检索规则说明:AND代表“并且”;OR代表“或者”;NOT代表“不包含”;(注意必须大写,运算符两边需空一格)
检 索 范 例 :范例一: (K=图书馆学 OR K=情报学) AND A=范并思 范例二:J=计算机应用与软件 AND (U=C++ OR U=Basic) NOT M=Visual
机构地区:[1]中国科学院大气物理研究所
出 处:《遥感技术与应用》1995年第2期1-8,共8页Remote Sensing Technology and Application
基 金:国家自然科学青年基金;中国博士后基金
摘 要:在仅有消光信息可利用的大气气溶胶观测资料处理过程中,需要寻找一种合理的反演复折射指数的方法。通过理论分析认为,Fymat消光比方法有潜在的反演不稳定性,经多种粒度谱的数值试验分析,认为消光比方法反演大气气溶胶复折射率,仅对特殊粒子谱型较为有效,而消光差方法却表现出适用谱分布广和具有良好精度的特点。用此方法反演出了中国科学院长春净月潭遥惑试验场1990年和1991年不同能见度下大气气溶胶的复折射率。对大气辐射传输计算,地物遥感大气订正,气溶胶的气候效应研究方面有参考价值。In the processing of atmospheric aerosol observations from the information of spectralextinction is only available,It is necessary to find a reasonable method of retrieving com-plex refractive index. This paper presents from theoretical analyses that there is a potentialinstability in Fymat’s extinction ratio method for the retrieval purpose. It is shown by thenumerical test with various aerosol size distribution that the extinction ratio method for re-trieving the refractive index is valid only for some particular types of the size distributions,and a new one,extinction difference method,presented in this paper however,can be appli-cable with broad sorts of aerosol size distributions and can work in good precision. As anexample of application,the extinction difference method is used to retrieve the complex re-fractive index of real atmospheric aerosols on certain visibility levels in 1990 and 1991 ob-served in Changchun Jingyuetan Remote Sensing Test of Academia Sinica. The resultswould be of particular value for researches in atmospheric radiation transfer model,atmo-spheric correction in remote sensing of earth surface,and the effect of atmospheric aerosols on climate.
分 类 号:P421.2[天文地球—大气科学及气象学]
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在链接到云南高校图书馆文献保障联盟下载...
云南高校图书馆联盟文献共享服务平台 版权所有©
您的IP:216.73.216.49