{convert|6,410|m3/s|cuft/s|disp=table}}

1864

|{{convert|6,150|m3/s|cuft/s|disp=table}}

|1874

|{{convert|4,680|m3/s|cuft/s|disp=table}}

|1884

|{{convert|5,250|m3/s|cuft/s|disp=table}}

|1894

|{{convert|4,770|m3/s|cuft/s|disp=table}}

|1904

|{{convert|4,940|m3/s|cuft/s|disp=table}}

|1914

|{{convert|6,560|m3/s|cuft/s|disp=table}}

1865

|{{convert|5,690|m3/s|cuft/s|disp=table}}

|1875

|{{convert|5,360|m3/s|cuft/s|disp=table}}

|1885

|{{convert|5,430|m3/s|cuft/s|disp=table}}

|1895

|{{convert|6,240|m3/s|cuft/s|disp=table}}

|1905

|{{convert|6,100|m3/s|cuft/s|disp=table}}

|1915

|{{convert|9,540|m3/s|cuft/s|disp=table}}

1866

|{{convert|3,780|m3/s|cuft/s|disp=table}}

|1876

|{{convert|7,520|m3/s|cuft/s|disp=table}}

|1886

|{{convert|5,660|m3/s|cuft/s|disp=table}}

|1896

|{{convert|6,470|m3/s|cuft/s|disp=table}}

|1906

|{{convert|6,190|m3/s|cuft/s|disp=table}}

|1916

|{{convert|7,550|m3/s|cuft/s|disp=table}}

1867

|{{convert|6,350|m3/s|cuft/s|disp=table}}

|1877

|{{convert|6,660|m3/s|cuft/s|disp=table}}

|1887

|{{convert|5,340|m3/s|cuft/s|disp=table}}

|1897

|{{convert|7,700|m3/s|cuft/s|disp=table}}

|1907

|{{convert|6,770|m3/s|cuft/s|disp=table}}

|1917

|{{convert|6,410|m3/s|cuft/s|disp=table}}

1868

|{{convert|5,660|m3/s|cuft/s|disp=table}}

|1878

|{{convert|7,040|m3/s|cuft/s|disp=table}}

|1888

|{{convert|6,800|m3/s|cuft/s|disp=table}}

|1898

|{{convert|4,550|m3/s|cuft/s|disp=table}}

|1908

|{{convert|4,400|m3/s|cuft/s|disp=table}}

|1918

|{{convert|4,300|m3/s|cuft/s|disp=table}}

1869

|{{convert|5,370|m3/s|cuft/s|disp=table}}

|1879

|{{convert|8,300|m3/s|cuft/s|disp=table}}

|1889

|{{convert|6,530|m3/s|cuft/s|disp=table}}

|1899

|{{convert|4,500|m3/s|cuft/s|disp=table}}

|1909

|{{convert|5,590|m3/s|cuft/s|disp=table}}

|1919

|{{convert|7,410|m3/s|cuft/s|disp=table}}

1870

|{{convert|7,470|m3/s|cuft/s|disp=table}}

|1880

|{{convert|5,660|m3/s|cuft/s|disp=table}}

|1890

|{{convert|4,650|m3/s|cuft/s|disp=table}}

|1900

|{{convert|6,900|m3/s|cuft/s|disp=table}}

|1910

|{{convert|7,450|m3/s|cuft/s|disp=table}}

|1920

|{{convert|6,720|m3/s|cuft/s|disp=table}}

colspan="3" |{{convert|5,483|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,520|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,070|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|5,790|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|5,815|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,770|m3/s|cuft/s|abbr=values}}

