Shuttle Radar Topography Mission

{{short description|Project to create a digital topographic database of Earth}}

File:Zagros Mountains, Iran, SRTM Shaded Relief Anaglyph.jpg.]]

File:Srtm 1.jpg in February 2000.{{cite web|url=http://www2.jpl.nasa.gov/srtm/|title=Shuttle Radar Topography Mission: Mission to Map the World|access-date=2009-04-26|url-status=live|archive-url=http://archive.wikiwix.com/cache/20080823022748/http://www2.jpl.nasa.gov/srtm/|archive-date=2008-08-23}}]]

File:Satellite image of Cape peninsula.jpg data to texture-map the surface created using SRTM Elevation data. The Cape Peninsula and Cape of Good Hope, South Africa, are visible in the foreground.[http://photojournal.jpl.nasa.gov/catalog/PIA04961] ]]

The Shuttle Radar Topography Mission (SRTM) is an international research effort that obtained digital elevation models on a near-global scale from 56°S to 60°N,{{cite journal|last1=Nikolakopoulos |first1=K. G. |last2=Kamaratakis |first2=E. K |last3=Chrysoulakis |first3=N. |date=10 November 2006 |title=SRTM vs ASTER elevation products. Comparison for two regions in Crete, Greece |journal=International Journal of Remote Sensing |volume=27 |issue=21 |pages=4819–4838 |issn=0143-1161 |url=http://www.iacm.forth.gr/_docs/pubs/4/Nikolakopoulos_et_al_2006.pdf |access-date=1 July 2009 |doi=10.1080/01431160600835853 |bibcode=2006IJRS...27.4819N |s2cid=1939968 |url-status=dead |archive-url=https://web.archive.org/web/20110721081314/http://www.iacm.forth.gr/_docs/pubs/4/Nikolakopoulos_et_al_2006.pdf |archive-date=21 July 2011 }}{{rp|4820}} to generate the most complete high-resolution digital topographic database of Earth prior to the release of the ASTER GDEM in 2009. SRTM consisted of a specially modified radar system that flew on board the Space Shuttle Endeavour during the 11-day STS-99 mission in February 2000. The radar system was based on the older Spaceborne Imaging Radar-C/X-band Synthetic Aperture Radar (SIR-C/X-SAR), previously used on the Shuttle in 1994. To acquire topographic data, the SRTM payload was outfitted with two radar antennas. One antenna was located in the Shuttle's payload bay, the other – a critical change from the SIR-C/X-SAR, allowing single-pass interferometry – on the end of a 60-meter (200-foot) mast that extended from the payload bay once the Shuttle was in space. The technique employed is known as interferometric synthetic aperture radar. Intermap Technologies was the prime contractor for processing the interferometric synthetic aperture radar data.

