Computation of the storm surge of 1 to 6 April 1973 using numerical models of the North West European continental shelf and the North Sea
Summary The storm surge period 1 to 6 April 1973 is computed using two numerical models. One of coarser resolution covers the whole North West European continental shelf, the other has a finer resolution and covers the North Sea only, including the Skagerrak and Kattegat. Comparison of the surge com...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Davies, A. M. [verfasserIn] Flather, R. A. [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1977 |
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| Schlagwörter: |
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| Anmerkung: |
© Deutsches Hydrographisches Institut 1977 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Deutsche Hydrografische Zeitschrift - Loviscach, Jörn, Springer Berlin Heidelberg, 2011, 30(1977), 5 vom: 01. Sept., Seite 139-162 |
|---|---|
| Übergeordnetes Werk: |
volume:30 ; year:1977 ; number:5 ; day:01 ; month:09 ; pages:139-162 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF02226974 |
|---|
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SPR055714889 |
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| 520 | |a Summary The storm surge period 1 to 6 April 1973 is computed using two numerical models. One of coarser resolution covers the whole North West European continental shelf, the other has a finer resolution and covers the North Sea only, including the Skagerrak and Kattegat. Comparison of the surge computed by these models with and without the tide (consisting of the $ M_{2} $ and $ S_{2} $ components) enables the effect of tide-surge interaction in each model to be examined. Also effects produced by changes in model resolution may be studied. Results obtained from the North Sea model, using the hydrostatic law of pressure to determine surge levels on the open boundary, are in good agreement with observations when the major contribution to the surge is generated within the North Sea. However the use of this boundary condition leads to an error in the magnitude of the computed North Sea surge when the disturbance is generated externally. It is demonstrated that when surge residuals computed by the shelf model—together with observed residuals from Wick—are used as input along the northern boundary of the North Sea model, the error in the computed surge arising from the use of the hydrostatic law along this boundary is reduced. | ||
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10.1007/BF02226974 doi (DE-627)SPR055714889 (SPR)BF02226974-e DE-627 ger DE-627 rakwb eng Davies, A. M. verfasserin aut Computation of the storm surge of 1 to 6 April 1973 using numerical models of the North West European continental shelf and the North Sea 1977 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Deutsches Hydrographisches Institut 1977 Summary The storm surge period 1 to 6 April 1973 is computed using two numerical models. One of coarser resolution covers the whole North West European continental shelf, the other has a finer resolution and covers the North Sea only, including the Skagerrak and Kattegat. Comparison of the surge computed by these models with and without the tide (consisting of the $ M_{2} $ and $ S_{2} $ components) enables the effect of tide-surge interaction in each model to be examined. Also effects produced by changes in model resolution may be studied. Results obtained from the North Sea model, using the hydrostatic law of pressure to determine surge levels on the open boundary, are in good agreement with observations when the major contribution to the surge is generated within the North Sea. However the use of this boundary condition leads to an error in the magnitude of the computed North Sea surge when the disturbance is generated externally. It is demonstrated that when surge residuals computed by the shelf model—together with observed residuals from Wick—are used as input along the northern boundary of the North Sea model, the error in the computed surge arising from the use of the hydrostatic law along this boundary is reduced. Shelf Model (dpeaa)DE-He213 North West European Continental Shelf (dpeaa)DE-He213 Pression Hydrostatique (dpeaa)DE-He213 Flather, R. A. verfasserin aut Enthalten in Loviscach, Jörn Deutsche Hydrografische Zeitschrift Springer Berlin Heidelberg, 2011 30(1977), 5 vom: 01. Sept., Seite 139-162 1 Online-Ressource (21 MB, 00:25:44:00) (DE-627)1820839486 nnnm volume:30 year:1977 number:5 day:01 month:09 pages:139-162 https://dx.doi.org/10.1007/BF02226974 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER GBV_ILN_23 GBV_ILN_30 GBV_ILN_63 GBV_ILN_118 GBV_ILN_122 GBV_ILN_140 GBV_ILN_264 GBV_ILN_2057 GBV_ILN_2403 AR 30 1977 5 01 09 139-162 |