colspan="18" |Observed
1921

|{{convert|3,906|m3/s|cuft/s|disp=table}}

|1931

|{{convert|6,706|m3/s|cuft/s|disp=table}}

|1941

|{{convert|9,916|m3/s|cuft/s|disp=table}}

|1951

|{{convert|6,368|m3/s|cuft/s|disp=table}}

|1961

|{{convert|5,860|m3/s|cuft/s|disp=table}}

|1971

|{{convert|5,272|m3/s|cuft/s|disp=table}}

1922

|{{convert|6,530|m3/s|cuft/s|disp=table}}

|1932

|{{convert|6,181|m3/s|cuft/s|disp=table}}

|1942

|{{convert|7,266|m3/s|cuft/s|disp=table}}

|1952

|{{convert|5,850|m3/s|cuft/s|disp=table}}

|1962

|{{convert|6,628|m3/s|cuft/s|disp=table}}

|1972

|{{convert|6,160|m3/s|cuft/s|disp=table}}

1923

|{{convert|6,430|m3/s|cuft/s|disp=table}}

|1933

|{{convert|6,344|m3/s|cuft/s|disp=table}}

|1943

|{{convert|4,308|m3/s|cuft/s|disp=table}}

|1953

|{{convert|6,117|m3/s|cuft/s|disp=table}}

|1963

|{{convert|6,047|m3/s|cuft/s|disp=table}}

|1973

|{{convert|5,766|m3/s|cuft/s|disp=table}}

1924

|{{convert|6,700|m3/s|cuft/s|disp=table}}

|1934

|{{convert|5,644|m3/s|cuft/s|disp=table}}

|1944

|{{convert|7,190|m3/s|cuft/s|disp=table}}

|1954

|{{convert|6,168|m3/s|cuft/s|disp=table}}

|1964

|{{convert|5,259|m3/s|cuft/s|disp=table}}

|1974

|{{convert|7,258|m3/s|cuft/s|disp=table}}

1925

|{{convert|5,255|m3/s|cuft/s|disp=table}}

|1935

|{{convert|5,718|m3/s|cuft/s|disp=table}}

|1945

|{{convert|5,870|m3/s|cuft/s|disp=table}}

|1955

|{{convert|8,834|m3/s|cuft/s|disp=table}}

|1965

|{{convert|8,400|m3/s|cuft/s|disp=table}}

|1975

|{{convert|7,190|m3/s|cuft/s|disp=table}}

1926

|{{convert|8,144|m3/s|cuft/s|disp=table}}

|1936

|{{convert|6,392|m3/s|cuft/s|disp=table}}

|1946

|{{convert|4,684|m3/s|cuft/s|disp=table}}

|1956

|{{convert|7,100|m3/s|cuft/s|disp=table}}

|1966

|{{convert|7,954|m3/s|cuft/s|disp=table}}

|1976

|{{convert|6,567|m3/s|cuft/s|disp=table}}

1927

|{{convert|5,990|m3/s|cuft/s|disp=table}}

|1937

|{{convert|8,325|m3/s|cuft/s|disp=table}}

|1947

|{{convert|5,418|m3/s|cuft/s|disp=table}}

|1957

|{{convert|6,254|m3/s|cuft/s|disp=table}}

|1967

|{{convert|7,500|m3/s|cuft/s|disp=table}}

|1977

|{{convert|7,073|m3/s|cuft/s|disp=table}}

1928

|{{convert|5,005|m3/s|cuft/s|disp=table}}

|1938

|{{convert|6,867|m3/s|cuft/s|disp=table}}

|1948

|{{convert|6,357|m3/s|cuft/s|disp=table}}

|1958

|{{convert|6,340|m3/s|cuft/s|disp=table}}

|1968

|{{convert|5,660|m3/s|cuft/s|disp=table}}

|1978

|{{convert|7,120|m3/s|cuft/s|disp=table}}

1929

|{{convert|5,330|m3/s|cuft/s|disp=table}}

|1939

|{{convert|6,310|m3/s|cuft/s|disp=table}}

|1949

|{{convert|4,301|m3/s|cuft/s|disp=table}}

|1959

|{{convert|5,375|m3/s|cuft/s|disp=table}}

|1969

|{{convert|7,710|m3/s|cuft/s|disp=table}}

|1979

|{{convert|7,747|m3/s|cuft/s|disp=table}}

1930

|{{convert|5,197|m3/s|cuft/s|disp=table}}

|1940

|{{convert|9,533|m3/s|cuft/s|disp=table}}

|1950

|{{convert|5,130|m3/s|cuft/s|disp=table}}

|1960

|{{convert|6,514|m3/s|cuft/s|disp=table}}

|1970

|{{convert|9,602|m3/s|cuft/s|disp=table}}

|1980

|{{convert|8,767|m3/s|cuft/s|disp=table}}

colspan="3" |{{convert|5,888|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,802|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,044|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,492|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|7,062|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,892|m3/s|cuft/s|abbr=values}}

1981

|{{convert|8,172|m3/s|cuft/s|disp=table}}

|1991

|{{convert|6,274|m3/s|cuft/s|disp=table}}

|2001

|{{convert|6,304.3|m3/s|cuft/s|disp=table}}

|2011

|{{convert|5,303|m3/s|cuft/s|disp=table}}

|2021

|{{convert|6,018|m3/s|cuft/s|disp=table}}

| colspan="3" rowspan="11" |

1982

|{{convert|6,700|m3/s|cuft/s|disp=table}}

|1992

|{{convert|5,710.8|m3/s|cuft/s|disp=table}}

|2002

|{{convert|6,837.1|m3/s|cuft/s|disp=table}}

|2012

|{{convert|5,053|m3/s|cuft/s|disp=table}}

|2022

|{{convert|5,753|m3/s|cuft/s|disp=table}}

1983

|{{convert|5,543|m3/s|cuft/s|disp=table}}

|1993

|{{convert|4,873|m3/s|cuft/s|disp=table}}

|2003

|{{convert|5,021|m3/s|cuft/s|disp=table}}

|2013

|{{convert|7,164|m3/s|cuft/s|disp=table}}

|2023

|{{convert|6,623.8|m3/s|cuft/s|disp=table}}

1984

|{{convert|6,325|m3/s|cuft/s|disp=table}}

|1994

|{{convert|6,031.8|m3/s|cuft/s|disp=table}}

|2004

|{{convert|6,524|m3/s|cuft/s|disp=table}}

|2014

|{{convert|7,446|m3/s|cuft/s|disp=table}}

|2024

|

1985

|{{convert|6,449|m3/s|cuft/s|disp=table}}

|1995

|{{convert|6,223.7|m3/s|cuft/s|disp=table}}

|2005

|{{convert|8,711|m3/s|cuft/s|disp=table}}

|2015

|{{convert|6,138|m3/s|cuft/s|disp=table}}

|2025

|

1986

|{{convert|6,257|m3/s|cuft/s|disp=table}}

|1996

|{{convert|7,035.8|m3/s|cuft/s|disp=table}}

|2006

|{{convert|8,428|m3/s|cuft/s|disp=table}}

|2016

|{{convert|6,465|m3/s|cuft/s|disp=table}}

|2026

|

1987

|{{convert|6,619|m3/s|cuft/s|disp=table}}

|1997

|{{convert|6,684.2|m3/s|cuft/s|disp=table}}

|2007

|{{convert|5,626|m3/s|cuft/s|disp=table}}

|2017

|{{convert|5,202|m3/s|cuft/s|disp=table}}

|2027

|

1988

|{{convert|6,383|m3/s|cuft/s|disp=table}}

|1998

|{{convert|6,804.6|m3/s|cuft/s|disp=table}}

|2008

|{{convert|5,909|m3/s|cuft/s|disp=table}}

|2018

|{{convert|6,487.8|m3/s|cuft/s|disp=table}}

|2028

|

1989

|{{convert|5,448|m3/s|cuft/s|disp=table}}

|1999

|{{convert|7,951.5|m3/s|cuft/s|disp=table}}

|2009

|{{convert|6,492|m3/s|cuft/s|disp=table}}

|2019

|{{convert|5,579|m3/s|cuft/s|disp=table}}

|2029

|

1990

|{{convert|4,194|m3/s|cuft/s|disp=table}}

|2000

|{{convert|6,580.6|m3/s|cuft/s|disp=table}}

|2010

|{{convert|9,598|m3/s|cuft/s|disp=table}}

|2020

|{{convert|4,893.5|m3/s|cuft/s|disp=table}}

|2030

|

colspan="3" |{{convert|6,209|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,417|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,945|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|5,973|m3/s|cuft/s|abbr=values}}

| colspan="3" |{{convert|6,131.6|m3/s|cuft/s|abbr=values}}

colspan="18" |Multiannual average discharge 1742 to 2022: ~ {{convert|6,500|m3/s|cuft/s|abbr=on}}

Tributaries

File:Szeged-tisza3.jpg is the longest tributary of the Danube.]]

