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硫酸盐气溶胶直接辐射效应在线与离线模拟方法的比较
引用本文:吴涧,蒋维楣,刘红年,王卫国,罗燕.硫酸盐气溶胶直接辐射效应在线与离线模拟方法的比较[J].气象学报,2004,62(4):486-492.
作者姓名:吴涧  蒋维楣  刘红年  王卫国  罗燕
作者单位:1. 云南大学资源环境与地球科学学院大气科学系,昆明,650091;南京大学大气科学系,南京,210093
2. 南京大学大气科学系,南京,210093
3. 云南大学资源环境与地球科学学院大气科学系,昆明,650091
基金项目:国家自然科学基金资助项目 (40 2 0 50 1 6和 40 1 650 0 1 ),云南省自然科学基金资助项目 (2 0 0 3D0 0 1 1 )
摘    要:利用区域气候模式RegCM 2与大气化学模式连接的模拟系统 ,比较了硫酸盐气溶胶辐射强迫的在线、离线模拟方法的硫酸盐柱含量、大气顶直接辐射强迫及地表温度响应。发现 :在线与离线模拟方法得到的硫酸盐柱含量、有无反馈大气顶直接辐射强迫和地表温度响应在许多地区有很大差异 ,这种差异在较小区域平均的尺度上更显著 ,在全区域平均尺度上也较为明显 ,是不能被忽略的 ;结果显示从硫酸盐含量到辐射强迫和地表温度响应逐渐加大的差异 ,说明硫酸盐气溶胶的辐射强迫与模拟方法有关 ,显示出较大的不确定性。

关 键 词:硫酸盐气溶胶  直接辐射强迫  地表温度响应  模拟方法比较
收稿时间:6/9/2003 12:00:00 AM
修稿时间:2003年6月9日

COMPARISON OF ON-LINE AND OFF-LINE SIMULATION METHODS FOR DIRECT RADIATIVE FORCING OF ANTHROPOGENIC SULFATE
Wu Jian,Jiang Weimei,Liu Hongnian,Wang Weiguo and Luo Yan.COMPARISON OF ON-LINE AND OFF-LINE SIMULATION METHODS FOR DIRECT RADIATIVE FORCING OF ANTHROPOGENIC SULFATE[J].Acta Meteorologica Sinica,2004,62(4):486-492.
Authors:Wu Jian  Jiang Weimei  Liu Hongnian  Wang Weiguo and Luo Yan
Institution:Department of Atmospheric Science, Yunnan University, Kunming 650091;Department of Atmospheric Science, Nanjing University, Nanjing 210093;Department of Atmospheric Science, Nanjing University, Nanjing 210093;Department of Atmospheric Science, Nanjing University, Nanjing 210093;Department of Atmospheric Science, Yunnan University, Kunming 650091;Department of Atmospheric Science, Yunnan University, Kunming 650091
Abstract:An on-line coupled regional climate and atmospheric chemical model system has been modified and used to compare the on-line and off-line methods for direct radiative forcing and climate response simulation of sulfate aerosol over China area under the same model system and the same polutant release inventory condition.The differences between sulfate column burden and TOA radiative forcing without climate response have been discussed based on four-month simulation,i.e.January,April,July and October in 2000.The results reveals the maximum difference of sulfate burden between online and off-line methods emerges in July,and the percentage ratio to on-line burden of the difference is less than 3% at the whole modeling area average scale,but there are about 13% to some regions.It has been concluded that the sulfate burden has less difference at large scale,but is obvious at regional scale.The radiative forcing at TOA without climate response has a variable range between-1.5 W/m2 and 1 W/m2 in the two methods,and positive value locates in the negative sulfate burden difference region.At the whole average scale,the difference of radiative forcing is about 11% to that of on-line result,but the difference is more than 30% to that of on-line result in the central and northern region.At the regional scale,the radiative forcing has been effected deeply by the model linking methods,and there is indeterminacy in regional scale radiative forcing.If climate response has been considered in the modeling,there would be-10-10 W/m2 difference between two TOA radiative forcing.Surface temperature response over China area have also been compared.The following results can be figured out based on the comparison:(1) It has been clarified that there is difference in most region between results of the on-line and off-line methods both in sulfate burden and in radiative forcing at TOA and in surface temperature response.The differences on each regional averaged results are more obvious than that of large scale averaged results,which is clear and cannot be neglected.(2) T he percentage deviation of sulfate burden between the two methods is smaler than that of radiative forcing at TOA,which is smaller than that of surface temperature response.The results show indet erminacy in radiative forcing of anthropogenic sulfate and climate responses when different model linking methods have been used.The modeling results depend on the model linking methods deeply at regional scale level even,which should be emphasized in the future research work.
Keywords:Sulfate aerosol  Direct radiative forcing  Surface temperature response  Comparison of simulation methods  
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