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Time-variations of the regional evapotranspiration rate from GRACE satellite gravimetry
Ramillien G., Frappart F., Güntner A., Ngo-Duc T., Cazenave A., Laval K.
Water Resources Research 42 (2006) W10403 - http://hal.archives-ouvertes.fr/hal-00429435
Article in peer-reviewed journal
Sciences of the Universe/Earth Sciences
Time-variations of the regional evapotranspiration rate from GRACE satellite gravimetry
Guillaume Ramillien 1, Frédéric Frappart () 1, 2, Andreas Güntner 3, Thanh Ngo-Duc () 4, Anny Cazenave 1, Katia Laval 4
1:  Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS)
http://www.legos.obs-mip.fr/
CNRS : UMR5566 – Institut de recherche pour le développement [IRD] – CNES – Observatoire Midi-Pyrénées – INSU – Université Paul Sabatier [UPS] - Toulouse III
14 avenue Edouard Belin 31400 Toulouse
France
2:  Laboratoire des Mécanismes et Transfert en Géologie (LMTG)
http://www.lmtg.obs-mip.fr/
CNRS : UMR5563 – Observatoire Midi-Pyrénées – Université Paul Sabatier [UPS] - Toulouse III – Institut de recherche pour le développement [IRD] : UMR154
14 avenue Edouard Belin 31400 Toulouse
France
3:  GeoForschungsZentrum (GFZ)
GeoForschungsZentrum
Potsdam
Germany
4:  Laboratoire de Météorologie Dynamique (LMD)
http://www.lmd.jussieu.fr/
CNRS : UMR8539 – INSU – Université Pierre et Marie Curie [UPMC] - Paris VI – Polytechnique - X – Ecole normale supérieure de Paris - ENS Paris
LMD ENS 24 Rue Lhomond 75231 Paris Cedex 05
France
Since its launch in March 2002, the GRACE mission is measuring the global time variations of the Earth's gravity field with a current resolution of ~500 km. Especially over the continents, these measurements represent the integrated land water mass including surface waters (lakes, wetlands and rivers), soil moisture, groundwater and snow cover. In this study, we use the GRACE land water solutions computed by Ramillien et al. (2005a) through an iterative inversion of monthly geoids from April 2002 to May 2004, to estimate time-series of basin-scale regional evapotranspiration rate -and associated uncertainties-. Evapotranspiration is determined by integrating and solving the water mass balance equation, which relates land water storage (from GRACE), precipitation data (from the Global Precipitation Climatology Centre), runoff (from a global land surface model) and evapotranspiration (the unknown). We further examine the sensibility of the computation when using different model runoff. Evapotranspiration results are compared to outputs of four different global land surface models. The overall satisfactory agreement between GRACE-derived and model-based evapotranspiration prove the ability of GRACE to provide realistic estimates of this parameter.
English
2005-06-09

Water Resources Research
Publisher American Geophysical Union (AGU)
ISSN 0043-1397 
international
2006-10-04
42
W10403

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