{{Main|List of tributaries of the Danube}}

The land drained by the Danube extends into many other countries. Many Danubian tributaries are important rivers in their own right, navigable by barges and other shallow-draught boats. From its source to its outlet into the Black Sea, its main tributaries are (as they enter):

style="width:590px;"
style="width:45%;"|

  1. Iller (entering at Ulm)
  2. Lech
  3. Altmühl (entering at Kelheim)
  4. Naab (entering at Regensburg)
  5. Regen (entering at Regensburg)
  6. Isar
  7. Inn (entering at Passau)
  8. Ilz (entering at Passau)
  9. Enns
  10. Morava (entering near Devín Castle)
  11. Rába (entering at Győr)
  12. Váh (entering at Komárno)
  13. Hron (entering at Štúrovo)
  14. Ipeľ
  15. Sió
  16. Drava (entering near Osijek)
  17. Vuka (entering at Vukovar)

| style="width:45%;"|

18. Tisza (entering near Titel)

19. Sava (entering at Belgrade)

20. Timiș (river) (entering at Pančevo)

21. Great Morava (entering near Smederevo)

22. Mlava (entering near Kostolac)

23. Karaš (entering near Banatska Palanka)

24. Jiu (entering at Bechet)

25. Iskar (entering near Gigen)

26. Olt (entering at Turnu Măgurele)

27. Osam (entering near Nikopol, Bulgaria)

28. Yantra (entering near Svishtov)

29. Argeș (entering at Oltenița)

30. Ialomița

31. Siret (entering near Galați)

32. Prut (entering near Galați)

File:Donaueschingen Donauzusammenfluss 20080714.jpg|The Danube's source confluence in Donaueschingen: the Donauzusammenfluss, the confluence of Breg and Brigach.

File:Дунайський біосферний заповідник 2.JPG|0 km, Danube Delta, Ukraine

File:Danube Delta ESA23450088.jpeg|Where the Danube meets the Black Sea (European Space Agency Sentinel-2 image)

File:The Danube Spills into the Black Sea.jpg|The Danube discharges into the Black Sea (the upper body of water in the image).

Cities and towns

File:Aerial image of Passau.jpg, Danube, and Ilz in Passau]]

{{Main|List of cities and towns on the Danube river}}

The Danube flows through many cities, including four national capitals (shown below in bold), more than any other river in the world. Ordered from the source to the mouth they are:

File:Linz Ars electronica center lila DL.jpg, Austria]]

File:Danube Bratislava 6.jpg, Slovakia]]

File:Várhegy2.JPG, Hungary]]

File:Petrovaradinska tvrđava, 12.jpg overlooking the Danube and Novi Sad, regional capital of Vojvodina in Serbia]]

File:Kalemegdanska_terasa_Apr_2011.jpg into the Danube beneath Fortress in Belgrade, capital of Serbia]]

File:Nikopol-danube.jpg in winter]]

File:Cazaresulinaoras2.jpg, Romania]]

{{wide image|Panorama of Danube in Vienna.jpg|1000px|Panorama of the Danube in Vienna}}

{{wide image|DonauknieVisegrad_2.jpg|1000px|The Danube Bend is a curve of the Danube in Hungary, near the city of Visegrád. The Transdanubian Mountains lie on the right bank (left side of the picture), while the North Hungarian Mountains on the left bank (right side of the picture).}}

{{wide image|Budapest view with Parliament.jpg|1000px|Panorama of the Danube in Budapest with the Hungarian Parliament (left)}}

{{wide image|Budapest from Gellert Hill MC.jpg|1000px|Budapest at night}}

{{wide image|Novi Sad - Gigapixelna panorama2.jpg|1000px|Panorama of the Danube in Novi Sad from Petrovaradin Fortress, Serbia}}

{{wide image|The confluence of the Sava into the Danube at Belgrade.jpg|900px|The confluence of the Sava into the Danube at Belgrade. Pictured from Belgrade Fortress, Serbia}}

{{Wide image|Belgrade Panorama.jpg|1000px|Panoramic image of the Danube and Sava river from Kalemegdan, Belgrade Serbia}}

{{wide image|Pano-Donau-Danube.jpg|1000px|The Danube entering the Iron Gate at the South-Western end of the Carpathian Mountains. Romania on the left side, Golubac Fortress and Serbia on the right side.}}

Islands

{{Further|List of islands in the Danube}}

File:Budapest by air.jpg, Budapest, Hungary. There are 15 bridges over the Danube in Budapest.]]

File:Belgrade_Aerial_K1.jpg in Belgrade, Serbia. It is located at the confluence of the Sava and Danube.]]

File:Ada Kaleh.jpg island in the Danube was forgotten during the peace talks at the Congress of Berlin in 1878, which allowed it to remain a de jure Turkish territory and the Ottoman Sultan Abdul Hamid II's private possession until the Treaty of Lausanne in 1923 (de facto until Romania unilaterally declared its sovereignty on the island in 1919 and further strengthened it with the Treaty of Trianon in 1920).{{Citation|date=24 July 1923|title=Treaty of Peace with Turkey signed at Lausanne|place=Lausanne, Switzerland|access-date=6 December 2014|url=http://wwi.lib.byu.edu/index.php/Treaty_of_Lausanne |publisher=World War I Document Archive }}{{cite web|url=http://alexisphoenix.org/adakaleh.php|title=Ada Kaleh|website=The Alexis Project |first1=Dorel |last1=Bondoc |access-date=6 December 2014|archive-date=25 July 2011|archive-url=https://web.archive.org/web/20110725000112/http://alexisphoenix.org/adakaleh.php}} The island was submerged during the construction of the Iron Gates hydroelectric plant in 1970.]]

==Sectioning==

  • Upper Section: From spring to Devín Gate, at the border of Austria and Slovakia. Danube remains a characteristic mountain river until Passau, with average bottom gradient 0.12% (1200 ppm), from Passau to Devín Gate the gradient lessens to 0.06% (600 ppm).
  • Middle Section: From Devín Gate to Iron Gate, at the border of Serbia and Romania. The riverbed widens and the average bottom gradient becomes only 0.006% (60 ppm).
  • Lower Section: From Iron Gate to Sulina, with average gradient as little as 0.003% (30 ppm).

Modern navigation

{{expand section|how the "Iron Gate" relates to ship navigation?|date=November 2022}}

File:Parliament Budapest Hungary.jpg]]

File:DanubedeltaSulinaarm2.jpg]]

File:Freight-ship-danube-320x240.ogg]]

The Danube is navigable by ocean ships from the Black Sea to Brăila in Romania (the maritime river sector), and further on by river ships to Kelheim, Bavaria, Germany; smaller craft can navigate further upstream to Ulm, Württemberg, Germany. About 60 of its tributaries are also navigable.

Since the completion of the German Rhine–Main–Danube Canal in 1992, the river has been part of a trans-European waterway from Rotterdam on the North Sea to Sulina on the Black Sea, a distance of {{convert|3500|km|sp=us|abbr=on}}. In 1994 the Danube was declared one of ten Pan-European transport corridors, routes in Central and Eastern Europe that required major investment over the following ten to fifteen years.{{citation needed|date=November 2022}} The amount of goods transported on the Danube increased to about 100 million tons in 1987. In 1999, transport on the river was made difficult by the NATO bombing of three bridges in Serbia during the Kosovo War. Clearance of the resulting debris was completed in 2002, and a temporary pontoon bridge that hampered navigation was removed in 2005.{{citation needed|date=November 2022}}

At the Iron Gate, the Danube flows through a gorge that forms part of the boundary between Serbia and Romania; it contains the Iron Gate I Hydroelectric Power Station dam, followed at about {{convert|60|km|sp=us|abbr=on}} downstream (outside the gorge) by the Iron Gate II Hydroelectric Power Station. On 13 April 2006, a record peak discharge at Iron Gate Dam reached {{convert|15400|m3/s|sp=us|abbr=on}}.

