2003-2010年青藏高原积雪及雪水当量的时空变化

被引:39
作者
孙燕华 [1 ]
黄晓东 [1 ]
王玮 [1 ]
冯琦胜 [1 ]
李红星 [2 ]
梁天刚 [1 ]
机构
[1] 兰州大学草地农业科技学院草地农业生态系统国家重点实验室
[2] 中国科学院寒区旱区环境与工程研究所
关键词
MODIS; 积雪面积; 雪水当量; 青藏高原;
D O I
暂无
中图分类号
P426.635 [];
学科分类号
摘要
利用MODIS逐日无云积雪产品与AMSR-E雪水当量产品进行融合,获取了青藏高原500 m分辨率的高精度雪水当量产品,通过研究青藏高原积雪时空动态变化特征,分析了积雪覆盖日数、雪水当量以及总雪量的季节及年际变化.结果表明:青藏高原地区降雪主要集中在高海拔山区,而高原腹地降雪较少,降雪在空间上分布极为不均;2003-2010年期间,平均积雪日数呈显著减少趋势,稳定积雪区面积在逐渐扩大,常年积雪区面积在不断缩小.与积雪日数时空变化相比,雪水当量增加的区域与积雪日数增加的区域基本一致,但喜马拉雅山脉在积雪日数减少的情况下雪水当量却在逐年增加,表明该地区温度升高虽然导致部分常年积雪向季节性积雪过渡,但降雪量却在增加.总的积雪面积年际变化呈波动下降的趋势,但趋势不显著,且减少的比例很少.最大积雪面积呈现波动上升后下降的趋势,平均累积积雪总量呈明显的波动下降趋势,年递减率为1.0×103m3·a-1.
引用
收藏
页码:1337 / 1344
页数:8
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