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作 者:白鸿涛[1] 陈勇航[1] 冯建东[2] 黄建平[3] 张文煜[3] 张强[4] 郭铌[4] 王胜[4]
机构地区:[1]东华大学环境科学与工程学院,上海201620 [2]四川省农业气象中心,四川成都610072 [3]兰州大学大气科学学院,甘肃兰州730000 [4]中国气象局兰州干旱研究所,甘肃兰州730002
出 处:《光学学报》2010年第4期928-934,共7页Acta Optica Sinica
基 金:国家973计划(2006CB400501);国家自然科学基金(40830957);国家科技支撑计划重点项目(2008BAC40B04)资助课题
摘 要:参照MODIS遥感陆地上空气溶胶第二代算法(C005-L),利用黄土高原半干旱地区(AERONET)(兰州大学半干旱气候与环境观测站,SACOL)的实测资料,基于6S大气辐射传输模式,分别用构建的SACOL气溶胶模型和6S的大陆型气溶胶模型对MODIS/Terra资料进行大气订正,得到了SACOL区域春季可见光通道和近红外通道的地表反射率以及0.66vs2.12和0.47vs0.66地表反射率简单关系式,并验证了三个通道的地表反射率关系及其随散射角和植被指数的变化。结果表明,0.47vs0.66通道地表反射率关系比0.47vs2.12通道地表反射率关系的相关性和稳定性更大,0.47vs2.12地表反射率关系与散射角的相关性不大。According to the second-generation(Moderate-resolution imaging spectroradiometer,MODIS) retrieval algorithm of aerosol properties over land(C005-L),the atmospheric correction of MODIS/Terra data at Semi-arid climate and environment observatory of lanzhou university(SACOL) of(Aerosol robotic network,AERONET) in the semi-arid region of the Loess Plateau was performed by respectively using the SACOL aerosol model based on surface observation and the continental aerosol model used in 6S.The surface reflectances of the visible and near-infrared channels of the SACOL area were obtained and the 0.66vs2.12 and 0.47vs0.66 surface reflectance relation and their change with scattering angle and vegetation index were verified.The results show that the correlation of surface reflectances between 0.47μm and 0.66μm is stronger and more stable than the one between 0.47μm and 2.12μm; the surface reflectance relation of 0.47vs2.12μm is not dependent on scattering angle.
分 类 号:P407.1[天文地球—大气科学及气象学]
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