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Reconciling the global terrestrial water budget using satellite remote sensing

Reconciling the global terrestrial water budget using satellite remote sensing
Reconciling the global terrestrial water budget using satellite remote sensing

Recent retrievals of multiple satellite products for each component of the terrestrial water cycle provide an opportunity to estimate the water budget globally. In this study, we estimate the water budget from satellite remote sensing over ten global river basins for 2003-2006. We use several satellite and non-satellite precipitation (P) and evapo-transpiration (ET) products in this study. The satellite precipitation products are the GPCP, TRMM, CMORPH and PERSIANN. For ET, we use four products generated from three retrieval models (Penman-Monteith (PM), Priestley-Taylor (PT) and the Surface Energy Balance System (SEBS)) with data inputs from the Earth Observing System (EOS) or the International Satellite Cloud Climatology Project (ISCCP) products. GPCP precipitation and PM (ISCCP) ET have less bias and errors over most of the river basins. To estimate the total water budget from satellite data for each basin, we generate merged products for P and ET by combining the four P and four ET products using weighted values based on their errors with respect to non-satellite merged product. The water storage change component is taken from GRACE satellite data, which are used directly with a single pre-specified error value. In the absence of satellite retrievals of river discharge, we use in-situ gauge measurements. Closure of the water budget over the river basins from the combined satellite and in-situ discharge products is not achievable with errors of the order of 5-25% of mean annual precipitation. A constrained ensemble Kalman filter is used to close the water budget and provide a constrained best-estimate of the water budget. The non-closure error from each water budget component is estimated and it is found that the merged satellite precipitation product carries most of the non-closure error.

Global terrestrial water budget, Remote sensing, Water budget closure
0034-4257
1850-1865
Sahoo, Alok K.
ac3309f9-a1aa-4b13-abef-e5bd9080d8ea
Pan, Ming
10c372fa-0e0e-4eb5-b95b-06a8f9786fc8
Troy, Tara J.
0f42a33e-d70e-4f52-a559-718f4a25d8d8
Vinukollu, Raghuveer K.
8ff428ba-17eb-4318-9a82-3ed70df6d013
Sheffield, Justin
dd66575b-a4dc-4190-ad95-df2d6aaaaa6b
Wood, Eric F.
8352c1b4-4fd3-42fe-bd23-46619024f1cf
Sahoo, Alok K.
ac3309f9-a1aa-4b13-abef-e5bd9080d8ea
Pan, Ming
10c372fa-0e0e-4eb5-b95b-06a8f9786fc8
Troy, Tara J.
0f42a33e-d70e-4f52-a559-718f4a25d8d8
Vinukollu, Raghuveer K.
8ff428ba-17eb-4318-9a82-3ed70df6d013
Sheffield, Justin
dd66575b-a4dc-4190-ad95-df2d6aaaaa6b
Wood, Eric F.
8352c1b4-4fd3-42fe-bd23-46619024f1cf

Sahoo, Alok K., Pan, Ming, Troy, Tara J., Vinukollu, Raghuveer K., Sheffield, Justin and Wood, Eric F. (2011) Reconciling the global terrestrial water budget using satellite remote sensing. Remote Sensing of Environment, 115 (8), 1850-1865. (doi:10.1016/j.rse.2011.03.009).

Record type: Article

Abstract

Recent retrievals of multiple satellite products for each component of the terrestrial water cycle provide an opportunity to estimate the water budget globally. In this study, we estimate the water budget from satellite remote sensing over ten global river basins for 2003-2006. We use several satellite and non-satellite precipitation (P) and evapo-transpiration (ET) products in this study. The satellite precipitation products are the GPCP, TRMM, CMORPH and PERSIANN. For ET, we use four products generated from three retrieval models (Penman-Monteith (PM), Priestley-Taylor (PT) and the Surface Energy Balance System (SEBS)) with data inputs from the Earth Observing System (EOS) or the International Satellite Cloud Climatology Project (ISCCP) products. GPCP precipitation and PM (ISCCP) ET have less bias and errors over most of the river basins. To estimate the total water budget from satellite data for each basin, we generate merged products for P and ET by combining the four P and four ET products using weighted values based on their errors with respect to non-satellite merged product. The water storage change component is taken from GRACE satellite data, which are used directly with a single pre-specified error value. In the absence of satellite retrievals of river discharge, we use in-situ gauge measurements. Closure of the water budget over the river basins from the combined satellite and in-situ discharge products is not achievable with errors of the order of 5-25% of mean annual precipitation. A constrained ensemble Kalman filter is used to close the water budget and provide a constrained best-estimate of the water budget. The non-closure error from each water budget component is estimated and it is found that the merged satellite precipitation product carries most of the non-closure error.

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More information

Accepted/In Press date: 12 March 2011
e-pub ahead of print date: 29 April 2011
Published date: 15 August 2011
Additional Information: Funding Information: The research described herein was supported by grants from the State for Higher Education of the Russian Federation (project No. 97-0-9.2-313) Russian Fund for Basic Research No. 98-03-32063).
Keywords: Global terrestrial water budget, Remote sensing, Water budget closure

Identifiers

Local EPrints ID: 480834
URI: http://eprints.soton.ac.uk/id/eprint/480834
ISSN: 0034-4257
PURE UUID: 5c903b6e-5845-4058-ad26-6a6785424f4e
ORCID for Justin Sheffield: ORCID iD orcid.org/0000-0003-2400-0630

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Date deposited: 10 Aug 2023 16:37
Last modified: 18 Mar 2024 03:33

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Contributors

Author: Alok K. Sahoo
Author: Ming Pan
Author: Tara J. Troy
Author: Raghuveer K. Vinukollu
Author: Eric F. Wood

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