Retreat of mountain glaciers of northern Eurasia since the Little Ice Age maximum
نویسندگان
چکیده
منابع مشابه
Ice Cores , High - Mountain Glaciers , and Climate
The near-global retreat of high-mountain glaciers and the shrinkage of ice fields and ice caps and retreat of their associated outlet glaciers are perhaps the most visible evidence for 20th-century climate change and the recent increase in the globally averaged near-surface temperatures of the Earth’s surface. The loss of high-mountain glaciers—including ice fields, ice caps, and other glaciers...
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The Atlantic Multidecadal Oscillation (AMO) represents a significant driver of Northern Hemisphere climate, but the forcing mechanisms pacing the AMO remain poorly understood. Here we use the available proxy records to investigate the influence of solar and volcanic forcing on the AMO over the last ~450 years. The evidence suggests that external forcing played a dominant role in pacing the AMO ...
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Introduction Conclusions References
متن کاملLittle Ice Age
Volume 1, The Earth system: physical and chemical dimensions of global environmental change, pp 504–509
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The last maximum glacier advance in many mountain ranges appears to have predated the last maximum advance of the Wisconsinan continental ice sheets (-20,000 years B.P.). Published evidence from widely spaced localities in North and South America, Europe, Asia, and Hawai'i suggests that some mountain glaciers extended farther during one or more stades early in the last glaciation, roughly 115,0...
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ژورنال
عنوان ژورنال: Annals of Glaciology
سال: 2000
ISSN: 0260-3055,1727-5644
DOI: 10.3189/172756400781820499