Validation of the North American Land Data Assimilation System (NLDAS) retrospective forcing over the southern Great Plains
Validation of the North American Land Data Assimilation System (NLDAS) retrospective forcing over the southern Great Plains
Atmospheric forcing used by land surface models is a critical component of the North American Land Data Assimilation System (NLDAS) and its quality crucially affects the final product of NLDAS and our work on model improvement. A three-year (September 1996-September 1999) retrospective forcing data set was created from the Eta Data Assimilation System and observations and used to run the NLDAS land surface models for this period. We compared gridded NLDAS forcing with station observations obtained from networks including the Oklahoma Mesonet and Atmospheric Radiation Measurement/Cloud and Radiation Testbed at the southern Great Plains. Differences in all forcing variables except precipitation between the NLDAS forcing data set and station observations are small at all timescales. While precipitation data do not agree very well at an hourly timescale, they do agree better at longer timescales because of the way NLDAS precipitation forcing is generated. A small high bias in downward solar radiation and a low bias in downward longwave radiation exist in the retrospective forcing. To investigate the impact of these differences on land surface modeling we compared two sets of model simulations, one forced by the standard NLDAS product and one with station-observed meteorology. The differences in the resulting simulations of soil moisture and soil temperature for each model were small, much smaller than the differences between the models and between the models and observations. This indicates that NLDAS retrospective forcing provides an excellent state-of-the-art data set for land surface modeling, at least over the southern Great Plains region.
Land surface modeling, LDAS, Surface fluxes
GCP 4-1 - GCP 4-10
Luo, Lifeng
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Robock, Alan
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Mitchell, Kenneth E.
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Houser, Paul R.
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Wood, Eric F.
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Schaake, John C.
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Lohmann, Dag
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Cosgrove, Brian A.
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Wen, Fenghua
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Sheffield, Justin
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Duan, Qingyun
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Higgins, R. Wayne
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Pinker, Rachel T.
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Tarpley, J. Dan
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27 November 2003
Luo, Lifeng
e9b25aa8-e877-45a6-bdca-53aba9bbde84
Robock, Alan
48548a44-cb37-4c27-b96c-3826a9769fef
Mitchell, Kenneth E.
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Houser, Paul R.
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Wood, Eric F.
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Schaake, John C.
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Lohmann, Dag
f8974c4b-bc29-499f-8270-9adf64cd0afe
Cosgrove, Brian A.
04c1e698-3d7c-412a-8d15-1fe35635e687
Wen, Fenghua
ed1a62d3-c289-4d18-942b-7a5bac10a768
Sheffield, Justin
dd66575b-a4dc-4190-ad95-df2d6aaaaa6b
Duan, Qingyun
b75b3e1f-c6c8-4062-bc33-e1d10a87f25b
Higgins, R. Wayne
93759215-b563-4735-8137-9acc5f14fc93
Pinker, Rachel T.
42f0f84f-36c8-412d-a317-851f70c6fe7d
Tarpley, J. Dan
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Luo, Lifeng, Robock, Alan, Mitchell, Kenneth E., Houser, Paul R., Wood, Eric F., Schaake, John C., Lohmann, Dag, Cosgrove, Brian A., Wen, Fenghua, Sheffield, Justin, Duan, Qingyun, Higgins, R. Wayne, Pinker, Rachel T. and Tarpley, J. Dan
(2003)
Validation of the North American Land Data Assimilation System (NLDAS) retrospective forcing over the southern Great Plains.
Journal of Geophysical Research: Atmospheres, 108 (22), .
(doi:10.1029/2002jd003246).
Abstract
Atmospheric forcing used by land surface models is a critical component of the North American Land Data Assimilation System (NLDAS) and its quality crucially affects the final product of NLDAS and our work on model improvement. A three-year (September 1996-September 1999) retrospective forcing data set was created from the Eta Data Assimilation System and observations and used to run the NLDAS land surface models for this period. We compared gridded NLDAS forcing with station observations obtained from networks including the Oklahoma Mesonet and Atmospheric Radiation Measurement/Cloud and Radiation Testbed at the southern Great Plains. Differences in all forcing variables except precipitation between the NLDAS forcing data set and station observations are small at all timescales. While precipitation data do not agree very well at an hourly timescale, they do agree better at longer timescales because of the way NLDAS precipitation forcing is generated. A small high bias in downward solar radiation and a low bias in downward longwave radiation exist in the retrospective forcing. To investigate the impact of these differences on land surface modeling we compared two sets of model simulations, one forced by the standard NLDAS product and one with station-observed meteorology. The differences in the resulting simulations of soil moisture and soil temperature for each model were small, much smaller than the differences between the models and between the models and observations. This indicates that NLDAS retrospective forcing provides an excellent state-of-the-art data set for land surface modeling, at least over the southern Great Plains region.
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Published date: 27 November 2003
Keywords:
Land surface modeling, LDAS, Surface fluxes
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Local EPrints ID: 480443
URI: http://eprints.soton.ac.uk/id/eprint/480443
ISSN: 0148-0227
PURE UUID: 712e2d5b-cf7f-4c8a-8b9f-40dbfe7eb1ff
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Date deposited: 02 Aug 2023 16:41
Last modified: 17 Mar 2024 03:40
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Contributors
Author:
Lifeng Luo
Author:
Alan Robock
Author:
Kenneth E. Mitchell
Author:
Paul R. Houser
Author:
Eric F. Wood
Author:
John C. Schaake
Author:
Dag Lohmann
Author:
Brian A. Cosgrove
Author:
Fenghua Wen
Author:
Qingyun Duan
Author:
R. Wayne Higgins
Author:
Rachel T. Pinker
Author:
J. Dan Tarpley
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