There are three artificial waterways built on the Danube: the Danube-Tisa-Danube Canal (DTD) in the Banat and Bačka regions (Vojvodina, northern province of Serbia); the {{convert|64|km|sp=us|abbr=on}} Danube-Black Sea Canal, between Cernavodă and Constanța (Romania) finished in 1984, shortens the distance to the Black Sea by {{convert|400|km|sp=us|abbr=on}}; the Rhine–Main–Danube Canal is about {{convert|171|km|sp=us|abbr=on}}, finished in 1992, linking the North Sea to the Black Sea.{{Cite web|url=http://ines-danube.info/goto.php?target=file_1442_download&client_id=viailias4|title=Danube navigation at a glance |website=INeS Danube |archive-url=https://web.archive.org/web/20210226160839/http://ines-danube.info/goto.php?target=file_1442_download&client_id=viailias4 |archive-date= Feb 26, 2021 }} A Danube-Aegean canal has been proposed.{{Cite web |last=Tzimas |first=Stavros |title=Chinese interests could make plan to link Danube and Aegean a reality |url=https://www.ekathimerini.com/economy/221159/chinese-interests-could-make-plan-to-link-danube-and-aegean-a-reality/ |access-date=11 July 2022 |website=eKathimerini.com |date=Aug 28, 2017 |language=English}}

Cruising on the Danube is a popular sightseeing activity, especially between Passau, Germany, to Budapest, Hungary.{{Cite web |last=Sarna |first=Heidi |date=August 15, 2019 |title=10 Best River Cruises |url=https://www.frommers.com/slideshows/818945-10-best-river-cruises |url-status=live |archive-url=https://web.archive.org/web/20230921093944/https://www.frommers.com/slideshows/818945-10-best-river-cruises |archive-date=Sep 21, 2023 |website=Frommer's}}

Piracy

In 2010–12, shipping companies, especially from Ukraine, claimed that their vessels suffered from "regular pirate attacks" on the Serbian and the Romanian stretches of the Danube.{{cite web|url=http://www.jutarnji.hr/rijecni-gusari-u-srbiji-pljackaju-hrvatske-brodove--zadnja-zrtva-brod--quot-sloga-quot--sisackog--quot-dunavskog-lloyda-quot-/980402/|title=Riječni gusari u Srbiji pljačkaju hrvatske brodove|language=hr|first=Mate|last=Piškor|date=12 October 2011 |website=Jutarnji list |archive-url=https://web.archive.org/web/20200301213528/https://www.jutarnji.hr/vijesti/crna-kronika/rijecni-gusari-u-srbiji-pljackaju-hrvatske-brodove-sa-sloge-ukrali-opremu-vrijednu-60-tisuca-eura/1724961/ |archive-date= Mar 1, 2020 }}{{cite web |url=http://un.ua/eng/article/369989.html |title=Ukrainian Danube Shipping Company Says Its Ships Are Being Attacked Frequently in Romanian Part Of River Danube |publisher=Ukrainian News |date=January 13, 2012 |access-date=11 June 2012 |archive-url=https://web.archive.org/web/20120114032713/http://un.ua/eng/article/369989.html |archive-date=14 January 2012 }}{{cite web|url=https://gazeta.ua/articles/np/_ukrajinski-korabli-vse-chastishe-stayut-zhertvami-rumunskih-pirativ/419063|title=Українські кораблі все частіше стають жертвами румунських піратів|website=Gazeta.ua|trans-title=Romanian Pirates Attack Ukrainian Ships More Frequently|language=uk|date=20 January 2012|first=Олена|last=Гордієва |url-status=live |archive-url=https://web.archive.org/web/20230405202115/https://gazeta.ua/articles/np/_ukrayinski-korabli-vse-chastishe-stayut-zhertvami-rumunskih-pirativ/419063 |archive-date= Apr 5, 2023 }} However, the transgressions may not be considered acts of piracy, as defined according to the United Nations Convention on the Law of the Sea, but rather instances of "river robbery".{{cite web |url=http://www.rivercruiseinfo.com/content/pirates-lower-danube |title=Pirates on the lower Danube |archive-url=https://web.archive.org/web/20131214175158/http://www.rivercruiseinfo.com/content/pirates-lower-danube |archive-date=14 December 2013 |website=rivercruiseinfo |author=Ingo_Eigen |date=Feb 27, 2012 }}

On the other hand, media reports say the crews on transport ships often steal and sell their own cargo and then blame the plundering on "pirates", and the alleged attacks are not piracy but small-time contraband theft along the river.{{Cite news |last=Tomiuc |first=Eugen |date=2012-02-05 |title=Reports Of 'Pirates Of The Danube' Get The Old Heave-Ho |language=en |work=Radio Free Europe/Radio Liberty |url=https://www.rferl.org/a/romania_danube_river_pirates_ukraine/24474067.html |url-status=live |archive-url= https://web.archive.org/web/20230909064917/https://www.rferl.org/a/romania_danube_river_pirates_ukraine/24474067.html |archive-date= Sep 9, 2023 }}

Danube Delta

{{Main|Danube Delta}}

File:Вилково, Дунайские плавни 1962 г.JPG in the Danube Delta]]

The Danube Delta ({{langx|ro|Delta Dunării}} {{IPA|ro|ˈdelta ˈdunərij|pron}}; {{langx|uk|Дельта Дунаю|translit=Del'ta Dunayu}}) is the largest river delta in the European Union. The greater part of the Danube Delta lies in Romania (Tulcea county), while its northern part, on the left bank of the Chilia arm, is situated in Ukraine (Odesa Oblast). The approximate surface is {{convert|4152|km2|sp=us|abbr=on}}, of which {{convert|3446|km2|sp=us|abbr=on}} are in Romania. If one includes the lagoons of Razim-Sinoe ({{convert|1015|km2|sp=us|abbr=on}} of which {{convert|865|km2|sp=us|abbr=on}} water surface), which are located south of the delta proper, but are related to it geologically and ecologically (their combined territory is part of the World Heritage Site), the total area of the Danube Delta reaches {{convert|5165|km2|sp=us|abbr=on}}.

