Simultaneous inversion of multiple land surface parameters from MODIS optical-thermal observations

被引:23
|
作者
Ma, Han [1 ]
Liang, Shunlin [1 ,2 ]
Xiao, Zhiqiang [1 ]
Shi, Hanyu [1 ]
机构
[1] Beijing Normal Univ, Fac Geog Sci, Coll Remote Sensing Sci & Engn, State Key Lab Remote Sensing Sci, Beijing 100875, Peoples R China
[2] Univ Maryland, Dept Geog Sci, College Pk, MD 20742 USA
基金
中国国家自然科学基金;
关键词
Radiative transfer; Multiple parameters; MODIS; Data assimilation; Land Surface Temperature (LST); Upwelling Longwave radiation (LWUP); LEAF-AREA INDEX; PHOTOSYNTHETICALLY ACTIVE RADIATION; TEMPERATURE RETRIEVAL; ALBEDO PRODUCT; SNOW-COVER; REFLECTANCE; EMISSIVITY; ALGORITHM; BAND; VEGETATION;
D O I
10.1016/j.isprsjprs.2017.04.007
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Land surface parameters from remote sensing observations are critical in monitoring and modeling of global climate change and biogeochemical cycles. Current methods for estimating land surface variables usually focus on individual parameters separately even from the same satellite observations, resulting in inconsistent products. Moreover, no efforts have been made to generate global products from integrated observations from the optical to Thermal InfraRed (TIR) spectrum. Particularly, Middle InfraRed (MIR) observations have received little attention due to the complexity of the radiometric signal, which contains both reflected and emitted radiation. In this paper, we propose a unified algorithm for simultaneously retrieving six land surface parameters - Leaf Area Index (LAI), Fraction of Absorbed Photosynthetically Active Radiation (FAPAR), land surface albedo, Land Surface Emissivity (LSE), Land Surface Temperature (LST), and Upwelling Longwave radiation (LWUP) by exploiting MODIS visible-to-TIR observations. We incorporate a unified physical radiative transfer model into a data assimilation framework. The MODIS visible-to-TIR time series datasets include the daily surface reflectance product and MIR-to-TIR surface radiance, which are atmospherically corrected from the MODIS data using the Moderate Resolution Transmittance program (MODTRAN, ver. 5.0). LAI was first estimated using a data assimilation method that combines MODIS daily reflectance data and a LAI phenology model, and then the LAI was input to the unified radiative transfer model to simulate spectral surface reflectance and surface emissivity for calculating surface broadband albedo and emissivity, and FAPAR. LST was estimated from the MIR-TIR surface radiance data and the simulated emissivity, using an iterative optimization procedure. Lastly, LWUP was estimated using the LST and surface emissivity. The retrieved six parameters were extensively validated across six representative sites with different biome types, and compared with MODIS, GLASS, and GlobAlbedo land surface products. The results demonstrate that the unified inversion algorithm can retrieve temporally complete and physically consistent land surface parameters, and provides more accurate estimates of surface albedo, LST, and LWUP than existing products, with R-2 values of 0.93 and 0.62, RMSE of 0.029 and 0.037, and BIAS values of 0.016 and 0.012 for the retrieved and MODIS albedo products, respectively, compared with field albedo measurements; R-2 values of 0.95 and 0.93, RMSE of 2.7 and 4.2 K, and BIAS values of -0.6 and -2.7 K for the retrieved and MODIS LST products, respectively, compared with field LST measurements; and R2 values of 0.93 and 0.94, RMSE of 18.2 and 22.8 W/m(2), and BIAS values of -2.7 and -14.6 W/m(2) for the retrieved and MODIS LWUP products, respectively, compared with field LWUP measurements. (C) 2017 International Society for Photogrammetry and Remote Sensing, Inc. (ISPRS). Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:240 / 254
页数:15
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