Evaluation of the MODIS (MOD10A1) daily snow albedo product over the Greenland ice sheet

被引:130
作者
Stroeve, Julienne C. [1 ]
Box, Jason E.
Haran, Terry
机构
[1] Univ Colorado, CIRES, NSIDC, Boulder, CO 80309 USA
[2] Ohio State Univ, Byrd Polar Res Ctr, Atmospher Sci Program, Columbus, OH 43210 USA
基金
美国国家航空航天局;
关键词
remote sensing; snow and ice; MODIS; Greenland ice sheet;
D O I
10.1016/j.rse.2006.06.009
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This study evaluates the performance of the beta-test MODIS (MOD10A1) daily albedo product using in situ data collected in Greenland during summer 2004. Results indicate the beta-test product tracks the general seasonal variability in albedo but exhibits significant more temporal variability than observed at the stations. This may indicate problems with the cloud detection algorithm, and/or failure of the BRDF model to adequately model the bidirectional reflectance of snow. Comparisons with in situ observations at five automatic weather stations in Greenland indicate an overall RMSE of 0.067 for the Terra instrument and an RMSE of 0.075 on Aqua. The Terra-retrieved-albedo are slightly better correlated with the in situ data than the Aqua retrievals (r=0.79 versus r=0.77). Comparisons were also made between the MODIS daily albedo product and the MODIS 16-day albedo product (MOD43133). Results indicate general correspondence between the two products, with better agreement found using the Terra-retrieved-albedo than the Aqua-retrieved albedo. The reason for the differences in albedo between the Aqua and Terra satellites remains unclear. At the stations examined, both the Terra and Aqua retrievals were made at nearly the same time of the day and therefore the differences in albedo between the satellites cannot be explained by differences in solar illumination. Finally, the albedo derived using MODIS data and the direct estimation algorithm (DEA) was also compared with 2004 Greenland in situ data. Results from this comparison suggest that the DEA performs well as long as the solar zenith angle of the observation is not greater than 70 degrees. (c) 2006 Elsevier Inc. All rights reserved.
引用
收藏
页码:155 / 171
页数:17
相关论文
共 32 条
[1]   Greenland ice sheet melt extent: 1979-1999 [J].
Abdalati, W ;
Steffen, K .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2001, 106 (D24) :33983-33988
[2]  
Box J., 1997, THESIS U COLORADO BO
[3]   Evaluation of Greenland ice sheet surface climate in the HIRHAM regional climate model using automatic weather station data [J].
Box, JE ;
Rinke, A .
JOURNAL OF CLIMATE, 2003, 16 (09) :1302-1319
[4]  
BOX JE, 1997, AGU FALL M DEC 1997
[5]  
FOWLER C, 2000, AVHRR POLAR PATHFIND
[6]   Validation of AVHRR- and MODIS-derived albedos of snow and ice surfaces by means of helicopter measurements [J].
Greuell, W ;
Oerlemans, J .
JOURNAL OF GLACIOLOGY, 2005, 51 (172) :37-48
[7]   MODIS snow-cover products [J].
Hall, DK ;
Riggs, GA ;
Salomonson, VV ;
DiGirolamo, NE ;
Bayr, KJ .
REMOTE SENSING OF ENVIRONMENT, 2002, 83 (1-2) :181-194
[8]   Consistency of MODIS surface bidirectional reflectance distribution function and albedo retrievals: 2. Validation [J].
Jin, YF ;
Schaaf, CB ;
Woodcock, CE ;
Gao, F ;
Li, XW ;
Strahler, AH ;
Lucht, W ;
Liang, SL .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2003, 108 (D5)
[9]   An overview of MODIS Land data processing and product status [J].
Justice, CO ;
Townshend, JRG ;
Vermote, EF ;
Masuoka, E ;
Wolfe, RE ;
Saleous, N ;
Roy, DP ;
Morisette, JT .
REMOTE SENSING OF ENVIRONMENT, 2002, 83 (1-2) :3-15
[10]   Development and validation of a snow albedo algorithm for the MODIS instrument [J].
Klein, AG ;
Stroeve, J .
ANNALS OF GLACIOLOGY, VOL 34, 2002, 2002, 34 :45-52