期刊
RUSSIAN METEOROLOGY AND HYDROLOGY
卷 33, 期 1, 页码 43-47出版社
ALLERTON PRESS INC
DOI: 10.3103/S106837390801007X
关键词
-
资金
- Russian Foundation for Basic Research [05-05-79128-k]
For the first time, based on direct observations of carbon dioxide concentration at modern Russian drifting stations, the role of the Arctic sea ice in maximum seasonal changes in carbon dioxide distribution is considered. Carbon dioxide is generated during growth of ice mass at the sea ice under-surface and is absorbed at the surface of melting sea ice. The time of ice growth is three or four times greater than that of its melting in summer months, and, as result, the time of carbon dioxide generation is longer that that of its uptake. Consequently, the Arctic Ocean is a source of carbon dioxide on the mean annual scale (the effect of Arctic breathing). Experiments in a freezing chamber confirm these conclusions.
作者
我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。
推荐
暂无数据