The Danube Delta is also the best-preserved river delta in Europe, a UNESCO World Heritage Site (since 1991) and a Ramsar Site. Its lakes and marshes support 45 freshwater fish species. Its wetlands support vast flocks of migratory birds of over 300 species, including the endangered pygmy cormorant (Phalacrocorax pygmaeus). These are threatened by rival canalization and drainage schemes such as the Bystroye Canal.{{cite book|url=https://www.unece.org/fileadmin/DAM/env/eia/documents/inquiry/Rom.1.pdf|title=Documentation on the likely significant transboundary impact of the Ukrainian deep-water navigation canal Danube-black sea in the context of Espoo Convention, 1991|year=2005|author=Staras, Mircea|publisher=Danube Delta National Institute|publication-date=February 2005|location=Tulcea, Romania|archive-date=3 August 2020|archive-url=https://web.archive.org/web/20200803080734/https://www.unece.org/fileadmin/DAM/env/eia/documents/inquiry/Rom.1.pdf|access-date=20 September 2020|url-status=live}}

International cooperation

=Ecology and environment=

{{Main|International Commission for the Protection of the Danube River}}

File:Pelicani din Delta Dunarii.PNG in the Danube Delta, Romania]]

The International Commission for the Protection of the Danube River (ICPDR) is an organization that consists of 14 member states (Germany, Austria, the Czech Republic, Slovakia, Slovenia, Hungary, Croatia, Bosnia and Herzegovina, Serbia, Bulgaria, Romania, Moldova, Montenegro, and Ukraine) and the European Union. The commission, established in 1998, deals with the whole Danube river basin, which includes tributaries and groundwater resources. Its goal is to implement the Danube River Protection Convention by promoting and coordinating sustainable and equitable water management, including conservation, improvement, and rational use of waters and the implementation of the EU Water Framework Directive and the Danube Strategy.

=Navigation=

{{Main|Danube Commission}}

The Danube Commission is concerned with the maintenance and improvement of the river's navigation conditions. It was established in 1948 by seven countries bordering the river. Members include representatives from Austria, Bulgaria, Croatia, Germany, Hungary, Moldova, Slovakia, Romania, Russia, Ukraine, and Serbia; it meets regularly twice a year. It also convenes groups of experts to consider items provided for in the commission's working plans.

The commission dates to the Paris Conferences of 1856 and 1921, which established for the first time an international regime to safeguard free navigation on the Danube. Today the Commission include riparian and non-riparian states.

Geology

File:Evening at Danube gorge.jpg, Serbia-Romania border]]

File:Dam Serbia Djerdap 2.jpg, Romania-Serbia]]

Although the headwaters of the Danube are relatively small today, geologically, the Danube is much older than the Rhine, with which its catchment area competes in today's southern Germany. This has a few interesting geological complications. Since the Rhine flows north towards the North Sea, a continental divide beginning at Piz Lunghin divides large parts of southern Germany, which is sometimes referred to as the European Watershed.

Before the last ice age in the Pleistocene, the Rhine started at the southwestern tip of the Black Forest, while the waters from the Alps that today feed the Rhine were carried east by the so-called Urdonau (original Danube). Parts of this ancient river's bed, which was much larger than today's Danube, can still be seen in (now waterless) canyons in today's landscape of the Swabian Alb. The erosion of the Upper Rhine valley led to stream capture; waters from the Alps changed their direction and began feeding the Rhine. Today's upper Danube is thus an underfit stream.

File:Danube Iron Gorge La Cazane.JPG, on the Serbian-Romanian border (Iron Gates natural park and Đerdap national park)]]

Since the Swabian Alb is largely shaped of porous limestone, and since the Rhine's level is much lower than the Danube's, today subsurface rivers carry much water from the Danube to the Rhine. On many days in the summer, when the Danube carries little water, it completely sinks into these underground channels at two locations in the Swabian Alb, which are referred to as the Donauversickerung (Danube Sink). Most of this water resurfaces only {{convert|12|km|mi|sp=us|abbr=on}} south at the Aachtopf, Germany's wellspring with the highest flow, an average of {{convert|8500|L/s|cuft/s|sp=us|abbr=on}}, north of Lake Constance—thus feeding the Rhine. The European Water Divide applies only for those waters that pass beyond this point, which only occurs during the days of the year when the Danube carries enough water to survive the sinkholes in the Donauversickerung.

Since such large volumes of underground water erode much of the surrounding limestone, it is predicted that the Danube upper course will one day disappear entirely in favor of the Rhine, an event called stream capturing.

The hydrological parameters of Danube are regularly monitored in Croatia at Batina, Dalj, Vukovar and Ilok.{{cite web | url = http://hidro.hr/hidro_e.php?id=hidro¶m=Podaci_e | title = Daily hydrological report | publisher = State Hydrometeorological Bureau of the Republic of Croatia | access-date = 9 September 2010 | archive-date = 30 May 2010 | archive-url = https://web.archive.org/web/20100530062812/http://hidro.hr/hidro_e.php?id=hidro¶m=Podaci_e }}

History

File:Guerre d'orient, combat sur le Danube.jpg (1853–1856)]]

The Danube basin was the site of some of the earliest human cultures. The Danubian Neolithic cultures include the Linear Pottery cultures of the mid-Danube basin. Many sites of the sixth-to-third millennium BCE Vinča culture (Vinča, Serbia), are sited along the Danube. The third millennium BCE Vučedol culture (from the Vučedol site near Vukovar, Croatia) is famous for its ceramics.

Darius the Great, king of Persia, crossed the river in the late 6th century BCE to invade European Scythia and to subdue the Scythians.

Alexander the Great defeated the Triballian king Syrmus and the northern barbarian Thracian and Illyrian tribes by advancing from Macedonia as far as the Danube in 336 BCE.

Under the Romans, the Danube formed the border of the Empire with the tribes to the north almost from its source to its mouth. At the same time, it was a route for the transport of troops and the supply of settlements downstream. From 37 CE to the reign of the Emperor Valentinian I (364–375) the Danubian Limes was the northeastern border of the Empire, with occasional interruptions such as the fall of the Danubian Limes in 259. The crossing of the Danube into Dacia was achieved by the Imperium Romanum, first in two battles in 102 and then in 106 after the construction of a bridge in 101 near the garrison town of Drobeta at the Iron Gate. This victory over Dacia under Decebalus enabled the Province of Dacia to be created, but in 271 it was abandoned by emperor Aurelian.

Avars used the river as their southeastern border in the 6th century.

File:Trajan's Bridge Across the Danube, Modern Reconstruction.jpg|The oldest bridge across the Danube, constructed by Apollodorus of Damascus between 103 and 105 CE, directed by Trajan, modern Serbia and Romania

File:Mária Valéria´s bridge.jpg|At Esztergom and Štúrovo, the Danube separates Hungary from Slovakia.

