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DOI10.1126/science.282.5388.436
A short circuit in thermohaline circulation: A cause for Northern Hemisphere glaciation?
Driscoll N.W.; Haug G.H.
发表日期1998
ISSN0036-8075
起始页码436
结束页码438
卷号282期号:5388
英文摘要The cause of Northern Hemisphere glaciation about 3 million years ago remains uncertain. Closing the Panamanian Isthmus increased thermohaline circulation and enhanced moisture supply to high latitudes, but the accompanying heat would have inhibited ice growth. One possible solution is that enhanced moisture transported to Eurasia also enhanced freshwater delivery to the Arctic via Siberian rivers. Freshwater input to the Arctic would facilitate sea ice formation, increase the albedo, and isolate the high heat capacity of the ocean from the atmosphere. It would also act as a negative feedback on the efficiency of the 'conveyor belt' heat pump.
英文关键词fresh water; ice; freshwater input; glaciation; Northern Hemisphere; paleoceanography; paleoclimate; thermohaline circulation; arctic; heat exchange; lake; moisture; priority journal; review; sea
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/243570
作者单位Woods Hole Oceanographic Institution, Woods Hole, MA 02543, United States; GEOMAR, Forschungszentrum Mar. G., Universität Kiel, Wischhofstrasse 1-3, D-24148 Kiel, Germany
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Driscoll N.W.,Haug G.H.. A short circuit in thermohaline circulation: A cause for Northern Hemisphere glaciation?[J],1998,282(5388).
APA Driscoll N.W.,&Haug G.H..(1998).A short circuit in thermohaline circulation: A cause for Northern Hemisphere glaciation?.Science,282(5388).
MLA Driscoll N.W.,et al."A short circuit in thermohaline circulation: A cause for Northern Hemisphere glaciation?".Science 282.5388(1998).
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