长江流域资源与环境 >> 2016, Vol. 25 >> Issue (03): 486-496.doi: 10.11870/cjlyzyyhj201603016
潘鑫1,2,3, 刘元波1,2
PAN Xin1,2,3, LIU Yuan-bo1,2
摘要: 本文采用统计相关分析、Morlet小波分析、Rodionov时间序列分析与GIS空间分析等技术方法,分析了1983年7月至2012年9月长江流域SRB和CERES地表净辐射月产品的时空变化特征。结果表明:拟合后遥感产品比气象辐射站点观测值整体高15.8%,平均误差为15.31 W/m2,均方根误差为21.58 W/m2。长江流域地表净辐射多年均值为78.0 W/m2,整体呈下降趋势,于1996年突降,存在16年和10年周期;季相上,呈夏 > 春 > 秋 > 冬。空间上,呈现西部地区 > 东部地区 > 中部地区;1996~2012年相较1983~1995年净辐射整体下降,其中上游流域降幅大于中下游;净辐射降低主要出现在5~7月,降幅较大地区主要是长江上游流域部分地区和长江中游流域纬度较低地区。研究结果对于认识长江流域的气候变化条件下的能量和水分循环过程等具有重要意义。
中图分类号:
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