Comparison of MOD16 and LSA-SAF MSG evapotranspiration products over Europe for 2011

被引:150
作者
Hu, Guangcheng [1 ]
Jia, Li [1 ]
Menenti, Massimo [2 ]
机构
[1] Chinese Acad Sci, Inst Remote Sensing & Digital Earth, State Key Lab Remote Sensing Sci, Beijing 100101, Peoples R China
[2] Delft Univ Technol, Delft, Netherlands
基金
国家高技术研究发展计划(863计划);
关键词
Evapotranspiration; MOD16; LSA-SAF MSG ETa; Intercomparison; LAND-SURFACE EVAPORATION; BALANCE SYSTEM SEBS; TIME-SERIES; IMPROVING EVAPOTRANSPIRATION; STOMATAL-RESISTANCE; SPATIAL-RESOLUTION; TERRESTRIAL GROSS; SOLAR-RADIATION; ECMWF MODEL; FLUX TOWER;
D O I
10.1016/j.rse.2014.10.017
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Terrestrial actual evapotranspiration (ETa) is an important component of the terrestrial water cycle. Currently there are two operational ETa products using moderate spatial resolution remote sensing data at continental and global scales, i.e. MOD16 and LSA-SAF MSG ETa These two products are based on different parameterizations and forcing data, with the spatial and temporal resolutions of 1-km/8-day and 5-km/daily for MOD16 and LSA-SAF MSG ETa respectively. We compared the MOD16 ETa and LSA-SAF MSG ETa products and evaluated them against in-situ measurements at 15 ground sites with biome types ranging from croplands, grasslands, shrublands, savannas, to forests over Europe for 2011. The intercomparison results at local scale demonstrate that LSA-SAF MSG ETa is closer to eddy covariance (EC) measurements than MOD16 ETa product, with larger correlation coefficient Rest-obs, smaller root mean square error RMSEest-obs and bias of LSA-SAF MSG vs. EC at most of the 15 flux sites. Spatial distributions of the RMOD16-MSG and RMSEMOD16-MSG between MOD16 and LSA-SAF MSG ETa for 2011 show that both ETa data products are consistent over most of Europe, except for some semi-arid regions where the water availability is the main limiting factor of land surface evapotranspiration. LSA-SAF MSG ETa is shown to have a more adequate response to the forest fire. Our study contributes to assess the quality and uncertainty of each product, which can be beneficial for improving ETa algorithm and product quality. (C) 2014 Elsevier Inc. All rights reserved.
引用
收藏
页码:510 / 526
页数:17
相关论文
共 94 条
[1]   Soil Moisture Analyses at ECMWF: Evaluation Using Global Ground-Based In Situ Observations [J].
Albergel, C. ;
de Rosnay, P. ;
Balsamo, G. ;
Isaksen, L. ;
Munoz-Sabater, J. .
JOURNAL OF HYDROMETEOROLOGY, 2012, 13 (05) :1442-1460
[2]  
[Anonymous], 2001, GLOBAL CHANGE BIOL
[3]   A Revised Hydrology for the ECMWF Model: Verification from Field Site to Terrestrial Water Storage and Impact in the Integrated Forecast System [J].
Balsamo, Gianpaolo ;
Viterbo, Pedro ;
Beljaars, Anton ;
van den Hurk, Bart ;
Hirschi, Martin ;
Betts, Alan K. ;
Scipal, Klaus .
JOURNAL OF HYDROMETEOROLOGY, 2009, 10 (03) :623-643
[4]   Surface energy balance and actual evapotranspiration of the transboundary Indus Basin estimated from satellite measurements and the ETLook model [J].
Bastiaanssen, W. G. M. ;
Cheema, M. J. M. ;
Immerzeel, W. W. ;
Miltenburg, I. J. ;
Pelgrum, H. .
WATER RESOURCES RESEARCH, 2012, 48
[5]  
Bastiaanssen WGM, 1998, J HYDROL, V212, P198, DOI [10.1016/S0022-1694(98)00253-4, 10.1016/S0022-1694(98)00254-6]
[6]   THE SENSITIVITY OF WINTER EVAPORATION TO THE FORMULATION OF AERODYNAMIC RESISTANCE IN THE ECMWF MODEL [J].
BELJAARS, ACM ;
VITERBO, P .
BOUNDARY-LAYER METEOROLOGY, 1994, 71 (1-2) :135-149
[7]  
BENMEHREZ M, 1992, AGR FOREST METEOROL, V58, P285, DOI 10.1016/0168-1923(92)90066-D
[8]   A comparison of data sources for creating a long-term time series of daily gridded solar radiation for Europe [J].
Bojanowski, Jedrzej S. ;
Vrieling, Anton ;
Skidmore, Andrew K. .
SOLAR ENERGY, 2014, 99 :152-171
[9]  
Brutsaert W., 1982, EVAPORATION ATMOSPHE, DOI DOI 10.1007/978-94-017-1497-6
[10]   Remote sensing-based soil water balance to estimate Mediterranean holm oak savanna (dehesa) evapotranspiration under water stress conditions [J].
Campos, Isidro ;
Villodre, Julio ;
Carrara, Arnaud ;
Calera, Alfonso .
JOURNAL OF HYDROLOGY, 2013, 494 :1-9