File:Vena 06.jpg|The Danube in Vienna

File:Danube at belene.jpg|The Danube between Belene and Belene Island, Bulgaria

File:Frozen Danube Reichsbrücke.JPG|A look upstream from the Donauinsel in Vienna, Austria during an unusually cold winter (February 2006). A frozen Danube usually occurs just once or twice in a lifetime.

File:Bratislavaminorflood.jpg|Bratislava does not usually suffer major floods, but the Danube sometimes overflows its right bank.

=Ancient cultural perspectives of the lower Danube=

Part of the rivers Danubius or Istros was also known as (together with the Black Sea) the Okeanos in ancient times, being called the Okeanos Potamos (Okeanos River). The lower Danube was also called the Keras Okeanoio (Gulf or Horn of Okeanos) in the Argonautica by Apollonius Rhodos (Argon. IV. 282).

At the end of the Okeanos Potamos, is the holy island of Alba (Leuke, Pytho Nisi, Isle of Snakes), sacred to the Pelasgian (and later, Greek) Apollo, greeting the sun rising in the east. Hecateus Abderitas refers to Apollo's island from the region of the Hyperboreans, in the Okeanos. It was on Leuke, in one version of his legend, that the hero Achilles was buried (to this day, one of the mouths of the Danube is called Chilia). Old Romanian folk songs recount a white monastery on a white island with nine priests.[http://www.pelasgians.org/ Dacia Preistorica] {{Webarchive|url=https://web.archive.org/web/20080707015920/http://www.pelasgians.org/ |date=7 July 2008 }}, Nicolae Densusianu (1913).

=Rivalry along the Danube=

{{Unreferenced section|date=February 2013}}

File:Reprise Buda 1686.jpg took Ottoman-held Buda after a long siege in 1686.]]

Between the late 14th and late 19th centuries, the Ottoman Empire competed first with the Kingdom of Serbia, Second Bulgarian Empire, Kingdom of Hungary, Principality of Wallachia, Principality of Moldavia and later with the Habsburg monarchy, Polish–Lithuanian Commonwealth, and Russian Empire for controlling the Danube (طونه,Tuna in Turkish), which became the northern border of the Ottoman Empire for centuries. Many of the Ottoman–Hungarian Wars (1366–1526) and Ottoman–Habsburg wars (1526–1791) were fought along the river.

The most important wars of the Ottoman Empire along the Danube include the Battle of Nicopolis (1396), the Siege of Belgrade (1456), the Battle of Mohács (1526), the first Turkish Siege of Vienna (1529), the Siege of Esztergom (1543), the Long War (1591–1606), the Battle of Vienna (1683), the Great Turkish War (1683–1699), the Crimean War (1853–1856) and the Russo-Turkish War (1877–1878).

=Second World War=

During the 2011 renovation of the Margaret Bridge, Budapest, human remains were discovered. The mostly Jewish remains were victims of the far-right Arrow Cross Party, who briefly governed Hungary from 1944.{{cite news |agency=The Associated Press|title=Hungary buries remains of Holocaust victims executed by Nazis on banks of the Danube River |url=https://nationalpost.com/news/world/hungary-buries-remains-of-holocaust-victims-executed-by-nazis-on-banks-of-the-danube-river |website=National Post |access-date=16 February 2022 |language=en |date=15 April 2016}}

Economics

=Drinking water=

Along its course, the Danube is a source of drinking water for about 20 million people.{{Cite web |title=About Us |url=https://www.icpdr.org/main/icpdr/about-us |access-date=5 February 2021 |website=International Commission for the Protection of the Danube River}}{{Cite web|last=|first=|date=|title=Blue River|url=https://wwf.panda.org/discover/knowledge_hub/where_we_work/black_sea_basin/danube_carpathian/our_solutions/freshwater/danube_river_basin/?|url-status=live|archive-url=https://web.archive.org/web/20210412152545/https://wwf.panda.org/discover/knowledge_hub/where_we_work/black_sea_basin/danube_carpathian/our_solutions/freshwater/danube_river_basin/? |archive-date=12 April 2021 |access-date=5 February 2021|website=wwf.panda.org}} In Baden-Württemberg, Germany, almost 30 percent (as of 2004) of the water for the area between Stuttgart, Bad Mergentheim, Aalen and Alb-Donau (district) comes from purified water of the Danube. Other cities such as Ulm and Passau also use some water from the Danube.

In Austria and Hungary, most water is drawn from ground and spring sources, and only in rare cases is water from the Danube used. Most states also find it too difficult to clean the water because of extensive pollution; only parts of Romania where the water is cleaner still obtain drinking water from the Danube on a regular basis.{{cite web |url=http://www.iawd.at/cms/pages/en/the-danube.php |title=The Danube |publisher=International Association of Water Supply Companies in the Danube River Catchment Area |access-date=28 July 2012 |archive-url=https://web.archive.org/web/20120519200631/http://www.iawd.at/cms/pages/en/the-danube.php |archive-date=19 May 2012 }}

=Navigation and transport=

File:Fischerzille LüA 10 m Donau bei Greifenstein Niederösterreich.jpg

In the 19th century, the Danube was an important waterway but was, as The Times of London put it, "annually swept by ice that will lift a large ship out of the water or cut her in two as if she were a carrot."{{Cite web|url=https://www.thetimes.com/|title=The Times & The Sunday Times|website=The Times}}

Today, as "Corridor VII" of the European Union, the Danube is an important transport route. Since the opening of the Rhine–Main–Danube Canal, the river connects the Port of Rotterdam and the industrial centers of Western Europe with the Black Sea and, also, through the Danube – Black Sea Canal, with the Port of Constanța.

The waterway is designed for large-scale inland vessels ({{nowrap|110 × 11.45 m}}) but it can carry much larger vessels on most of its course. The Danube has been partly canalized in Germany (5 locks) and Austria (10 locks). Proposals to build a number of new locks to improve navigation have not progressed, due in part to environmental concerns.

Downstream from the Freudenau locks in Vienna, canalization of the Danube was limited to the Gabčíkovo dam and locks near Bratislava and the two double Iron Gate locks in the border stretch of the Danube between Serbia and Romania. These locks have larger dimensions. Downstream of the Iron Gate, the river is free flowing all the way to the Black Sea, a distance of more than {{convert|860|km|mi}}.

The Danube connects with the Rhine–Main–Danube Canal at Kelheim, with the Donaukanal in Vienna, and with the Danube–Black Sea Canal at Cernavodă.

