Multivariate hydrological data assimilation of soil moisture and groundwater head

Observed groundwater head and soil moisture profiles are assimilated into an integrated hydrological model. The study uses the ensemble transform Kalman filter (ETKF) data assimilation method with the MIKE SHE hydrological model code. The method was firstly tested on synthetic data in a catchment...

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Main Authors: D. Zhang, H. Madsen, M. E. Ridler, J. Kidmose, K. H. Jensen, J. C. Refsgaard
Format: Article
Language:English
Published: Copernicus Publications 2016-10-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/20/4341/2016/hess-20-4341-2016.pdf
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spelling doaj-f10a6f38503f4940a9bd17811b17a4762020-11-24T22:39:24ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382016-10-01204341435710.5194/hess-20-4341-2016Multivariate hydrological data assimilation of soil moisture and groundwater headD. Zhang0H. Madsen1M. E. Ridler2J. Kidmose3K. H. Jensen4J. C. Refsgaard5Department of Geosciences and Natural Resource Management, University of Copenhagen, Copenhagen, DenmarkDHI, Hørsholm, DenmarkDHI, Hørsholm, DenmarkGeological Survey of Denmark and Greenland (GEUS), Copenhagen, DenmarkDepartment of Geosciences and Natural Resource Management, University of Copenhagen, Copenhagen, DenmarkGeological Survey of Denmark and Greenland (GEUS), Copenhagen, DenmarkObserved groundwater head and soil moisture profiles are assimilated into an integrated hydrological model. The study uses the ensemble transform Kalman filter (ETKF) data assimilation method with the MIKE SHE hydrological model code. The method was firstly tested on synthetic data in a catchment of less complexity (the Karup catchment in Denmark), and later implemented using data from real observations in a larger and more complex catchment (the Ahlergaarde catchment in Denmark). In the Karup model, several experiments were designed with respect to different observation types, ensemble sizes and localization schemes, to investigate the assimilation performance. The results showed the necessity of using localization, especially when assimilating both groundwater head and soil moisture. The proposed scheme with both distance localization and variable localization was shown to be more robust and provide better results. Using the same assimilation scheme in the Ahlergaarde model, groundwater head and soil moisture were successfully assimilated into the model. The hydrological model with assimilation showed an overall improved performance compared to the model without assimilation.https://www.hydrol-earth-syst-sci.net/20/4341/2016/hess-20-4341-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. Zhang
H. Madsen
M. E. Ridler
J. Kidmose
K. H. Jensen
J. C. Refsgaard
spellingShingle D. Zhang
H. Madsen
M. E. Ridler
J. Kidmose
K. H. Jensen
J. C. Refsgaard
Multivariate hydrological data assimilation of soil moisture and groundwater head
Hydrology and Earth System Sciences
author_facet D. Zhang
H. Madsen
M. E. Ridler
J. Kidmose
K. H. Jensen
J. C. Refsgaard
author_sort D. Zhang
title Multivariate hydrological data assimilation of soil moisture and groundwater head
title_short Multivariate hydrological data assimilation of soil moisture and groundwater head
title_full Multivariate hydrological data assimilation of soil moisture and groundwater head
title_fullStr Multivariate hydrological data assimilation of soil moisture and groundwater head
title_full_unstemmed Multivariate hydrological data assimilation of soil moisture and groundwater head
title_sort multivariate hydrological data assimilation of soil moisture and groundwater head
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2016-10-01
description Observed groundwater head and soil moisture profiles are assimilated into an integrated hydrological model. The study uses the ensemble transform Kalman filter (ETKF) data assimilation method with the MIKE SHE hydrological model code. The method was firstly tested on synthetic data in a catchment of less complexity (the Karup catchment in Denmark), and later implemented using data from real observations in a larger and more complex catchment (the Ahlergaarde catchment in Denmark). In the Karup model, several experiments were designed with respect to different observation types, ensemble sizes and localization schemes, to investigate the assimilation performance. The results showed the necessity of using localization, especially when assimilating both groundwater head and soil moisture. The proposed scheme with both distance localization and variable localization was shown to be more robust and provide better results. Using the same assimilation scheme in the Ahlergaarde model, groundwater head and soil moisture were successfully assimilated into the model. The hydrological model with assimilation showed an overall improved performance compared to the model without assimilation.
url https://www.hydrol-earth-syst-sci.net/20/4341/2016/hess-20-4341-2016.pdf
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AT jkidmose multivariatehydrologicaldataassimilationofsoilmoistureandgroundwaterhead
AT khjensen multivariatehydrologicaldataassimilationofsoilmoistureandgroundwaterhead
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