The elevation models are arranged into tiles, each covering one degree of latitude and one degree of longitude, named according to their south western corners. For example, "n45e006" stretches from 45°N 6°E to 46°N 7°E and "s45w006" from 45°S 6°W to 44°S 5°W. The resolution of the raw data is one arcsecond (30 m along the equator) and coverage includes Africa, Europe, North America, South America, Asia, and Australia.{{cite web|title=NASA Shuttle Radar Topography Mission (SRTM) Version 3.0 Global 1 arc second Data Released over Asia and Australia Version 1.0|url=https://earthdata.nasa.gov/nasa-shuttle-radar-topography-mission-srtm-version-3-0-global-1-arc-second-data-released-over-asia-and-australia|url-status=dead|archive-url=https://web.archive.org/web/20170513032841/https://earthdata.nasa.gov/nasa-shuttle-radar-topography-mission-srtm-version-3-0-global-1-arc-second-data-released-over-asia-and-australia|archive-date=2017-05-13}} A derived one arcsecond dataset with trees and other non-terrain features removed covering Australia was made available in November 2011; the raw data are restricted for government use.{{cite web|title=SRTM-derived 1 Second Digital Elevation Models Version 1.0|url=https://www.ga.gov.au/products/servlet/controller?event=GEOCAT_DETAILS&catno=72759|url-status=live|archive-url=https://web.archive.org/web/20120228201506/https://www.ga.gov.au/products/servlet/controller?event=GEOCAT_DETAILS&catno=72759|archive-date=2012-02-28}} For the rest of the world, only three arcsecond (90 m along the equator) data are available.{{rp|4821}} Each one arcsecond tile has 3,601 rows, each consisting of 3,601 16 bit bigendian cells. The dimensions of the three arcsecond tiles are 1201 x 1201. The original SRTM elevations were calculated relative to the WGS84 ellipsoid and then the EGM96 geoid separation values were added to convert to heights relative to the geoid for all the released products.{{cite journal|last1=Hirt|first1=C.|last2=Filmer|first2=M.S.|last3=Featherstone|first3=W.E.|date=2010|title=Comparison and validation of recent freely-available ASTER-GDEM ver1, SRTM ver4.1 and GEODATA DEM-9S ver3 digital elevation models over Australia|journal=Australian Journal of Earth Sciences|volume=57|issue=3|pages=337–347|url=http://espace.library.curtin.edu.au:80/R?func=dbin-jump-full&local_base=gen01-era02&object_id=137777|access-date=May 5, 2012|bibcode=2010AuJES..57..337H|doi=10.1080/08120091003677553|hdl=20.500.11937/43846|s2cid=140651372|hdl-access=free|archive-date=May 3, 2013|archive-url=https://web.archive.org/web/20130503104047/http://espace.library.curtin.edu.au/R?func=dbin-jump-full&local_base=gen01-era02&object_id=137777|url-status=live}}

The elevation models derived from the SRTM data are used in geographic information systems. They can be downloaded freely over the Internet, and their file format (.hgt) is widely supported.

The Shuttle Radar Topography Mission is an international project spearheaded by the U.S. National Geospatial-Intelligence Agency (NGA), an agency of the U.S. Department of Defense, and the U.S. National Aeronautics and Space Administration (NASA). NASA transferred the SRTM payload to the Smithsonian National Air and Space Museum in 2003; the canister, mast, and antenna are now on display at the Steven F. Udvar-Hazy Center in Chantilly, Virginia.{{cite web|title=Cannister/Mast, Shuttle Radar Topography Mission Payload|url=http://airandspace.si.edu/collections/artifact.cfm?object=nasm_A20040261000|publisher=Smithsonian National Air and Space Museum|access-date=24 July 2014|archive-date=9 August 2014|archive-url=https://web.archive.org/web/20140809103617/http://airandspace.si.edu/collections/artifact.cfm?object=nasm_A20040261000|url-status=live}}

Versions

The USGS SRTM data is based on NASA's SIR-C instrument. It is available in at the following versions:

  • Version 1 (2003–2004) is almost the raw data.{{Cite web|date=|title=What's new|url=https://dds.cr.usgs.gov/srtm/version1/Whats_new.txt|url-status=live|archive-url=https://web.archive.org/web/20161230132420/https://dds.cr.usgs.gov/srtm/version1/Whats_new.txt|archive-date=2016-12-30|access-date=|website=USGS Data Distribution Service}}
  • Version 2.1 (~2005) is an edited version of v1. Artifacts are removed, but voids are not yet filled. There are 1-arcsecond data over the US.{{cite journal|doi=10.1029/2005RG000183|title=The Shuttle Radar Topography Mission|date=2007|last1=Farr|first1=Tom G.|last2=Rosen|first2=Paul A.|last3=Caro|first3=Edward|last4=Crippen|first4=Robert|last5=Duren|first5=Riley|last6=Hensley|first6=Scott|last7=Kobrick|first7=Michael|last8=Paller|first8=Mimi|last9=Rodriguez|first9=Ernesto|last10=Roth|first10=Ladislav|last11=Seal|first11=David|last12=Shaffer|first12=Scott|last13=Shimada|first13=Joanne|last14=Umland|first14=Jeffrey|last15=Werner|first15=Marian|last16=Oskin|first16=Michael|last17=Burbank|first17=Douglas|last18=Alsdorf|first18=Douglas|journal=Reviews of Geophysics|volume=45|issue=2|pages=RG2004|bibcode = 2007RvGeo..45.2004F |citeseerx=10.1.1.102.9372|s2cid=140735782 }}
  • Version 3 (2013), also known as SRTM Plus, is void-filled with ASTER GDEM and USGS GMTED2010. This release is available in global 1-arcsecond (30 meter) resolution since 2014.

