The Model of Dependence of the Temperature of the Surface Layer of Atmosphere from the Earth's Albedo and Thermal Inertia of the Hydrosphere  

作　　者：Nikolay N. Zavalishin 

机构地区：[1]Siberian Regional Research,Hydrometeorological Institute,Sovetskaya str.,30,Novosibirsk 630099,Russia

出　　处：《Journal of Atmospheric Science Research》2018年第1期13-17,共5页大气科学研究（英文）

摘　　要：The assumption of M. Milankovich about the constancy of the Earth's albedo during the interglacial period was replaced with the alternative one. The model was developed where anomalies of the average annual temperature of the surface atmosphere were related with interannual changes in the planetary albedo and the thermal inertia of the hydrosphere. The surface temperature changes due to albedo actual and model changes were calculated. Possible external causes of albedo changes were considered.

关 键 词：Radiation imbalance Hemisphere's ALBEDO Milankovich theory Model extension Geospheres' heat balance Variability of the planetary ALBEDO NEAR-SURFACE ATMOSPHERE TEMPERATURE 

分 类 号：O4[理学—物理]