单位1:Institute of Atmospheric Physics, Academia Sinica
语种:英文
起始页:15
总页数:13
刊名:海洋文集
是否内版:是
主办单位:中国海洋学会海洋科技资料中心
期:1
期刊索取号:P\226.06\449-27
摘要
The effect of ice caps-temperature-albedo feedback on the global climate is examined by meansof a two-dimensional energy balance model.Under some approximations the new model is simplifiedinto Seller's one-dimensional model. According to the calculation made by us, therequirement forthe ice edge to move southward from the normal 72° to 50°N (i.e.where the glacial climate wouldtake place)is that the solar constant should decrease about 15% rather than 2% as predicted bysome authors according to the one-dimensional model. This means that the climate can not drastically“deteriorate”even if the solar energy output decreases slightly.