The SRTM also carries the X-SAR instrument operated by the German Aerospace Center (DLR) and Italian Space Agency (ASI). The resulting dataset is usually called SRTM/X-SAR, or SRTMX for short. The grid resolution is high at 25 meters, but it has many gaps. The data was made public in May 2011.{{cite web |title=SRTM X-SAR - Digital Elevation Model (DEM) 10° Mosaics - Global |url=https://www.europeandataportal.eu/data/datasets/f4d4079a-ada3-41d0-ba95-630ba232e147?locale=en |website=European Data Portal |access-date=2021-02-14 |archive-date=2021-09-10 |archive-url=https://web.archive.org/web/20210910132029/https://data.europa.eu/data/datasets/f4d4079a-ada3-41d0-ba95-630ba232e147?locale=en |url-status=live }}{{cite web |title=SRTM |url=https://www.dlr.de/caf/en/desktopdefault.aspx/tabid-5515/9214_read-17716/ |website=DLR - Earth Observation Center |access-date=2021-02-14 |archive-date=2018-05-20 |archive-url=https://web.archive.org/web/20180520035726/http://www.dlr.de/caf/en/desktopdefault.aspx/tabid-5515/9214_read-17716/ |url-status=live }}

The terminology regarding versions and resolutions can be confusing. "SRTM1" and "SRTM3" refers to the resolutions in 1 and 3 arc-seconds, not the versions of the format. On the other hand, "SRTM4.1" refers to a specific filled version by CGIAR-CSI. It is recommended to add a "v" in front of the version number to disambiguate.

No-data areas

File:Srtm voidfilling grass gis.png.]]

The elevation datasets are affected by mountain and desert no-data areas. These amount to no more than 0.2% of the total area surveyed,Reuter H.I, A. Nelson, A. Jarvis, 2007, [https://www.researchgate.net/publication/220650064_An_Evaluation_of_Void-Filling_Interpolation_Methods_for_SRTM_Data An evaluation of void filling interpolation methods for SRTM data], International Journal of Geographical Information Science, 21:9, 983–1008 – 'the ‘finished’ grade version of the data (also referred to as Version 2) still contains data voids (some 836,000 km^2)'; 836,000 is 0.164% of the Earth's 5.1×10^8 km^2 surface but can be a problem in areas of very high relief. They affect all summits over 8,000 meters, most summits over 7,000 meters, many Alpine and similar summits and ridges, and many gorges and canyons. There are some SRTM data sources which have filled these data voids, but some of these have used only interpolation from surrounding data, and may therefore be very inaccurate. If the voids are large, or completely cover summit or ridge areas, no interpolation algorithms will give satisfactory results.

Void-filled SRTM datasets

Image:Maps-for-free Sierra Nevada.png]]

File:SRTM1 Example Nevada.png

Groups of scientists have worked on algorithms to fill the voids of the original SRTM (v2.1) data. Three datasets offer global coverage void-filled SRTM data at full (3-arcsecond) resolution:

  • The CGIAR-CSI version 4 provides the best global coverage using interpolation.{{cite web

|url=http://srtm.csi.cgiar.org/

|publisher=Consultative Group on International Agricultural Research

|access-date = 26 December 2023

|title=SRTM 90m Digital Elevation Data

|date=19 August 2008

|archive-date=16 October 2014

|archive-url=https://web.archive.org/web/20141016030443/http://srtm.csi.cgiar.org/

|url-status=live

}}

  • The USGS HydroSHEDS dataset was generated for hydrological applications and is suitable for consistent drainage and water flow information. References are provided{{cite web

|url=http://hydrosheds.cr.usgs.gov/references.php

|publisher=United States Geological Survey

|access-date=10 October 2014

|title=USGS HydroSHEDS References

|date=5 September 2010

|archive-date=21 October 2014

|archive-url=https://web.archive.org/web/20141021005444/http://hydrosheds.cr.usgs.gov/references.php

|url-status=live

}} on the algorithms used and quality assessment.

