An atmosphere–wave regional coupled model: improving predictions of wave heights and surface winds in the southern North Sea

The coupling of models is a commonly used approach when addressing the complex interactions between different components of earth systems. We demonstrate that this approach can result in a reduction of errors in wave forecasting, especially in dynamically complicated coastal ocean areas, such as the...

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Main Authors: K. Wahle, J. Staneva, W. Koch, L. Fenoglio-Marc, H. T. M. Ho-Hagemann, E. V. Stanev
Format: Article
Language:English
Published: Copernicus Publications 2017-04-01
Series:Ocean Science
Online Access:http://www.ocean-sci.net/13/289/2017/os-13-289-2017.pdf
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author K. Wahle
J. Staneva
W. Koch
L. Fenoglio-Marc
H. T. M. Ho-Hagemann
E. V. Stanev
author_facet K. Wahle
J. Staneva
W. Koch
L. Fenoglio-Marc
H. T. M. Ho-Hagemann
E. V. Stanev
author_sort K. Wahle
collection DOAJ
description The coupling of models is a commonly used approach when addressing the complex interactions between different components of earth systems. We demonstrate that this approach can result in a reduction of errors in wave forecasting, especially in dynamically complicated coastal ocean areas, such as the southern part of the North Sea – the German Bight. Here, we study the effects of coupling of an atmospheric model (COSMO) and a wind wave model (WAM), which is enabled by implementing wave-induced drag in the atmospheric model. The numerical simulations use a regional North Sea coupled wave–atmosphere model as well as a nested-grid high-resolution German Bight wave model. Using one atmospheric and two wind wave models simultaneously allows for study of the individual and combined effects of two-way coupling and grid resolution. This approach proved to be particularly important under severe storm conditions as the German Bight is a very shallow and dynamically complex coastal area exposed to storm floods. The two-way coupling leads to a reduction of both surface wind speeds and simulated wave heights. In this study, the sensitivity of atmospheric parameters, such as wind speed and atmospheric pressure, to the wave-induced drag, in particular under storm conditions, and the impact of two-way coupling on the wave model performance, is quantified. Comparisons between data from in situ and satellite altimeter observations indicate that two-way coupling improves the simulation of wind and wave parameters of the model and justify its implementation for both operational and climate simulations.
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spelling doaj.art-e40349f2b3f64d829f9b3010289987b12022-12-22T01:58:52ZengCopernicus PublicationsOcean Science1812-07841812-07922017-04-0113228930110.5194/os-13-289-2017An atmosphere–wave regional coupled model: improving predictions of wave heights and surface winds in the southern North SeaK. Wahle0J. Staneva1W. Koch2L. Fenoglio-Marc3H. T. M. Ho-Hagemann4E. V. Stanev5Institute of Coastal Research, Helmholtz-Zentrum Geesthacht, Geesthacht, GermanyInstitute of Coastal Research, Helmholtz-Zentrum Geesthacht, Geesthacht, GermanyInstitute of Coastal Research, Helmholtz-Zentrum Geesthacht, Geesthacht, GermanyInstitute of Geodesy and Geoinformation, University of Bonn, Bonn, GermanyInstitute of Coastal Research, Helmholtz-Zentrum Geesthacht, Geesthacht, GermanyInstitute of Coastal Research, Helmholtz-Zentrum Geesthacht, Geesthacht, GermanyThe coupling of models is a commonly used approach when addressing the complex interactions between different components of earth systems. We demonstrate that this approach can result in a reduction of errors in wave forecasting, especially in dynamically complicated coastal ocean areas, such as the southern part of the North Sea – the German Bight. Here, we study the effects of coupling of an atmospheric model (COSMO) and a wind wave model (WAM), which is enabled by implementing wave-induced drag in the atmospheric model. The numerical simulations use a regional North Sea coupled wave–atmosphere model as well as a nested-grid high-resolution German Bight wave model. Using one atmospheric and two wind wave models simultaneously allows for study of the individual and combined effects of two-way coupling and grid resolution. This approach proved to be particularly important under severe storm conditions as the German Bight is a very shallow and dynamically complex coastal area exposed to storm floods. The two-way coupling leads to a reduction of both surface wind speeds and simulated wave heights. In this study, the sensitivity of atmospheric parameters, such as wind speed and atmospheric pressure, to the wave-induced drag, in particular under storm conditions, and the impact of two-way coupling on the wave model performance, is quantified. Comparisons between data from in situ and satellite altimeter observations indicate that two-way coupling improves the simulation of wind and wave parameters of the model and justify its implementation for both operational and climate simulations.http://www.ocean-sci.net/13/289/2017/os-13-289-2017.pdf
spellingShingle K. Wahle
J. Staneva
W. Koch
L. Fenoglio-Marc
H. T. M. Ho-Hagemann
E. V. Stanev
An atmosphere–wave regional coupled model: improving predictions of wave heights and surface winds in the southern North Sea
Ocean Science
title An atmosphere–wave regional coupled model: improving predictions of wave heights and surface winds in the southern North Sea
title_full An atmosphere–wave regional coupled model: improving predictions of wave heights and surface winds in the southern North Sea
title_fullStr An atmosphere–wave regional coupled model: improving predictions of wave heights and surface winds in the southern North Sea
title_full_unstemmed An atmosphere–wave regional coupled model: improving predictions of wave heights and surface winds in the southern North Sea
title_short An atmosphere–wave regional coupled model: improving predictions of wave heights and surface winds in the southern North Sea
title_sort atmosphere ndash wave regional coupled model improving predictions of wave heights and surface winds in the southern north sea
url http://www.ocean-sci.net/13/289/2017/os-13-289-2017.pdf
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