Effect of Thin High Clouds and Aerosol Layers on the Heating and Dissipation of Low-level Clouds in the Arctic

被引：0

作者：

Belikov, Yu E. ^{[1
]}

Dyshlevsky, S., V ^{[1
]}

Repin, A. Yu ^{[1
]}

机构：

[1] Fedorov Inst Appl Geophys, Ul Rostokinskaya 9, Moscow 129128, Russia

来源：

RUSSIAN METEOROLOGY AND HYDROLOGY | 2021年 / 46卷 / 04期

基金：

俄罗斯基础研究基金会;

关键词：

the Arctic; climate; radiative transfer; aerosol layers; cloud dissipation; ice cover melting; ULTRAVIOLET-RADIATION; VOLCANIC AEROSOLS; SURFACE;

D O I：

10.3103/S1068373921040051

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

Based on the radiative transfer simulation and analysis of observational data on cloudiness, temperature, and humidity in the Arctic atmosphere in the years of the increased ice melting, a hypothesis is proposed on the effect of thin high clouds and aerosol layers on the heating and dissipation of low-level clouds in the Arctic. Along with the effect of thin high scattering layers on the transmission of solar radiation by tropospheric clouds, the dissipation of low-level clouds in the years of the increased ice melting can be one of the main mechanisms of the natural warming in the Arctic.

引用

页码：245 / 255

页数：11

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