Evaluation of the North American Land Data Assimilation System over the southern Great Plains during the warm season
Evaluation of the North American Land Data Assimilation System over the southern Great Plains during the warm season
North American Land Data Assimilation System (NLDAS) land surface models have been run for a retrospective period forced by atmospheric observations from the Eta analysis and actual precipitation and downward solar radiation to calculate land hydrology. We evaluated these simulations using in situ observations over the southern Great Plains for the periods of May-September of 1998 and 1999 by comparing the model outputs with surface latent, sensible, and ground heat fluxes at 24 Atmospheric Radiation Measurement/Cloud and Radiation Testbed stations and with soil temperature and soil moisture observations at 72 Oklahoma Mesonet stations. The standard NLDAS models do a fairly good job but with differences in the surface energy partition and in soil moisture between models and observations and among models during the summer, while they agree quite well on the soil temperature simulations. To investigate why, we performed a series of experiments accounting for differences between model-specified soil types and vegetation and those observed at the stations, and differences in model treatment of different soil types, vegetation properties, canopy resistance, soil column depth, rooting depth, root density, snow-free albedo, infiltration, aerodynamic resistance, and soil thermal diffusivity. The diagnosis and model enhancements demonstrate how the models can be improved so that they can be used in actual data assimilation mode.
Data assimilation, Soil moisture, Surface fluxes
GCP 7-1 - GCP 7-21
Robock, Alan
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Luo, Lifeng
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Wood, Eric F.
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Wen, Fenghua
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Mitchell, Kenneth E.
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Houser, Paul R.
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Schaake, John C.
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Lohmann, Dag
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Cosgrove, Brian A.
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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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Basara, Jeffery B.
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Crawford, Kenneth C.
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27 November 2003
Robock, Alan
48548a44-cb37-4c27-b96c-3826a9769fef
Luo, Lifeng
e9b25aa8-e877-45a6-bdca-53aba9bbde84
Wood, Eric F.
8352c1b4-4fd3-42fe-bd23-46619024f1cf
Wen, Fenghua
ed1a62d3-c289-4d18-942b-7a5bac10a768
Mitchell, Kenneth E.
91d961dc-4337-4c48-aace-74ebe14f1e2b
Houser, Paul R.
67aba422-f8ae-4d1d-a33f-2e6117ee1d54
Schaake, John C.
d9224d5c-d695-4d9b-88bb-2bfbfe8eeb61
Lohmann, Dag
f8974c4b-bc29-499f-8270-9adf64cd0afe
Cosgrove, Brian A.
04c1e698-3d7c-412a-8d15-1fe35635e687
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
e4eb84c6-998f-4269-999a-bcddabb8796c
Basara, Jeffery B.
c93bbf3e-9f4d-47ef-96b6-0feec645560b
Crawford, Kenneth C.
3fa8c188-8152-42a5-acfc-a4e01426f295
Robock, Alan, Luo, Lifeng, Wood, Eric F., Wen, Fenghua, Mitchell, Kenneth E., Houser, Paul R., Schaake, John C., Lohmann, Dag, Cosgrove, Brian A., Sheffield, Justin, Duan, Qingyun, Higgins, R. Wayne, Pinker, Rachel T., Tarpley, J. Dan, Basara, Jeffery B. and Crawford, Kenneth C.
(2003)
Evaluation of the North American Land Data Assimilation System over the southern Great Plains during the warm season.
Journal of Geophysical Research: Atmospheres, 108 (22), .
(doi:10.1029/2002jd003245).
Abstract
North American Land Data Assimilation System (NLDAS) land surface models have been run for a retrospective period forced by atmospheric observations from the Eta analysis and actual precipitation and downward solar radiation to calculate land hydrology. We evaluated these simulations using in situ observations over the southern Great Plains for the periods of May-September of 1998 and 1999 by comparing the model outputs with surface latent, sensible, and ground heat fluxes at 24 Atmospheric Radiation Measurement/Cloud and Radiation Testbed stations and with soil temperature and soil moisture observations at 72 Oklahoma Mesonet stations. The standard NLDAS models do a fairly good job but with differences in the surface energy partition and in soil moisture between models and observations and among models during the summer, while they agree quite well on the soil temperature simulations. To investigate why, we performed a series of experiments accounting for differences between model-specified soil types and vegetation and those observed at the stations, and differences in model treatment of different soil types, vegetation properties, canopy resistance, soil column depth, rooting depth, root density, snow-free albedo, infiltration, aerodynamic resistance, and soil thermal diffusivity. The diagnosis and model enhancements demonstrate how the models can be improved so that they can be used in actual data assimilation mode.
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Published date: 27 November 2003
Keywords:
Data assimilation, Soil moisture, Surface fluxes
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Local EPrints ID: 480438
URI: http://eprints.soton.ac.uk/id/eprint/480438
ISSN: 0148-0227
PURE UUID: 3bbf6ef7-970a-45fe-b10a-9dc338157a17
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Date deposited: 02 Aug 2023 16:39
Last modified: 17 Mar 2024 03:40
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Contributors
Author:
Alan Robock
Author:
Lifeng Luo
Author:
Eric F. Wood
Author:
Fenghua Wen
Author:
Kenneth E. Mitchell
Author:
Paul R. Houser
Author:
John C. Schaake
Author:
Dag Lohmann
Author:
Brian A. Cosgrove
Author:
Qingyun Duan
Author:
R. Wayne Higgins
Author:
Rachel T. Pinker
Author:
J. Dan Tarpley
Author:
Jeffery B. Basara
Author:
Kenneth C. Crawford
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