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青藏高原地区MODIS反照率的精度分析
引用本文:陈爱军,梁学伟,卞林根,刘玉洁,王飞,朱小祥.青藏高原地区MODIS反照率的精度分析[J].南京气象学院学报,2012(6):664-672.
作者姓名:陈爱军  梁学伟  卞林根  刘玉洁  王飞  朱小祥
作者单位:[1]南京信息工程大学气象灾害省部共建教育部重点实验室,江苏南京210044 [2]南京信息工程大学大气物理学院,江苏南京210044 [3]中国气象科学研究院,北京100081 [4]国家卫星气象中心,北京100081 [5]国家气象中心,北京100081
基金项目:国家自然科学基金资助项目(40875015);江苏高校优势学科建设工程资助项目(PAPD)
摘    要:应用2002-2004年青藏高原CAMP/Tibet试验期间4个地面站点的反照率观测结果定量分析Te丌aMODISlkm分辨率短波SW波段(0.3—5.0μm)反照率全反演结果和当量反演结果的精度。对于全反演结果,黑空反照率、白空反照率与地面观测结果的均方根差分别为0.0187和0.0168;对于当量反演结果,黑空反照率、白空反照率与地面观测结果的均方根差分别为0.0766和0.0761。综合全反演结果和当量反演结果,则黑空反照率、白空反照率与地面观测结果的均方根差分别为0.0679和0.0675。当地面观测结果与MODIS反照率当量反演结果均为“无雪”状态时,黑空反照率、白空反照率与地面观测结果的均方根差分别为0.0352和0.0364;当地面观测结果为“积雪”状态,MODIS反照率当量反演结果为“无雪”状态时,黑空反照率、白空反照率与地面观测结果的均方根差分别高达0.1556和0.1541。

关 键 词:反照率  验证  MODIS  青藏高原

Assessment on the accuracy of MODIS albedos over the Tibetan Plateau
CHEN mi-jun,LIANG Xue-wei,BIAN Lin-gen,LIU Yu-jie,WANG Fei,ZHU Xiao-xiang.Assessment on the accuracy of MODIS albedos over the Tibetan Plateau[J].Journal of Nanjing Institute of Meteorology,2012(6):664-672.
Authors:CHEN mi-jun  LIANG Xue-wei  BIAN Lin-gen  LIU Yu-jie  WANG Fei  ZHU Xiao-xiang
Institution:1. Key Laboratory of Meteorological Disaster of Ministry of Education, NUIST, Nanjing 210044, China; 2. School of Atmospheric Physics,NUIST, Nanjing 210044, China ;3. Chinese Academy of Meteorological Sciences, Beijing 100081, China 4. National Satellite Meteorological Center, Beijing 100081, China; 5. National Meteorological Center, Beijing 100081, China )
Abstract:Using ground-observed albedos from four stations over the Tibetan Plateau from 2002 to 2004 in the CAMP/Tibet experiments, the accuracies of Terra MODIS ( MODerateesolution Imaging Spectroradiometer) shortwave bands(0. 3-5.0 μ m) albedos in 1 km resolution derived with the full inversion and the magnitude inversion are individually quantitatively assessed. When MODIS albedos are derived with the full inversion,the root-mean-square errors(RMSEs) between the ground-observed albedos and the black-sky albedos(BSA) ,and the white-sky albedos(WSA) are 0. 018 7 and 0. 016 8 ,respectively; when MODIS albedos are derived with the magnitude inversion, they are 0. 076 6 and 0. 076 1, respectively. And, when MODIS albedos derived with the full inversion and the magnitude inversion are all included, the RMSEs are 0. 067 9 and 0. 067 5, respectively. When the ground-observed albedos and MODIS albedos derived with the magnitude inversion are both from the no-snow condition, RMSEs between the ground-observed albedos and BSA, and WSA derived with the magnitude inversion are 0. 035 2 and 0. 036 4, respectively. However, when the ground-observed albedos are fromthe snowy condition, while MODIS albedos derived with the magnitude inversion are from the no-snow condition,RMSEs between the ground-observed albedos and BSA, and WSA derived with the magnitude inversion are 0. 155 6 and 0. 154 1.
Keywords:albedo  validation  MODIS  Tibetan Plateau
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