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alpine climate

{{Short description|Typical weather for regions above the tree line}}

{{For|the climate of the mountains named the "Alps"|Climate of the Alps}}

File:White Mountain CA.JPG, an alpine environment at {{convert|4300|m|ft|-3}} above sea level in California]]

Alpine climate is the typical climate for elevations above the tree line, where trees fail to grow due to cold. This climate is also referred to as a mountain climate or highland climate.

Definition

There are multiple definitions of alpine climate.

In the Köppen climate classification, the alpine and mountain climates are part of group E, along with the polar climate, where no month has a mean temperature higher than {{convert|10|C|F}}.{{cite book | last1=McKnight | first1=Tom L | last2=Hess | first2=Darrel | year=2000 | chapter=Climate Zones and Types: The Köppen System | title=Physical Geography: A Landscape Appreciation | pages=[https://archive.org/details/physicalgeographmckn/page/235 235–7] | location=Upper Saddle River, New Jersey | publisher=Prentice Hall | isbn=978-0-13-020263-5 | chapter-url-access=registration | chapter-url=https://archive.org/details/physicalgeographmckn | url=https://archive.org/details/physicalgeographmckn/page/235 }}

According to the Holdridge life zone system, there are two mountain climates which prevent tree growth :

a) the alpine climate,

which occurs when the mean biotemperature of a location is between {{convert|1.5|and|3|C|F}}. The alpine climate in Holdridge system is roughly equivalent to the warmest tundra climates (ET) in the Köppen system.

b) the alvar climate, the coldest mountain climate since the biotemperature is between 0 °C and 1.5 °C (biotemperature can never be below 0 °C). It corresponds more or less to the coldest tundra climates and to the ice cap climates (EF) as well.

Holdrige reasoned that plants net primary productivity ceases with plants becoming dormant at temperatures below {{convert|0|C|F}} and above {{convert|30|C|F}}.{{cite journal|last1=Lugo|first1=A. E.|title=The Holdridge life zones of the conterminous United States in relation to ecosystem mapping|journal=Journal of Biogeography|date=1999|volume=26|issue=5|pages=1025–1038|url=https://www.researchgate.net/publication/227649905|access-date=27 May 2015|doi=10.1046/j.1365-2699.1999.00329.x|bibcode=1999JBiog..26.1025L |s2cid=11733879 }} Therefore, he defined biotemperature as the mean of all temperatures but with all temperatures below freezing and above 30 °C adjusted to 0 °C; that is, the sum of temperatures not adjusted is divided by the number of all temperatures (including both adjusted and non-adjusted ones).

The variability of the alpine climate throughout the year depends on the latitude of the location. For tropical oceanic locations, such as the summit of Mauna Loa, the temperature is roughly constant throughout the year.{{cite web|work=MAUNA LOA SLOPE OBS, HAWAII|title=Period of Record Monthly Climate Summary|url=http://www.wrcc.dri.edu/cgi-bin/cliMAIN.pl?himaun|publisher=NOAA|access-date=2012-06-05}} For mid-latitude locations, such as Mount Washington in New Hampshire, the temperature varies seasonally, but never gets very warm.{{cite web |title=Station Name: NH MT WASHINGTON |publisher=National Oceanic and Atmospheric Administration |url=ftp://ftp.ncdc.noaa.gov/pub/data/normals/1981-2010/products/station/USW00014755.normals.txt |archive-url=https://web.archive.org/web/20170525074713/ftp://ftp.ncdc.noaa.gov/pub/data/normals/1981-2010/products/station/USW00014755.normals.txt |archive-date=2017-05-25 |url-status=dead |access-date=9 June 2014}}{{cite web |title=WMO Climate Normals for MOUNT WASHINGTON, NH 1961–1990 |publisher=National Oceanic and Atmospheric Administration |url=ftp://ftp.atdd.noaa.gov/pub/GCOS/WMO-Normals/TABLES/REG_IV/US/GROUP3/72613.TXT |archive-url=https://web.archive.org/web/20170525074713/ftp://ftp.atdd.noaa.gov/pub/GCOS/WMO-Normals/TABLES/REG_IV/US/GROUP3/72613.TXT |archive-date=2017-05-25 |url-status=dead |access-date=9 June 2014}}

Cause

The temperature profile of the atmosphere is a result of an interaction between radiation and convection. Sunlight in the visible spectrum hits the ground and heats it. The ground then heats the air at the surface. If radiation were the only way to transfer heat from the ground to space, the greenhouse effect of gases in the atmosphere would keep the ground at roughly {{convert|333|K|C F}}, and the temperature would decay exponentially with height.{{cite book|first1=Richard M.|last1=Goody|first2=James C.G.|last2=Walker|title=Atmospheres|chapter=Atmospheric Temperatures|chapter-url=http://lasp.colorado.edu/~bagenal/3720/GoodyWalker/AtmosCh3sm.pdf|publisher=Prentice-Hall|year=1972|access-date=2016-05-02|archive-date=2016-07-29|archive-url=https://web.archive.org/web/20160729075851/http://lasp.colorado.edu/~bagenal/3720/GoodyWalker/AtmosCh3sm.pdf|url-status=dead}}

However, when air is hot, it tends to expand, which lowers its density. Thus, hot air tends to rise and transfer heat upward. This is the process of convection. Convection comes to equilibrium when a parcel of air at a given altitude has the same density as its surroundings. Air is a poor conductor of heat, so a parcel of air will rise and fall without exchanging heat. This is known as an adiabatic process, which has a characteristic pressure-temperature curve. As the pressure gets lower, the temperature decreases. The rate of decrease of temperature with elevation is known as the adiabatic lapse rate, which is approximately 9.8 °C per kilometer (or 5.4 °F per 1000 feet) of altitude.

