The Heat Balance of the Surface of the Earth
The Heat Balance of the Surface of the Earth
复制标题
地球表面的热平衡
DOI：
10.1080/00385417.1962.10769936
复制
发表时间：
1962
期刊：
影响因子：
--
通讯作者：
L. A. Strokina
中科院分区：
文献类型：
--
作者：
M. Budyko;N. Yefimova;L. I. Aubenok;L. A. Strokina
摘要 国际地球物理年观测计划提供了新的气象数据，使更精确地计算地球热平衡成为可能。通过改进或计算方法也实现了更高的准确性。作者利用 2,000 个站点（包括海洋区域 300 个点）的数据，绘制了热平衡主要组成部分的世界地图。从这些地图中，他们得出了各成分的平均纬度值（辐射平衡、蒸发热量损失、湍流热交换、通过洋流的热量重新分配）。这些发现已推广到大陆、海洋和整个地球。
AbstractThe observation program of the International Geophysical Year has provided new meteorological data that have made possible more precise computations of the heat balance of the earth. Greater accuracy has also been achieved through improvement or computation methods. Using data for 2,000 stations, including 300 points in ocean areas, the authors have constructed world maps for major components of the heat balance. From these maps they have derived mean latitudinal values of the components (radiation balance, loss of heat in evaporation, turbulent heat exchange, redistribution of heat through ocean currents). The findings have been generalized for continents, oceans and the earth as a whole.