Iqlim — versiyalar orasidagi farq

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xulosa tahrirlanmadi
(yangi)
 
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Mintaqa iqlimi '''iqlim tizimi''' tomonidan shakllanadi, iqlim tizimi besh komponentdan iborat: [[atmosfera]], [[gidrosfera]], [[kriosfera]], quruqlik va [[biosfera]].<ref name="IPCC glossary">[http://www.ipcc.ch/publications_and_data/ar4/syr/en/annexes.html AR4 SYR Synthesis Report Annexes]. Ipcc.ch. Retrieved on 2011-06-28.</ref>
 
Joy iqlimiga uning [[balandlik|balandligi]], [[kenglik]] va [[uzunligi]], [[relyefi]] hamda atrofdagi [[suv havzasi|suv havzalari]] taʼsir qiladi. Iqlimlar harorat va yogʻiniga qarab [[iqlim tasnifi|sinflarga]] ajratiladi. Iqlimni [[iqlimshunoslik]] oʻrganadi.
The climate of a location is affected by its [[latitude]], [[terrain]], and [[altitude]], as well as nearby [[body of water|water bodies]] and their currents. Climates can be [[Climate classification|classified]] according to the average and the typical ranges of different variables, most commonly temperature and precipitation. The most commonly used classification scheme was originally developed by [[Wladimir Köppen]]. The Thornthwaite system,<ref>{{cite journal|doi=10.2307/210739|url=http://www.unc.edu/courses/2007fall/geog/801/001/www/ET/Thornthwaite48-GeogrRev.pdf|author=C. W. Thornthwaite|title=An Approach Toward a Rational Classification of Climate|journal=Geographical Review|volume=38|issue=1|pages=55–94|year=1948|jstor=210739}}</ref> in use since 1948, incorporates [[evapotranspiration]] along with temperature and precipitation information and is used in studying animal species diversity and potential effects of climate changes. The Bergeron and [[Spatial Synoptic Classification system]]s focus on the origin of air masses that define the climate of a region.
 
Global iqlim vaqti-vaqti bilan oʻzgarib turadi. Hozirgi shunday oʻzgarish [[global issiqlashuv]] nomi bilan atalgan.
[[Paleoclimatology]] is the study of ancient climates. Since direct observations of climate are not available before the 19th century, paleoclimates are inferred from ''proxy variables'' that include non-biotic evidence such as sediments found in [[lake beds]] and [[ice cores]], and biotic evidence such as tree rings and coral. [[Climate model]]s are mathematical models of past, present and future climates. [[Climate change]] may occur over long and short timescales from a variety of factors; recent warming is discussed in [[global warming]].
 
== Manbalar ==
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[[af:Klimaat]]
[[ang:Medumƿeder]]
[[ar:مناخ]]
[[an:Clima]]
[[az:İqlim]]
[[bn:জলবায়ু]]
[[ba:Климат]]
[[be:Клімат]]
[[be-x-old:Клімат]]
[[bg:Климат]]
[[bar:Klima]]
[[bs:Klima]]
[[br:Hin]]
[[ca:Clima]]
[[ceb:Klima]]
[[cs:Podnebí]]
[[cy:Hinsawdd]]
[[da:Klima]]
[[de:Klima]]
[[et:Kliima]]
[[el:Κλίμα]]
[[en:Climate]]
[[es:Clima]]
[[eo:Klimato]]
[[eu:Klima]]
[[fa:اقلیم]]
[[fr:Climat]]
[[fy:Klimaat]]
[[ga:Aeráid]]
[[gl:Clima]]
[[ko:기후]]
[[hy:Կլիմա]]
[[hi:जलवायु]]
[[hr:Klima]]
[[io:Klimato]]
[[id:Iklim]]
[[ia:Climate]]
[[is:Loftslag]]
[[it:Clima]]
[[he:אקלים]]
[[jv:Iklim]]
[[kn:ವಾಯುಗುಣ]]
[[krc:Климат]]
[[ka:კლიმატი]]
[[kk:Климат]]
[[ht:Klima]]
[[ky:Климат]]
[[la:Clima]]
[[lv:Klimats]]
[[lt:Klimatas]]
[[hu:Éghajlat]]
[[mk:Клима]]
[[mg:Toe-tany]]
[[ms:Iklim]]
[[mwl:Clima]]
[[mn:Уур амьсгал]]
[[my:ရာသီဥတု]]
[[nl:Klimaat]]
[[ja:気候]]
[[no:Klima]]
[[nn:Klima]]
[[oc:Clima]]
[[pnb:کلائمیٹ]]
[[pap:Klima]]
[[pl:Klimat]]
[[pt:Clima]]
[[kaa:Klimat]]
[[ro:Climă]]
[[rue:Клімат]]
[[ru:Климат]]
[[sco:Climate]]
[[stq:Klima]]
[[sq:Klima]]
[[scn:Clima]]
[[simple:Climate]]
[[sk:Podnebie]]
[[sl:Podnebje]]
[[sr:Клима]]
[[sh:Klima]]
[[fi:Ilmasto]]
[[sv:Klimat]]
[[ta:தட்பவெப்பநிலை]]
[[tt:Климат]]
[[th:ภูมิอากาศ]]
[[tg:Иқлим]]
[[tr:İklim]]
[[uk:Клімат]]
[[ur:آب و ہوا]]
[[za:Heiqhaeuh]]
[[vec:Clima]]
[[vi:Khí hậu]]
[[fiu-vro:Kliima]]
[[war:Klema]]
[[yi:קלימאט]]
[[zh-yue:氣候]]
[[zh:氣候]]