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Glacial Thermohaline Circulation and Climate:Forcing from the North or South?
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作者 Zhengyu LIU 《Advances in Atmospheric Sciences》 SCIE CAS CSCD 2006年第2期199-206,共8页
Based on the evidence available from both observations and model simulations, the author proposes a view that may provide a unified interpretation of the North Atlantic thermohaline variability. Because of the slow re... Based on the evidence available from both observations and model simulations, the author proposes a view that may provide a unified interpretation of the North Atlantic thermohaline variability. Because of the slow response time of the Southern Ocean (millennia) and the relatively faster response time of the North Atlantic (centuries), the North Atlantic thermohaline circulation is controlled predominantly by the climate forcing over the Southern Ocean at the long glacial cycle timescales, but by the North Atlantic climate forcing at the short millennial timescaies. 展开更多
关键词 interhemispheric interaction thermohaline circulation glacial cycle millennial variability
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