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火山喷发对辐射传输影响的研究
引用本文:周清波.火山喷发对辐射传输影响的研究[J].地理研究,1993,12(3):19-25.
作者姓名:周清波
作者单位:中国科学院、国家计划委员会地理研究所
摘    要:本文根据火山灰粒子的辐射光学特性,计算了火山灰粒子和平流层本底的辐射光学参数。另外,采用大气多次散射的辐射传输方程,计算了火山喷发对大气辐射变温的影响效果。结果表明,与平流层本底相比,火山灰粒子具有很强的吸收性。火山喷发使平流层吸收太阳辐射增温,并使到达对流层和地面的太阳辐射减少;同时,对大气长波冷却率的影响甚微。

关 键 词:火山喷发  大气辐射传输  太阳辐射加热率  大气长波冷却率  
收稿时间:1992-03-26
修稿时间:1992-11-02

A STUDY ON THE INFLUENCE OF VOLCANIC ERUPTION ON ATMOSPHERIC RADIATION TRANSFER
Zhon Qingbo.A STUDY ON THE INFLUENCE OF VOLCANIC ERUPTION ON ATMOSPHERIC RADIATION TRANSFER[J].Geographical Research,1993,12(3):19-25.
Authors:Zhon Qingbo
Institution:Institute of Geography, Chinese Academy of Sciences and State Planning Commission of the People''s Republic of China
Abstract:According to the radiation-optical quality of volcanic ash we calculated the parameter of radiation-optic. Meanwhile, by using the equation of atmospheric radiation transfer, and the change rate of. temperature was calcuJated.The result is as follows. The absorbant ability of volca'nic ash is stronger than it of the background of stratosphere. Valcanic eruption witl heat the stratosplere by absorbing solar radiation, decrease the solar radiation on the earth surface, and have no effect on long wave radiative cooling rate.
Keywords:Volcanic eruption  Atmospheric radiation transfer  Solar radiation heating rate  Atmosporic long wave cooling rate
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