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10.1007/BF02226974 doi (DE-627)SPR055714889 (SPR)BF02226974-e DE-627 ger DE-627 rakwb eng Davies, A. M. verfasserin aut Computation of the storm surge of 1 to 6 April 1973 using numerical models of the North West European continental shelf and the North Sea 1977 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Deutsches Hydrographisches Institut 1977 Summary The storm surge period 1 to 6 April 1973 is computed using two numerical models. One of coarser resolution covers the whole North West European continental shelf, the other has a finer resolution and covers the North Sea only, including the Skagerrak and Kattegat. Comparison of the surge computed by these models with and without the tide (consisting of the $ M_{2} $ and $ S_{2} $ components) enables the effect of tide-surge interaction in each model to be examined. Also effects produced by changes in model resolution may be studied. Results obtained from the North Sea model, using the hydrostatic law of pressure to determine surge levels on the open boundary, are in good agreement with observations when the major contribution to the surge is generated within the North Sea. However the use of this boundary condition leads to an error in the magnitude of the computed North Sea surge when the disturbance is generated externally. It is demonstrated that when surge residuals computed by the shelf model—together with observed residuals from Wick—are used as input along the northern boundary of the North Sea model, the error in the computed surge arising from the use of the hydrostatic law along this boundary is reduced. Shelf Model (dpeaa)DE-He213 North West European Continental Shelf (dpeaa)DE-He213 Pression Hydrostatique (dpeaa)DE-He213 Flather, R. A. verfasserin aut Enthalten in Loviscach, Jörn Deutsche Hydrografische Zeitschrift Springer Berlin Heidelberg, 2011 30(1977), 5 vom: 01. Sept., Seite 139-162 1 Online-Ressource (21 MB, 00:25:44:00) (DE-627)1820839486 nnnm volume:30 year:1977 number:5 day:01 month:09 pages:139-162 https://dx.doi.org/10.1007/BF02226974 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER GBV_ILN_23 GBV_ILN_30 GBV_ILN_63 GBV_ILN_118 GBV_ILN_122 GBV_ILN_140 GBV_ILN_264 GBV_ILN_2057 GBV_ILN_2403 AR 30 1977 5 01 09 139-162 |
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10.1007/BF02226974 doi (DE-627)SPR055714889 (SPR)BF02226974-e DE-627 ger DE-627 rakwb eng Davies, A. M. verfasserin aut Computation of the storm surge of 1 to 6 April 1973 using numerical models of the North West European continental shelf and the North Sea 1977 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Deutsches Hydrographisches Institut 1977 Summary The storm surge period 1 to 6 April 1973 is computed using two numerical models. One of coarser resolution covers the whole North West European continental shelf, the other has a finer resolution and covers the North Sea only, including the Skagerrak and Kattegat. Comparison of the surge computed by these models with and without the tide (consisting of the $ M_{2} $ and $ S_{2} $ components) enables the effect of tide-surge interaction in each model to be examined. Also effects produced by changes in model resolution may be studied. Results obtained from the North Sea model, using the hydrostatic law of pressure to determine surge levels on the open boundary, are in good agreement with observations when the major contribution to the surge is generated within the North Sea. However the use of this boundary condition leads to an error in the magnitude of the computed North Sea surge when the disturbance is generated externally. It is demonstrated that when surge residuals computed by the shelf model—together with observed residuals from Wick—are used as input along the northern boundary of the North Sea model, the error in the computed surge arising from the use of the hydrostatic law along this boundary is reduced. Shelf Model (dpeaa)DE-He213 North West European Continental Shelf (dpeaa)DE-He213 Pression Hydrostatique (dpeaa)DE-He213 Flather, R. A. verfasserin aut Enthalten in Loviscach, Jörn Deutsche Hydrografische Zeitschrift Springer Berlin Heidelberg, 2011 30(1977), 5 vom: 01. Sept., Seite 139-162 1 Online-Ressource (21 MB, 00:25:44:00) (DE-627)1820839486 nnnm volume:30 year:1977 number:5 day:01 month:09 pages:139-162 https://dx.doi.org/10.1007/BF02226974 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER GBV_ILN_23 GBV_ILN_30 GBV_ILN_63 GBV_ILN_118 GBV_ILN_122 GBV_ILN_140 GBV_ILN_264 GBV_ILN_2057 GBV_ILN_2403 AR 30 1977 5 01 09 139-162 |
