SOUTHERN OCEAN Sea-ice-driven shallow overturning

被引：3
|
作者：
Bindoff, Nathaniel L. [1 ,2 ,3 ,4 ]
Hobbs, William R. [1 ,2 ]
机构：
[1] UNSW Sydney, ARC Ctr Excellence Climate Syst Sci, Sydney, NSW 2052, Australia
[2] Univ Tasmania, Antarctic Climate & Ecosyst Cooperat Res Ctr, Private Bag 80, Hobart, Tas 7001, Australia
[3] Univ Tasmania, IMAS, Sandy Bay, Tas 7005, Australia
[4] CSIRO Marine & Atmospher Res, Hobart, Tas 7000, Australia
来源：
NATURE GEOSCIENCE | 2016年 / 9卷 / 08期
关键词：
CIRCULATION; WATER;
D O I：
10.1038/ngeo2766
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
Conversion of Antarctic circumpolar upwelling waters to less dense water has mainly been attributed to surface heat fluxes. An analysis of water-mass transformation shows that the dominant process is the formation of sea ice near Antarctica and its melt offshore.
引用
收藏
页码：569 / 570
页数：3
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