Apart from a couple of secondary navigable branches, the only major navigable rivers linked to the Danube are the Drava, Sava and Tisa. In Serbia, a canal network also connects to the river; the network, known as the Danube–Tisa–Danube Canals, links sections downstream.

In the Austrian and German sections of the Danube, a type of flat-bottomed boat called a Zille was developed for use along the river. Zillen are still used today for fishing, ferrying, and other transport of goods and people in this area.

=Fishing=

The importance of fishing on the Danube, which was critical in the Middle Ages, has declined dramatically. Some fishermen are still active at certain points on the river, and the Danube Delta still has an important industry. However, some of the river's resources have been managed in an environmentally unsustainable manner in the past, leading to damage by pollution, alterations to the channel, and major infrastructure development, including large hydropower dams.{{cite book |last=Holcik |first=Juraj |date=1989 |title=The freshwater fishes of Europe Vol.I Part II General introduction to fishes|location=Wiesbaden |publisher=Aula Verlag}}

The sturgeon stocks associated with the Danube River basin have, over the centuries, formed the basis of a large and significant commercial fishery, renowned throughout the world. The construction of the dams, besides overfishing and river pollution, has a significant role in sturgeon population decline because it creates a barrier for fish migratory species that usually spawn in the upper parts of the river.{{cite book |last1=Hensel |first1=K |last2=Holcik |first2=J |date=1997 |title=Past and current status of sturgeons in the upper and middle Danube River.|url=https://www.researchgate.net/publication/226596320}} The spawning areas of migratory fishes species has been dramatically reduced by the construction of hydropower and navigation systems at Iron Gates I (1974) and Iron Gates II (1984).{{cite web |author=Corda |date=1988 |title=Iron gates II design and performance of dams- geotechnical considerations |url=https://scholarsmine.mst.edu/cgi/viewcontent.cgi?article=1503&context=icchge |publisher=International Conference on Case Histories in Geotechnical Engineering |format=PDF}} The initial design of these dams has not included any fish passage facility.{{cite conference |url=https://www.danube-iad.eu/docs/IAD39_Proceeding_Book_lores.pdf |title=Have sturgeons a future in the Danube River? |author=Suciu Radu, Guti Gabor |year=2012 |conference=39th IAD Conference: Living Danube |location=Szentendre, Hungary }} The possibility of building a human-made fish pass enabling migration for fish species including the sturgeon, is currently under review by projects such as We Pass.{{cite AV media |date= 11 November 2019 |title= We Pass – Facilitating Fish Migration and Conservation at the Iron Gates |language=en |url=https://www.youtube.com/watch?v=81i25THmBws |archive-url=https://ghostarchive.org/varchive/youtube/20211215/81i25THmBws |archive-date=15 December 2021 |url-status=live|publisher=ICPDR }}{{cbignore}}

The Upper Danube ecoregion alone has about 60 fish species and the Lower Danube–Dniester ecoregion has about twice as many.Hales, J. (2013). [http://www.feow.org/ecoregions/details/417 Upper Danube]. Freshwater Ecoregions of the World. Retrieved 25 February 2013. Among these are an exceptionally high diversity of sturgeon, a total of six species (beluga, Russian sturgeon, bastard sturgeon, sterlet, starry sturgeon and European sea sturgeon), but these are all threatened and have largely–or entirely in the case of the European sea sturgeon–disappeared from the river. The huchen, one of the largest species of salmon, is endemic to the Danube basin, but has been introduced elsewhere by humans.{{FishBase | genus = Hucho | species = hucho | month = February | year = 2013}}

=Tourism=

File:Ruine Aggstein 03.JPG above the Danube]]

File:Wachau (3).JPG near Spitz, Austria]]

Important tourist and natural spots along the Danube include the Wachau Valley, the Nationalpark Donau-Auen in Austria, Gemenc in Hungary, the Naturpark Obere Donau in Germany, Kopački rit in Croatia, Iron Gate in Serbia and Romania, the Danube Delta in Romania, and the Srebarna Nature Reserve in Bulgaria.

Also, leisure and travel cruises on the river are of significance. Besides the often frequented route between Vienna and Budapest, some ships even go from Passau in Germany to the Danube Delta and back. During the peak season, more than 70 cruise liners are in use on the river, while the traffic-free upper parts can only be discovered with canoes or boats.

The Danube region is not only culturally and historically of importance, but also important for the regional tourism industry due to its fascinating landmarks and sights. With its well established infrastructure regarding cycling, hiking, and travel possibilities, the region along the Danube attracts every year an international clientele. In Austria alone, there are more than 14 million overnight stays and about 6.5 million arrivals per year.{{cite web|url=http://www.strassederkaiserundkoenige.at/fileadmin/user_upload/Brosch%C3%BCren/ARGE_Donau_%C3%96sterreich2013.pdf |title=Press release of the "ARGE Donau Österreich" |access-date=1 April 2014 |language=de |archive-url=https://web.archive.org/web/20140313154833/http://www.strassederkaiserundkoenige.at/fileadmin/user_upload/Brosch%C3%BCren/ARGE_Donau_%C3%96sterreich2013.pdf |archive-date=13 March 2014 }}

The Danube Banks in Budapest are a part of Unesco World Heritage sites, they can be viewed from a number of sightseeing cruises offered in the city.

The Danube Bend is also a popular tourist destination.

==Danube Bike Trail==

File:Donauradweg Schloegener Schlinge - Aschach.jpg

File:LinzDonaulaende.jpg]]

The Danube Bike Trail (also called Danube Cycle Path or the Donauradweg) is a bicycle trail along the river. Especially the parts through Germany and Austria are very popular, which makes it one of the 10 most popular bike trails in Germany.{{cite web |title=Die ADFC-Radreiseanalyse 2013 – Zahlen, Daten und Fakten |url=http://www.adfc.de/radreiseanalyse/die-adfc-radreiseanalyse-2013 |access-date=12 March 2014 |language=de |archive-url=https://web.archive.org/web/20170618233337/http://www.adfc.de/radreiseanalyse/die-adfc-radreiseanalyse-2013 |archive-date=18 June 2017 }}

The Danube Bike Trail starts at the origin of the Danube and ends where the river flows into the Black Sea. It is divided into four sections:

  1. DonaueschingenPassau ({{Convert|559|km|mi|abbr=on|disp=or}})
  2. PassauVienna ({{Convert|340|km|mi|abbr=on|disp=or}})
  3. ViennaBudapest ({{Convert|306|km|mi|abbr=on|disp=or}})
  4. BudapestBlack Sea ({{Convert|1670|km|mi|abbr=on|disp=or}})

==Sultans Trail==

The Sultans Trail is a hiking trail that runs along the river between Vienna and Smederevo in Serbia. From there the Sultans Trail leaves the Danube, terminating in Istanbul. Sections along the river are as follows.

