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FY-3A/MERSI海上沙尘天气气溶胶光学厚度反演 总被引：1，自引：1，他引：0
利用FY-3A/MERSI资料,结合MODIS C005算法的海上气溶胶模型,研究了中国渤海、黄海以及东海海域沙尘天气气溶胶光学厚度反演方法。通过MERSI反演的气溶胶光学厚度与MODIS C005气溶胶光学厚度产品(MOD04)对比,发现MERSI气溶胶光学厚度反演结果存在较大偏差。分析认为,这种偏差是由MODIS C005算法的海上气溶胶模型对MERSI气溶胶光学厚度反演不完全适用造成的。鉴于此,本文研究引进了一种沙尘气溶胶模型,并将其与MODIS C005算法的粗粒子气溶胶模型按照一定比例混合,形成了改进的气溶胶模型。利用改进气溶胶模型再次反演海上沙尘天气气溶胶光学厚度,反演结果与MOD04一致性较好,说明改进气溶胶模型能有效地提高MERSI定量反演沙尘气溶胶的能力。 相似文献
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Combined with TRMM products and Tropical Cyclone (TC) best track data in Northwest Pacific from 1 January 2003 to 31 December 2009, a total of 118 TCs, including 336 instantaneous TC precipitation observations are established as the TRMM TC database, and the database is stratified into four intensity classes according to the standard of TC intensity adopted by China Meteorological Administration (CMA): Severe Tropical Storm (STS), Typhoon (TY), Severe Typhoon (STY) and Super Typhoon (SuperTY). For each TC snapshot, the mean rainfall distribution is computed using 10-km annuli from the TC center to a 300-km radius, then the axisymmetric component of TC rainfall is represented by the radial distribution of the azimuthal mean rain rate; the mean rain rates, rain types occurrence and contribution proportion are computed for each TC intensity class; and the mean quadrantal distribution of rain rates along TCs motion is analyzed. The result shows that: (1) TCs mean rain rates increase with their intensity classes, and their radial distributions show single-peak characteristic gradually, and furthermore, the characteristics of rain rates occurrence and contribution proportion change from dual-peak to single-peak distribution, with the peak rain rate at about 5.0 mm/h; (2) Stratiform rain dominate the rain type in the analysis zone, while convective rain mainly occurred in the eye-wall region; (3) The values of mean rain rate in each quadrant along TCs motion are close to each other, relatively, the value in the right-rear quadrant is the smallest one. 相似文献
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为了更好掌握西北太平洋热带气旋(Tropical Cyclone, TC)降水的分布特征,将2003—2009年TRMM资料同TC最佳路径数据集相匹配,共得到这7年中118个TC的336时次个例,包括强热带风暴、台风、强台风和超强台风4种强度等级样本,建立了TRMM卫星监测西北太平洋TC的样本数据库。在此基础上,选取距TC中心300 km范围为研究区域,每间隔10 km为圆环计算其降雨方位平均值,对各等级TC平均地表降雨率的径向分布、不同降雨率和降水类型的平均出现频率和降水贡献比例以及沿TC移动方向上各象限平均降雨率分布等特征进行统计分析,研究结果表明:(1) 随着强度等级的增加,TC平均地表降雨率逐渐增加,并在径向方向上表现出单峰型分布特征,降水出现频率和贡献比例的峰值也逐渐向8 mm/h附近的峰值靠拢;(2) 层性降水在研究区域内占统治地位,而对流性降水主要集中在眼壁附近;(3) 各象限平均降雨率相差不大,相对而言,沿TC移动的前侧降雨率更大,而右后侧最小。 相似文献
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