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Titlebook: Influence of Climate Change on the Changing Arctic and Sub-Arctic Conditions; Jacques C. J. Nihoul,Andrey G. Kostianoy Conference proceedi

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书目名称Influence of Climate Change on the Changing Arctic and Sub-Arctic Conditions
编辑Jacques C. J. Nihoul,Andrey G. Kostianoy
视频video
概述The first book to address the Arctic and Sub-Arctic Environmental and Geo-economic conditions including the effects of global warming on ecosystems and populations with a prospective view of the evolu
丛书名称NATO Science for Peace and Security Series C: Environmental Security
图书封面Titlebook: Influence of Climate Change on the Changing Arctic and Sub-Arctic Conditions;  Jacques C. J. Nihoul,Andrey G. Kostianoy Conference proceedi
描述.The current warming trends in the Arctic may shove the Arctic system into a seasonally ice-free state not seen for more than one million years. The melting is accelerating, and researchers were unable to identify natural processes that might slow the deicing of the Arctic. Such substantial additional melting of Arctic and Antarctic glaciers and ice sheets would raise the sea level worldwide, flooding the coastal areas where many of the world‘s population lives. Studies, led by scientists at the National Center for Atmospheric Research (NCAR) and the University of Arizona, show that greenhouse gas increases over the next century could warm the Arctic by 3-5°C in summertime. Thus, Arctic summers by 2100 may be as warm as they were nearly 130,000 years ago, when sea levels eventually rose up to 6 m higher than today..
出版日期Conference proceedings 2009
关键词Arctic Ocean; Climate Change; Coast; Global warming; Greenhouse Gas; Ocean; Plankton; Sea ice; Sediment; biog
版次1
doihttps://doi.org/10.1007/978-1-4020-9460-6
isbn_softcover978-1-4020-9459-0
isbn_ebook978-1-4020-9460-6Series ISSN 1874-6519 Series E-ISSN 1874-6543
issn_series 1874-6519
copyrightSpringer Science+Business Media B.V. 2009
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Conference proceedings 2009 gas increases over the next century could warm the Arctic by 3-5°C in summertime. Thus, Arctic summers by 2100 may be as warm as they were nearly 130,000 years ago, when sea levels eventually rose up to 6 m higher than today..
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Conference proceedings 2009elting is accelerating, and researchers were unable to identify natural processes that might slow the deicing of the Arctic. Such substantial additional melting of Arctic and Antarctic glaciers and ice sheets would raise the sea level worldwide, flooding the coastal areas where many of the world‘s p
发表于 2025-3-22 22:53:33 | 显示全部楼层
Overture,ates that the global average temperature could increase as much as 5.8°C by the end of the 21st century. But these estimates don‘t factor in some feedback mechanisms that may be triggered by rising temperatures. For instance, accelerated decomposition in soils and changes in ocean chemistry may add
发表于 2025-3-23 05:18:53 | 显示全部楼层
Global warming effects on the Arctic and Sub-Arctic Seas, effects of global warming were more of a hydrodynamic nature and that the ocean dynamics and its modifications in response to global warming constituted an essential factor. Taking into account the effect of global warming on ocean temperature distribution and currents contributed to a large extent
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