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穆松宁, 周广庆. 欧亚大陆季节增(融)雪盖面积变化特征分析[J]. 气候与环境研究, 2009, 14(5): 491-508. DOI: 10.3878/j.issn.1006-9585.2009.05.05
引用本文: 穆松宁, 周广庆. 欧亚大陆季节增(融)雪盖面积变化特征分析[J]. 气候与环境研究, 2009, 14(5): 491-508. DOI: 10.3878/j.issn.1006-9585.2009.05.05
Analyses of Seasonal Fresh Snow Extent over Northern Eurasia[J]. Climatic and Environmental Research, 2009, 14(5): 491-508. DOI: 10.3878/j.issn.1006-9585.2009.05.05
Citation: Analyses of Seasonal Fresh Snow Extent over Northern Eurasia[J]. Climatic and Environmental Research, 2009, 14(5): 491-508. DOI: 10.3878/j.issn.1006-9585.2009.05.05

欧亚大陆季节增(融)雪盖面积变化特征分析

Analyses of Seasonal Fresh Snow Extent over Northern Eurasia

  • 摘要: 利用美国冰雪资料中心(National Snow and Ice Data Center)提供的近40 年逐周的卫星反演雪盖资料,定义了各季节新增(融化)雪盖面积指数(fresh snow extent),即增/融雪覆盖率PFSE、增/融雪面积AFSE、欧亚大陆北部增/融雪面积之和TFSE,针对欧亚大陆各季节平均的雪盖面积本身(snow extent,PSE、ASE、TSE)和其增(融)雪盖面积,分析比较了二者的变化特征。结果表明,欧亚大陆各季节平均的雪盖面积和相应增(融)雪盖面积不论是气候态分布还是其年际、十年际变化均有明显不同,其中以冬、春季差别更为明显;夏、秋季二者虽有较好的一致性,但增(融)雪盖面积的变率明显强于雪盖面积本身;另外,冬季欧洲新增雪盖对欧亚北部冬季雪盖面积以及其后的春季雪盖都有较显著的影响,而春季欧洲和中纬度亚洲地区的融雪则受到冬、春两季雪盖情况的影响。进一步分析欧亚大陆冬、春两季增(融)雪盖与ENSO 关系显示,二者除在个别地区(西伯利亚北部、欧洲中东部以及青藏高原)存在较明显关系外,整体上,欧亚大陆北部雪盖变化既不受控于ENSO,也不会显著影响ENSO。

     

    Abstract: Using weekly snow cover data (Version 3) during 1966-2005 from the National Snow and Ice Data Center, new indexes for the seasonal fresh snow extent are defined: Percent of fresh snow extent (PFSE), area of fresh snow extent (AFSE) and total AFSE over northern Eurasia (TFSE). Then, the analyses are performed based on the new indexes and seasonal mean snow extent index (PSE, ASE, and TSE) to investigate the snow cover characteristics over Eurasia. The results show that the distinguished differences for the spatial distributions and temporal variations fromAFSE and ASE are observed from seasonal to decadal time scales, particularly in winter and spring. The variabilities of PFSE are stronger than those of PSE although their temporal and spatial distributions in summer and autumn are more consistent than in winter and spring. The winter AFSE in Europe is found to have close relations with TFSEand TSEin winter and the subsequent spring, and the spring AFSE in Europe and midlatitude Asia is controlled by the snow cover status both in winter and spring. Further analysis indicates that the fresh snow extent in winter and spring is independent of ENSO in general, except for some small regions in northern Siberia, mideastern Europe and Tibet.

     

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