Development and evaluation of a cloud-gap-filled MODIS daily snow-cover product

被引:192
|
作者
Hall, Dorothy K. [1 ]
Riggs, George A. [1 ,2 ]
Foster, James L. [3 ]
Kumar, Sujay V. [3 ,4 ]
机构
[1] NASA, Goddard Space Flight Ctr, Cryospher Sci Branch, Greenbelt, MD 20771 USA
[2] Sci Syst & Applicat Inc, Greenbelt, MD 20771 USA
[3] NASA, Goddard Space Flight Ctr, Hydrol Sci Branch, Greenbelt, MD 20771 USA
[4] Sci Applicat Int Corp, Greenbelt, MD 20771 USA
关键词
MODIS; Snow cover; SWE; Data assimilation; LIS; INTERACTIVE MULTISENSOR SNOW; LAND INFORMATION-SYSTEM; SURFACE MODEL; SATELLITE; TIME; VARIABILITY; COMBINATION; STREAMFLOW; FRAMEWORK; DEPLETION;
D O I
10.1016/j.rse.2009.10.007
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The utility of the Moderate Resolution Imaging Spectroradiometer (MODIS) snow-cover products is limited by cloud cover which causes gaps in the daily snow-cover map products. We describe a cloud-gap-filled (CGF) daily snow-cover map using a simple algorithm to track cloud persistence, to account for the uncertainty created by the age of the snow observation. Developed from the 0.05 degrees resolution climate-modeling grid daily snow-cover product, MOD10C1, each grid cell of the CGF map provides a cloud-persistence count (CPC) that tells whether the current or a prior day was used to make the snow decision. Percentage of grid cells "observable" is shown to increase dramatically when prior days are considered. The effectiveness of the CGF product is evaluated by conducting a suite of data assimilation experiments using the community Noah land surface model in the NASA Land Information System (LIS) framework. The Noah model forecasts of snow conditions, such as snow-water equivalent (SWE). are updated based on the observations of snow cover which are obtained either from the MOD10C1 standard product or the new CGF product. The assimilation integrations using the CGF maps provide domain-averaged bias improvement of similar to 11%, whereas such improvement using the standard MOD10C1 maps is similar to 3%. These improvements suggest that the Noah model underestimates SWE and snow depth fields, and that the assimilation integrations contribute to correcting this systematic error. We conclude that the gap-filling strategy is an effective approach for increasing cloud-free observations of snow cover. (C) 2009 Elsevier Inc. All rights reserved.
引用
收藏
页码:496 / 503
页数:8
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