{{cite web

|url = http://hydrosheds.cr.usgs.gov/

|publisher = United States Geological Survey

|access-date = 10 October 2014

|title = USGS HydroSHEDS

|date = 6 September 2010

|url-status = live

|archive-url = https://web.archive.org/web/20140928112952/http://hydrosheds.cr.usgs.gov/

|archive-date = 28 September 2014

}}

  • The void-filled SRTM data from Viewfinder Panoramas by Jonathan de Ferranti

{{cite web

|url = http://www.viewfinderpanoramas.org/dem3.html

|publisher = Viewfinder Panoramas

|access-date = 26 December 2023

|title = DIGITAL ELEVATION DATA

|url-status = live

|archive-url = https://web.archive.org/web/20091210183954/http://www.viewfinderpanoramas.org/dem3.html

|archive-date = 10 December 2009

}} are high quality at full SRTM resolution. The data is filled using local survey maps and photographs. The OpenTopoMap website uses this fill. It has been partially updated for the 1-arcsecond release in the US.

In November 2013, LP DAAC released

{{cite web

|url = https://lpdaac.usgs.gov/news/nasa-shuttle-radar-topography-mission-srtm-version-30-srtm-plus-product-release/

|publisher = United States Geological Survey

|access-date = 26 December 2023

|title = NASA Shuttle Radar Topography Mission (SRTM) Version 3.0 (SRTM Plus) Product Release

|date = 30 November 2013

|url-status = live

|archive-url = https://web.archive.org/web/20131224234411/https://lpdaac.usgs.gov/node/539

|archive-date = 24 December 2013

}} the NASA Shuttle Radar Topography Mission (SRTM) Version 3.0 (SRTM Plus) Product collection with all voids eliminated. Voids were filled primarily from ASTER GDEM2, and secondarily from USGS GMTED2010 – or USGS National Elevation Dataset (NED) for the United States (except Alaska) and northernmost Mexico according to the announcement.

Highest Resolution Global Release

1-arc second global digital elevation model (30 meters) is available from the United States Geological Survey web site. The United States Government announced on September 23, 2014 over a United Nations Climate Summit that the highest possible resolution of global topographic data derived from the SRTM mission will be released to public.{{cite web|title=U.S. Releases Enhanced Shuttle Land Elevation Data|url=http://www2.jpl.nasa.gov/srtm/|website=JPL-Shuttle Radar Topography Mission|access-date=31 January 2015|url-status=live|archive-url=http://archive.wikiwix.com/cache/20080823022748/http://www2.jpl.nasa.gov/srtm/|archive-date=23 August 2008}} Before the end of the same year, a 1-arc second global digital elevation model (30 meters) was released. Most parts of the world have been covered by this dataset ranging from 54°S to 60°N latitude except for the Middle East and North Africa area.{{cite web|title=USGS Earth Explorer|url=http://earthexplorer.usgs.gov/|website=USGS-EarthExplorer|access-date=31 January 2015|url-status=live|archive-url=https://web.archive.org/web/20150206111800/http://earthexplorer.usgs.gov/|archive-date=6 February 2015}} Missing coverage of the Middle East was completed in August 2015.{{cite web|url=https://lpdaac.usgs.gov/nasa_shuttle_radar_topography_mission_srtm_global_1_arc_second_data_released_over_middle_east|title=NASA Shuttle Radar Topography Mission (SRTM) Global 1 arc second Data Released Over the Middle East - LP DAAC :: NASA Land Data Products and Services|website=lpdaac.usgs.gov|url-status=live|archive-url=https://web.archive.org/web/20150913200035/https://lpdaac.usgs.gov/nasa_shuttle_radar_topography_mission_srtm_global_1_arc_second_data_released_over_middle_east|archive-date=2015-09-13}}