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10.1007/BF02226974 doi (DE-627)SPR055714889 (SPR)BF02226974-e DE-627 ger DE-627 rakwb eng Davies, A. M. verfasserin aut Computation of the storm surge of 1 to 6 April 1973 using numerical models of the North West European continental shelf and the North Sea 1977 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Deutsches Hydrographisches Institut 1977 Summary The storm surge period 1 to 6 April 1973 is computed using two numerical models. One of coarser resolution covers the whole North West European continental shelf, the other has a finer resolution and covers the North Sea only, including the Skagerrak and Kattegat. Comparison of the surge computed by these models with and without the tide (consisting of the $ M_{2} $ and $ S_{2} $ components) enables the effect of tide-surge interaction in each model to be examined. Also effects produced by changes in model resolution may be studied. Results obtained from the North Sea model, using the hydrostatic law of pressure to determine surge levels on the open boundary, are in good agreement with observations when the major contribution to the surge is generated within the North Sea. However the use of this boundary condition leads to an error in the magnitude of the computed North Sea surge when the disturbance is generated externally. It is demonstrated that when surge residuals computed by the shelf model—together with observed residuals from Wick—are used as input along the northern boundary of the North Sea model, the error in the computed surge arising from the use of the hydrostatic law along this boundary is reduced. Shelf Model (dpeaa)DE-He213 North West European Continental Shelf (dpeaa)DE-He213 Pression Hydrostatique (dpeaa)DE-He213 Flather, R. A. verfasserin aut Enthalten in Loviscach, Jörn Deutsche Hydrografische Zeitschrift Springer Berlin Heidelberg, 2011 30(1977), 5 vom: 01. Sept., Seite 139-162 1 Online-Ressource (21 MB, 00:25:44:00) (DE-627)1820839486 nnnm volume:30 year:1977 number:5 day:01 month:09 pages:139-162 https://dx.doi.org/10.1007/BF02226974 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER GBV_ILN_23 GBV_ILN_30 GBV_ILN_63 GBV_ILN_118 GBV_ILN_122 GBV_ILN_140 GBV_ILN_264 GBV_ILN_2057 GBV_ILN_2403 AR 30 1977 5 01 09 139-162 |
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10.1007/BF02226974 doi (DE-627)SPR055714889 (SPR)BF02226974-e DE-627 ger DE-627 rakwb eng Davies, A. M. verfasserin aut Computation of the storm surge of 1 to 6 April 1973 using numerical models of the North West European continental shelf and the North Sea 1977 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Deutsches Hydrographisches Institut 1977 Summary The storm surge period 1 to 6 April 1973 is computed using two numerical models. One of coarser resolution covers the whole North West European continental shelf, the other has a finer resolution and covers the North Sea only, including the Skagerrak and Kattegat. Comparison of the surge computed by these models with and without the tide (consisting of the $ M_{2} $ and $ S_{2} $ components) enables the effect of tide-surge interaction in each model to be examined. Also effects produced by changes in model resolution may be studied. Results obtained from the North Sea model, using the hydrostatic law of pressure to determine surge levels on the open boundary, are in good agreement with observations when the major contribution to the surge is generated within the North Sea. However the use of this boundary condition leads to an error in the magnitude of the computed North Sea surge when the disturbance is generated externally. It is demonstrated that when surge residuals computed by the shelf model—together with observed residuals from Wick—are used as input along the northern boundary of the North Sea model, the error in the computed surge arising from the use of the hydrostatic law along