  1. ViennaBudapest ({{Convert|323|km|mi|abbr=on|disp=or}})
  2. BudapestSmederevo ({{Convert|595|km|mi|abbr=on|disp=or}})

==Donausteig==

File:Donausteig Rastplatz.jpg]]

In 2010, the Donausteig, a hiking trail from Passau to Grein, was opened. It is {{convert|450|km|mi|sp=us|abbr=on}} long and it is divided into 23 stages. The route passes through five Bavarian and 40 Austrian communities. A landscape and viewpoints, which are along the river, are the highlights of the Donausteig.{{ cite web |title=Donausteig |url= http://www.traildino.com/trace/continents-Europe/countries-Austria/trails-Donausteig |website=Traildino.com |access-date=1 April 2014}}

==The Route of Emperors and Kings==

The Route of Emperors and Kings is an international touristic route leading from Regensburg to Budapest, calling in Passau, Linz and Vienna.{{Cite web|url=https://www.routeofemperorsandkings.com/|title=Welcome|website=Straße der Kaiser und Könige}} The international consortium ARGE Die Donau-Straße der Kaiser und Könige, comprising ten tourism organisations, shipping companies, and cities, strives for the conservation and touristic development of the Danube region.

In medieval Regensburg, with its maintained old town, stone bridge and cathedral, the Route of Emperors and Kings begins. It continues to Engelhartszell, with the only Trappist monastery in Austria. Further highlight-stops along the Danube, include the "Schlögener Schlinge", the city of Linz, which was European Capital of Culture in 2009 with its contemporary art richness, the Melk Abbey, the university city of Krems and the cosmopolitan city of Vienna. Before the Route of Emperors and Kings ends, you pass Bratislava and Budapest, the latter of which was seen as the twin town of Vienna during the times of the Austro-Hungarian Empire.

Since ancient Roman times, famous emperors and their retinue traveled on and along the Danube and used the river for travel and transportation. While traveling on the mainland was quite exhausting, most people preferred to travel by ship on the Danube. So the Route of Emperors and Kings was the setting for many important historical events, which characterize the Danube up until today.

The route got its name from the Holy Roman Emperor Frederick I of Barbarossa and the crusaders as well as from Richard I of England who had been jailed in the Dürnstein Castle, which is situated above the Danube. The most imperial journeys throughout time were those of the Habsburg family. Once crowned in Frankfurt, the emperors ruled from Vienna and also held in Regensburg the Perpetual Diet of Regensburg. Many famous castles, palaces, residences, and state-run convents were built by the Habsburger along the river. Nowadays they still remind us of the bold architecture of the "Donaubarock".

Today, people can not only travel by boat on the Danube but also by train, by bike on the Danube Bike Trail or walk on the "Donausteig" and visit the UNESCO World Heritage cities of Regensburg, Wachau and Vienna.{{cite web |title=The Route of Emperors and Kings |url=https://www.bavaria.by/the-route-of-emperors-and-kings |access-date=29 March 2014 |website=bavaria.by}}

Important national parks

  • Naturpark Obere Donau (Germany)
  • Donauauen zwischen Neuburg und Ingolstadt (Germany) – [https://web.archive.org/web/20111023161527/http://danubemap.eu/donauauwald map]
  • Nature protection area Donauleiten (Germany)
  • Nationalpark Donau Auen (Austria) – [https://web.archive.org/web/20111023161522/http://danubemap.eu/donauauen map]
  • Chránená krajinná oblasť Dunajské luhy (Slovakia) – [https://web.archive.org/web/20111021055315/http://danubemap.eu/dunajskeluhy map]
  • Danube-Ipoly National Park (Hungary) – [https://web.archive.org/web/20111021055252/http://danubemap.eu/dunaipoly map]
  • Danube-Drava National Park (Hungary) – [https://web.archive.org/web/20111023101801/http://danubemap.eu/dunadrava map]
  • Naturalpark Kopački Rit (Croatia) – [https://web.archive.org/web/20111023110151/http://danubemap.eu/kopackirit map]
  • Gornje Podunavlje Nature Reserve (Serbia) – [https://web.archive.org/web/20111024011005/http://danubemap.eu/podunavlje map]
  • Fruška Gora National Park (Serbia)
  • Koviljsko-petrovaradinski rit Nature Reserve (Serbia)
  • Great War Island Nature Reserve (Serbia)
  • Đerdap National park (Serbia)
  • Iron Gates Natural Park (Romania)
  • Persina Nature Park (Bulgaria) – [https://web.archive.org/web/20111023161537/http://danubemap.eu/persina map]
  • Kalimok-Brushlen Protected Site (Bulgaria) – [https://web.archive.org/web/20111023110144/http://danubemap.eu/kalimok map]
  • Srebarna Nature Reserve (Bulgaria) – [https://web.archive.org/web/20111024012109/http://danubemap.eu/srebarna map]
  • Măcin Mountains Natural Park (Romania)
  • Balta Mică a Brăilei Natural Park (Romania)
  • Danube Delta Biosphere Reserve (Romania) – [https://web.archive.org/web/20111023101756/http://danubemap.eu/delta map]
  • Danube Biosphere Reserve in Ukraine

File:Gornje Podunavlje.jpg|Gornje Podunavlje Special Nature Reserve in Serbia

File:Golubac Fortress (град Голубац).jpg|Golubac Fortress in Đerdap National park, Serbia

See also

Further reading

  • Lóczy, Dénes. The Danube: Morphology, Evolution, and Environmental Issues. In Avijit Gupta, ed., Large Rivers: Geomorphology and Management. 2nd Ed. Hoboken, N.J.: Wiley-Blackwell, 2022, pp. 335–367. ISBN 9781119412601
  • Sommerwerk, Nike, Jurg Bloesch, Christian Baumgartner, Thomas Bittl, Dubravka Cerba, Bela Csanyi, Grigore Davideanu, Martin Dokulil, Georg Frank, Iulia Grecu, Thomas Hein, Vladimir Kovac, Ilulian Nichersu, Tibor Mikuska, Karin Pall, Momir Paunovic, Carmen Postolache, Maja Rakovic, Cristina Sandu, Martin Schneider-Jacoby, Katharina Stefke, Klement Tockner, Ion Toderas, and Laurentia Ungureanu. The Danube River Basin. In Klement Tockner, Christiane Zarfl, and Christopher T. Robinson (eds.), Rivers of Europe, 2nd Ed. Cambridge, MA: Elsevier, 2022, pp. 83–181. ISBN 978-0-08-102612-0

References

{{Reflist}}

=Notes=

{{notelist}}

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