Estimation of sensible heat flux using the Surface Energy Balance System (SEBS) and ATSR measurements

被引:120
|
作者
Jia, L
Su, ZB
van den Hurk, B
Menenti, M
Moene, A
De Bruin, HAR
Yrisarry, JJB
Ibanez, M
Cuesta, A
机构
[1] Univ Wageningen & Res Ctr, ALTERRA Green World Res, NL-6700 AA Wageningen, Netherlands
[2] Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Lanzhou 730000, Peoples R China
[3] Royal Netherlands Meteorol Inst, NL-3730 AE De Bilt, Netherlands
[4] Univ Strasbourg 1, TRIO LSIIT, F-67400 Illkirch Graffenstaden, France
[5] Univ Wageningen & Res Ctr, Meteorol & Air Qual Grp, NL-6707 AB Wageningen, Netherlands
[6] Serv Invest & Desarrollo Tecnol, Badajoz, Spain
[7] Univ Lleida, Dept Medi Ambient & Ciencies Sol, Lleida, Spain
[8] Univ Castilla La Mancha, Dept Prod Vegetal & Tecnol Agr, Escuela Tecn Super Ingn Agron, E-13071 Ciudad Real, Spain
关键词
SEBS; ATSR; sensible heat flux; LAS;
D O I
10.1016/S1474-7065(03)00009-3
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This paper describes a modified version of the Surface Energy Balance System (SEBS) as regards the use of radiometric data from space and presents the results of a large area validation study on estimated sensible heat flux, extended over several months. The improvements were made possible by the characteristics of the Along Track Scanning Radiometer (ATSR-2) on board the European Remote Sensing satellite (ERS-2) and relate to: (a) the use of bi-angular radiometric data in two thermal infrared channels to estimate column atmospheric water vapor: (b) the use of bi-angular radiometric data in four spectral channels in the 550-1600 nm spectral regions to estimate aerosols optical depth: (c) determination of bottom of atmosphere (BOA) spectral reflectance using column water vapor, aerosols optical depth and a two-stream radiative transfer scheme to relate BOA spectral reflectance to top of atmosphere spectral radiance (d) direct and inverse modeling of radiative transfer in a vegetation canopy to relate BOA spectral reflectance to canopy properties, such as spectrally integrated hemispherical reflectance (albedo). A parameterization of the aerodynamic resistance for heat transfer (in term of kB(-1)) was applied for the first time at large spatial scales. For such large area analyses SEBS requires wind speed, potential temperature and humidity of air at an appropriate reference height. The latter was taken as being the height of the planetary boundary layer (PBL) and the data used were fields generated by an advanced numerical weather prediction model, i.e. regional atmospheric climate model (RACMO), integrated over the PBL. Validation of estimated sensible heat flux H obtained with the ATSR radiometric data was done using long-range, line-averaged measurements of H done with large aperture scintillometers (LAS) located at three sites in Spain and operated continuously between April and September 1999. The root mean square deviation of SEBS H estimates from LAS H measurements was 25.5 W m(-2). (C) 2003 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:75 / 88
页数:14
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