Permafrost and climatic change in Mongolia

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43410%2F09%3A00152365" target="_blank" >RIV/62156489:43410/09:00152365 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Permafrost and climatic change in Mongolia

Popis výsledku v původním jazyce

The permafrost area range in Mongolia is almost 1 million km2, and can be easily divided into latitudinal and altitudinal types. The permafrost environment has changed markedly several times in central Asia. The ice wedges and permafrost formed during the Late Pleistocene are still present in central Mongolia. The lower limit of altitudinal permafrost in western Mongolia has elevated only a little (near 300m) since the last glaciation maximum. Compared with that in northern Europe and North America, latitudinal permafrost in northeastern Mongolia is less sensitive to local warming, but altitudinal permafrost, especially permafrost in the Altai and Khangai and partially also in Khentii Mountains, is sensitive to climate warming. Since the middle of the20th century, significant permafrost degradation has occurred in Mongolia.

Název v anglickém jazyce

Permafrost and climatic change in Mongolia

Popis výsledku anglicky

The permafrost area range in Mongolia is almost 1 million km2, and can be easily divided into latitudinal and altitudinal types. The permafrost environment has changed markedly several times in central Asia. The ice wedges and permafrost formed during the Late Pleistocene are still present in central Mongolia. The lower limit of altitudinal permafrost in western Mongolia has elevated only a little (near 300m) since the last glaciation maximum. Compared with that in northern Europe and North America, latitudinal permafrost in northeastern Mongolia is less sensitive to local warming, but altitudinal permafrost, especially permafrost in the Altai and Khangai and partially also in Khentii Mountains, is sensitive to climate warming. Since the middle of the20th century, significant permafrost degradation has occurred in Mongolia.

Druh

D - Stať ve sborníku

CEP obor

DF - Pedologie

OECD FORD obor

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Projekt

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2009

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název statě ve sborníku

Sustainable development and bioclimate

ISBN

978-80-900450-1-9

ISSN

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e-ISSN

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Počet stran výsledku

2

Strana od-do

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Název nakladatele

Geophysical Institute of the Slovak Academy of Sciences and Slovak Bioclimatological Society of the Slovak Academy of Sciences

Místo vydání

Stará Lesná

Místo konání akce

Stará Lesná

Datum konání akce

5. 10. 2009

Typ akce podle státní příslušnosti

EUR - Evropská akce

Kód UT WoS článku

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