The presence of water in the atmosphere complicates the process of convection. Water vapor contains latent heat of vaporization. As air rises and cools, it eventually becomes saturated and cannot hold its quantity of water vapor. The water vapor condenses (forming clouds), and releases heat, which changes the lapse rate from the dry adiabatic lapse rate to the moist adiabatic lapse rate (5.5 °C per kilometre or 3 °F per 1000 feet).{{cite web|url=http://meteorologytraining.tpub.com/14312/css/14312_47.htm |title=Dry Adiabatic Lapse Rate |publisher=tpub.com |access-date=2016-05-02 |url-status=dead |archive-url=https://web.archive.org/web/20160603041448/http://meteorologytraining.tpub.com/14312/css/14312_47.htm |archive-date=2016-06-03 }} The actual lapse rate, called the environmental lapse rate, is not constant (it can fluctuate throughout the day or seasonally and also regionally), but a normal lapse rate is 5.5 °C per 1,000 m (3.57 °F per 1,000 ft).{{cite book

| chapter-url=http://goldbook.iupac.org/A00144.html

| chapter=Adiabatic Lapse Rate

| publisher=IUPAC| doi=10.1351/goldbook.A00144

| year=2009

| isbn=978-0-9678550-9-7

| title=The IUPAC Compendium of Chemical Terminology

}}{{Cite book|last=Dommasch|first=Daniel O.|title=Airplane Aerodynamics (3rd ed.)|publisher=Pitman Publishing Co.|year=1961|page=22}} Therefore, moving up {{convert|100|m}} on a mountain is roughly equivalent to moving 80 kilometres (50 miles or 0.75° of latitude) towards the pole.{{cite web

| title= Mountain Environments

| url= http://quin.unep-wcmc.org/mountains/mountain_watch/pdfs/mountainEnvironments.pdf

| archive-url= https://web.archive.org/web/20110825113735/http://quin.unep-wcmc.org/mountains/mountain_watch/pdfs/mountainEnvironments.pdf

| archive-date=2011-08-25

| publisher = United Nations Environment Programme World Conservation Monitoring Centre}} This relationship is only approximate, however, since local factors, such as proximity to oceans, can drastically modify the climate.{{cite web

| url=http://www.ecn.ac.uk/Education/factors_affecting_climate.htm

| archive-url=https://web.archive.org/web/20110716163841/http://www.ecn.ac.uk/Education/factors_affecting_climate.htm

| archive-date=2011-07-16

| title=Factors affecting climate

| publisher=The United Kingdom Environmental Change Network}} As the altitude increases, the main form of precipitation becomes snow and the winds increase. The temperature continues to drop until the tropopause, at {{convert|11000|m|ft}}, where it does not decrease further. This is higher than the highest summit.

Distribution

File:Alpine climate map.gif

Although this climate classification only covers a small portion of the Earth's surface, alpine climates are widely distributed.

Mountainous areas that have alpine climate include:{{cite journal|last1=Testolin|first1=Riccardo|last2=Attorre|first2=Fabio|last3=Jiménez-Alfaro|first3=Borja|year=2020|title=Global distribution and bioclimatic characterization of alpine biomes|journal=Ecography|volume=43|issue=6 |pages=779–788 |doi=10.1111/ecog.05012|bibcode=2020Ecogr..43..779T |hdl=11585/896830|hdl-access=free}}

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File:Treeline elevation.gif

The lowest altitude of alpine climate varies dramatically by latitude. If alpine climate is defined by the tree line, then it occurs as low as {{convert|650|m|ft}} at 68°N in Sweden,{{cite journal|last1=Körner|first1=Ch|year=1998|title=A re-assessment of high elevation treeline positions and their explanation|journal=Oecologia|volume=115|pages=445–459|doi=10.1007/s004420050540|pmid=28308263|issue=4|url=http://culter.colorado.edu/~kittel/TreelineLat_Koerner98.pdf|bibcode=1998Oecol.115..445K|citeseerx=10.1.1.454.8501|s2cid=8647814|access-date=2015-08-05|archive-date=2006-09-11|archive-url=https://web.archive.org/web/20060911194023/http://culter.colorado.edu/%7ekittel/TreelineLat_Koerner98.pdf|url-status=dead}} while on Mount Kilimanjaro in Tanzania, the tree line is at {{convert|3950|m}}.

See also

References

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Category:Köppen climate types

Category:Mountain meteorology

Category:Montane ecology

Category:Climate by mountain range

Category:Climate of the Alps