Sea Ice Growth, Melt, and Modeling: A Survey
Sea Ice Growth, Melt, and Modeling: A Survey
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海冰生长、融化和建模：一项调查
DOI：
10.1007/978-94-011-4132-1_23
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发表时间：
2000
影响因子：
4.9
通讯作者：
G. Flato
中科院分区：
文献类型：
--
作者：
M. Steele;G. Flato
整个北极地区的淡水收支可以简单地表述为：流入量减去流出量等于该地区的净变化。如果该区域被定义为包括所有被冰覆盖的海洋，那么海冰的增长和融化是一个内部术语，没有净效应。图1中的冰-海系统示意性地说明了这一点，其中北冰洋的净冰增长与格陵兰-冰岛-挪威（GIN）海的净冰融化相平衡。
The freshwater budget of the Arctic as a whole can be stated quite simply as: inflows minus outflows equals net change within the region. If the region is defined to include all ice-covered seas, then the growth and melt of sea ice is an internal term that has no net effect. This is illustrated schematically for the ice-ocean system in Figure 1 where net ice growth in the Arctic Ocean is balanced by net ice melt in the Greenland-IcelandNorwegian (GIN) Seas.