Comments on "Decadal Changes in the North Atlantic and Pacific Meridional Overturning Circulation and Heat Flux"
Comments on "Decadal Changes in the North Atlantic and Pacific Meridional Overturning Circulation and Heat Flux"
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对“北大西洋和太平洋经向翻转环流和热通量的年代际变化”的评论
DOI：
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发表时间：
2008
期刊：
影响因子：
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通讯作者：
A. Coward
中科院分区：
文献类型：
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作者：
P. M. Saunders;S. Cunningham;B. Cuevas;A. Coward
它表明，目前的水平模型，无论是同化和不同化，在北大西洋（就像他们的前辈）产生太浅的翻转，因为他们不再现从格陵兰岛和挪威海的冷水羽流的下降。因此，C. Wunsch和P.Heimbach提出了质疑。
It is demonstrated that current level models, both with and without assimilation, generate too shallow an overturning in the North Atlantic (just like their predecessors) because they do not reproduce the descent of plumes of cold water from the Greenland and Norwegian Seas. Consequently, the prediction of decadal change from one such model reported by C. Wunsch and P. Heimbach is queried.