Users

In early June 2011, there were 750,000 confirmed users of SRTM topography dataset. Users in 221 countries have accessed the site.{{cite web |url=http://dapa.ciat.cgiar.org/dapas-srtm-topography-data-reaches-750000-users/ |title=DAPA's SRTM topography data reaches 750,000 users | DAPA |access-date=2011-06-24 |url-status=live |archive-url=https://web.archive.org/web/20110819172254/http://dapa.ciat.cgiar.org/dapas-srtm-topography-data-reaches-750000-users/ |archive-date=2011-08-19 }}

See also

Notes

{{Reflist}}

References

  • {{cite journal|last1=Nikolakopoulos |first1=K. G. |last2=Kamaratakis |first2=E. K |last3=Chrysoulakis |first3=N. |date=10 November 2006 |title=SRTM vs ASTER elevation products. Comparison for two regions in Crete, Greece |journal=International Journal of Remote Sensing |volume=27 |issue=21 |page=4819 |doi=10.1080/01431160600835853 |bibcode=2006IJRS...27.4819N |s2cid=1939968 |issn=0143-1161 |url=http://www.iacm.forth.gr/_docs/pubs/4/Nikolakopoulos_et_al_2006.pdf |access-date=March 10, 2010 |url-status=dead |archive-url=https://web.archive.org/web/20110721081314/http://www.iacm.forth.gr/_docs/pubs/4/Nikolakopoulos_et_al_2006.pdf |archive-date=July 21, 2011 }}
  • {{cite journal|last1=Hirt|first1=C.|last2=Filmer|first2=M.S. |last3=Featherstone|first3=W.E.|date=2010|title=Comparison and validation of recent freely-available ASTER-GDEM ver1, SRTM ver4.1 and GEODATA DEM-9S ver3 digital elevation models over Australia|journal=Australian Journal of Earth Sciences|volume=57|issue=3|pages=337–347|url=http://espace.library.curtin.edu.au:80/R?func=dbin-jump-full&local_base=gen01-era02&object_id=137777|access-date=May 5, 2012|bibcode = 2010AuJES..57..337H |doi = 10.1080/08120091003677553 |hdl=20.500.11937/43846|s2cid=140651372|hdl-access=free}}
  • {{cite journal|last1=Rexer|first1=M.|last2=Hirt|first2=C.|date=2014|title=Comparison of free high-resolution digital elevation data sets (ASTER GDEM2, SRTM v2.1/v4.1) and validation against accurate heights from the Australian National Gravity Database|journal=Australian Journal of Earth Sciences|volume=61|issue=2|pages=213–226|url=http://geodesy.curtin.edu.au/local/docs/Rexer_Hirt_2014_DEM_AJES_av.pdf|access-date=April 24, 2014|doi=10.1080/08120099.2014.884983|bibcode=2014AuJES..61..213R|url-status=dead|archive-url=https://web.archive.org/web/20160607102637/http://geodesy.curtin.edu.au/local/docs/Rexer_Hirt_2014_DEM_AJES_av.pdf|archive-date=June 7, 2016|hdl=20.500.11937/38264|s2cid=3783826|hdl-access=free}}
  • Hennig, T., Kretsch, J, Salamonowicz, P, Pessagno, C, and Stein, W., The Shuttle Radar Topography Mission, Proceedings of the First International Symposium on Digital Earth Moving 2001, Springer Verlag, London, UK.

Further reading

  • {{cite journal |last1=Li |first1=P. |last2=Li |first2=Z. |last3=Muller |first3=J.-P. |last4=Shi |first4=C. |last5=Liu |first5=J. |title=A new quality validation of global digital elevation models freely available in China |journal=Survey Review |date=November 2016 |volume=48 |issue=351 |pages=409–420 |doi=10.1179/1752270615Y.0000000039|s2cid=129792781 }}