QUATERNARY GLACIATION IN NORTHERN CENTRAL ASIA
In Central Asia, Pleistocene glaciations occurred in two climatic regimes: arid regions where annual precipitation was Mountain glaciers in arid Central Asia are important in and of themselves because their meltwater is necessary to sustain some communities through dry seasons when rainfall is sligh...
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Федеральное государственное бюджетное образовательное учреждение высшего профессионального образования "Национальный исследовательский Томский государственный университет"
2012
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ftcyberleninka:oai:cyberleninka.ru:article/13980904 2023-05-15T16:37:30+02:00 QUATERNARY GLACIATION IN NORTHERN CENTRAL ASIA Gillespie, Alan 2012 text/html http://cyberleninka.ru/article/n/quaternary-glaciation-in-northern-central-asia http://cyberleninka.ru/article_covers/13980904.png unknown Федеральное государственное бюджетное образовательное учреждение высшего профессионального образования "Национальный исследовательский Томский государственный университет" ЧЕТВЕРТИЧНОЕ ОЛЕДЕНЕНИЕ ПАЛЕОКЛИМАТИЧЕСКИЕ УСЛОВИЯ ПАЛЕОГЛЯЦИОЛОГИЧЕСКИЕ ПОКАЗАТЕЛИ ЭКОЛОГИЧЕСКИЙ ПРОГНОЗ text 2012 ftcyberleninka 2015-11-17T00:43:46Z In Central Asia, Pleistocene glaciations occurred in two climatic regimes: arid regions where annual precipitation was Mountain glaciers in arid Central Asia are important in and of themselves because their meltwater is necessary to sustain some communities through dry seasons when rainfall is slight. Furthermore, glaciers are commonly associated with ice-dammed lakes that can rupture to release dangerous outburst floods downstream. However, because of their widespread distribution in Central Asia, the most significant role for glaciers may be as a warning system for climate change and a signal for the degradation of permafrost and consequent release of greenhouse CH4 into the atmosphere. Text Ice permafrost CyberLeninka (Scientific Electronic Library) |
institution |
Open Polar |
collection |
CyberLeninka (Scientific Electronic Library) |
op_collection_id |
ftcyberleninka |
language |
unknown |
topic |
ЧЕТВЕРТИЧНОЕ ОЛЕДЕНЕНИЕ ПАЛЕОКЛИМАТИЧЕСКИЕ УСЛОВИЯ ПАЛЕОГЛЯЦИОЛОГИЧЕСКИЕ ПОКАЗАТЕЛИ ЭКОЛОГИЧЕСКИЙ ПРОГНОЗ |
spellingShingle |
ЧЕТВЕРТИЧНОЕ ОЛЕДЕНЕНИЕ ПАЛЕОКЛИМАТИЧЕСКИЕ УСЛОВИЯ ПАЛЕОГЛЯЦИОЛОГИЧЕСКИЕ ПОКАЗАТЕЛИ ЭКОЛОГИЧЕСКИЙ ПРОГНОЗ Gillespie, Alan QUATERNARY GLACIATION IN NORTHERN CENTRAL ASIA |
topic_facet |
ЧЕТВЕРТИЧНОЕ ОЛЕДЕНЕНИЕ ПАЛЕОКЛИМАТИЧЕСКИЕ УСЛОВИЯ ПАЛЕОГЛЯЦИОЛОГИЧЕСКИЕ ПОКАЗАТЕЛИ ЭКОЛОГИЧЕСКИЙ ПРОГНОЗ |
description |
In Central Asia, Pleistocene glaciations occurred in two climatic regimes: arid regions where annual precipitation was Mountain glaciers in arid Central Asia are important in and of themselves because their meltwater is necessary to sustain some communities through dry seasons when rainfall is slight. Furthermore, glaciers are commonly associated with ice-dammed lakes that can rupture to release dangerous outburst floods downstream. However, because of their widespread distribution in Central Asia, the most significant role for glaciers may be as a warning system for climate change and a signal for the degradation of permafrost and consequent release of greenhouse CH4 into the atmosphere. |
format |
Text |
author |
Gillespie, Alan |
author_facet |
Gillespie, Alan |
author_sort |
Gillespie, Alan |
title |
QUATERNARY GLACIATION IN NORTHERN CENTRAL ASIA |
title_short |
QUATERNARY GLACIATION IN NORTHERN CENTRAL ASIA |
title_full |
QUATERNARY GLACIATION IN NORTHERN CENTRAL ASIA |
title_fullStr |
QUATERNARY GLACIATION IN NORTHERN CENTRAL ASIA |
title_full_unstemmed |
QUATERNARY GLACIATION IN NORTHERN CENTRAL ASIA |
title_sort |
quaternary glaciation in northern central asia |
publisher |
Федеральное государственное бюджетное образовательное учреждение высшего профессионального образования "Национальный исследовательский Томский государственный университет" |
publishDate |
2012 |
url |
http://cyberleninka.ru/article/n/quaternary-glaciation-in-northern-central-asia http://cyberleninka.ru/article_covers/13980904.png |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
_version_ |
1766027800747180032 |