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平流层温度调整后的辐射强迫的简化计算
引用本文:于秀兰,石广玉. 平流层温度调整后的辐射强迫的简化计算[J]. 高原气象, 2001, 20(3): 271-274
作者姓名:于秀兰  石广玉
作者单位:中国科学院大气物理研究所LASG,;中国科学院大气物理研究所LASG,
基金项目:国家“九五”重中之重科技攻关项目“我国短期气候预测系统的研究”( 96 90 8 0 1 0 6)资助
摘    要:采用石广玉[1] 一维辐射对流模式对温室气体浓度变化引起的平流层温度调整后的辐射强迫(ARF)进行了计算。参考文献 [1]的瞬时辐射强迫 (IRF)计算的简化公式的形式 ,将ARF的计算结果表示成简单的经验公式。与使用一维辐射对流模式计算得出的ARF结果的比较表明 ,简化计算公式可以达到很高的精度。

关 键 词:调整后的辐射强迫  简化计算  一维辐射对流模式
文章编号:1000-0534(2001)03-0271-04
修稿时间:2000-12-13

Simplified Calculation of Radiative Forcing with Adjusted Stratosphere Temperature
YU Xiu|lan, SHI Guang|yu. Simplified Calculation of Radiative Forcing with Adjusted Stratosphere Temperature[J]. Plateau Meteorology, 2001, 20(3): 271-274
Authors:YU Xiu|lan   SHI Guang|yu
Abstract:Adjusted radiative forcing due to greenhouse gases is calculated in this paper using Shi (1991)'s 1|RCM. The 1|D radiation|convection model results can be expressed with simple empirical formula, which is fast and has reasonable precision. It is to be special noted that the formulae in IPCC(1990) and Shi (1992) were given in IPCC (1994). However, both of them are calculations based on IRF, so it's necessary to find the simplified calculation equations for ARF. Moreover, the simplified empirical equations are given out for ARF results refer to those of IRF given by Shi in 1991. And the comparison with the results calculated with 1|RCM shows that our simplified formulae could provide good accuracy.
Keywords:Adjusted radiative forcing  Simplified formulae  1|RCM
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