DocumentCode :
1460419
Title :
The SMOS Soil Moisture Retrieval Algorithm
Author :
Kerr, Yann H. ; Waldteufel, Philippe ; Richaume, Philippe ; Wigneron, Jean Pierre ; Ferrazzoli, Paolo ; Mahmoodi, Ali ; Al Bitar, Ahmad ; Cabot, François ; Gruhier, Claire ; Juglea, Silvia Enache ; Leroux, Delphine ; Mialon, Arnaud ; Delwart, Steven
Author_Institution :
CESBIO, Univ. Toulouse, Toulouse, France
Volume :
50
Issue :
5
fYear :
2012
fDate :
5/1/2012 12:00:00 AM
Firstpage :
1384
Lastpage :
1403
Abstract :
The Soil Moisture and Ocean Salinity (SMOS) mission is European Space Agency (ESA´s) second Earth Explorer Opportunity mission, launched in November 2009. It is a joint program between ESA Centre National d´Etudes Spatiales (CNES) and Centro para el Desarrollo Tecnologico Industrial. SMOS carries a single payload, an L-Band 2-D interferometric radiometer in the 1400-1427 MHz protected band. This wavelength penetrates well through the atmosphere, and hence the instrument probes the earth surface emissivity. Surface emissivity can then be related to the moisture content in the first few centimeters of soil, and, after some surface roughness and temperature corrections, to the sea surface salinity over ocean. The goal of the level 2 algorithm is thus to deliver global soil moisture (SM) maps with a desired accuracy of 0.04 m3/m3. To reach this goal, a retrieval algorithm was developed and implemented in the ground segment which processes level 1 to level 2 data. Level 1 consists mainly of angular brightness temperatures (TB), while level 2 consists of geophysical products in swath mode, i.e., as acquired by the sensor during a half orbit from pole to pole. In this context, a group of institutes prepared the SMOS algorithm theoretical basis documents to be used to produce the operational algorithm. The principle of the SM retrieval algorithm is based on an iterative approach which aims at minimizing a cost function. The main component of the cost function is given by the sum of the squared weighted differences between measured and modeled TB data, for a variety of incidence angles. The algorithm finds the best set of the parameters, e.g., SM and vegetation characteristics, which drive the direct TB model and minimizes the cost function. The end user Level 2 SM product contains SM, vegetation opacity, and estimated dielectric constant of any surface, TB computed at 42.5°, flags and quality indices, and other parameters of interest. This paper gives an overview- of the algorithm, discusses the caveats, and provides a glimpse of the Cal Val exercises.
Keywords :
geophysical techniques; ocean chemistry; radiometry; soil; AD 2009; Cal Val exercises; Centro para el Desarrollo Tecnologico Industrial; ESA Centre National dEtudes Spatiales; Earth Explorer Opportunity mission; European Space Agency; L-Band 2-D interferometric radiometer; SMOS mission; SMOS soil moisture retrieval algorithm; Soil Moisture and Ocean Salinity; angular brightness temperatures; cost function; earth surface emissivity; frequency 1400 MHz to 1427 MHz; global soil moisture maps; moisture content; protected band; sea surface salinity; vegetation opacity; L-band; Land surface; Ocean temperature; Sea surface; Surface roughness; Surface topography; Vegetation mapping; Cal/Val; SMOS; model; retrievals; soil moisture; vegetation opacity;
fLanguage :
English
Journal_Title :
Geoscience and Remote Sensing, IEEE Transactions on
Publisher :
ieee
ISSN :
0196-2892
Type :
jour
DOI :
10.1109/TGRS.2012.2184548
Filename :
6161633
Link To Document :
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