this boundary is reduced. Shelf Model (dpeaa)DE-He213 North West European Continental Shelf (dpeaa)DE-He213 Pression Hydrostatique (dpeaa)DE-He213 Flather, R. A. verfasserin aut Enthalten in Loviscach, Jörn Deutsche Hydrografische Zeitschrift Springer Berlin Heidelberg, 2011 30(1977), 5 vom: 01. Sept., Seite 139-162 1 Online-Ressource (21 MB, 00:25:44:00) (DE-627)1820839486 nnnm volume:30 year:1977 number:5 day:01 month:09 pages:139-162 https://dx.doi.org/10.1007/BF02226974 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER GBV_ILN_23 GBV_ILN_30 GBV_ILN_63 GBV_ILN_118 GBV_ILN_122 GBV_ILN_140 GBV_ILN_264 GBV_ILN_2057 GBV_ILN_2403 AR 30 1977 5 01 09 139-162 |
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computation of the storm surge of 1 to 6 april 1973 using numerical models of the north west european continental shelf and the north sea |
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Computation of the storm surge of 1 to 6 April 1973 using numerical models of the North West European continental shelf and the North Sea |
| abstract |
Summary The storm surge period 1 to 6 April 1973 is computed using two numerical models. One of coarser resolution covers the whole North West European continental shelf, the other has a finer resolution and covers the North Sea only, including the Skagerrak and Kattegat. Comparison of the surge computed by these models with and without the tide (consisting of the $ M_{2} $ and $ S_{2} $ components) enables the effect of tide-surge interaction in each model to be examined. Also effects produced by changes in model resolution may be studied. Results obtained from the North Sea model, using the hydrostatic law of pressure to determine surge levels on the open boundary, are in good agreement with observations when the major contribution to the surge is generated within the North Sea. However the use of this boundary condition leads to an error in the magnitude of the computed North Sea surge when the disturbance is generated externally. It is demonstrated that when surge residuals computed by the shelf model—together with observed residuals from Wick—are used as input along the northern boundary of the North Sea model, the error in the computed surge arising from the use of the hydrostatic law along this boundary is reduced. © Deutsches Hydrographisches Institut 1977 |
| abstractGer |
Summary The storm surge period 1 to 6 April 1973 is computed using two numerical models. One of coarser resolution covers the whole North West European continental shelf, the other has a finer resolution and covers the North Sea only, including the Skagerrak and Kattegat. Comparison of the surge computed by these models with and without the tide (consisting of the $ M_{2} $ and $ S_{2} $ components) enables the effect of tide-surge interaction in each model to be examined. Also effects produced by changes in model resolution may be studied. Results obtained from the North Sea model, using the hydrostatic law of pressure to determine surge levels on the open boundary, are in good agreement with observations when the major contribution to the surge is generated within the North Sea. However the use of this boundary condition leads to an error in the magnitude of the computed North Sea surge when the disturbance is generated externally. It is demonstrated that when surge residuals computed by the shelf model—together with observed residuals from Wick—are used as input along the northern boundary of the North Sea model, the error in the computed surge arising from the use of the hydrostatic law along this boundary is reduced. © Deutsches Hydrographisches Institut 1977 |
| abstract_unstemmed |
Summary The storm surge period 1 to 6 April 1973 is computed using two numerical models. One of coarser resolution covers the whole North West European continental shelf, the other has a finer resolution and covers the North Sea only, including the Skagerrak and Kattegat. Comparison of the surge computed by these models with and without the tide (consisting of the $ M_{2} $ and $ S_{2} $ components) enables the effect of tide-surge interaction in each model to be examined. Also effects produced by changes in model resolution may be studied. Results obtained from the North Sea model, using the hydrostatic law of pressure to determine surge levels on the open boundary, are in good agreement with observations when the major contribution to the surge is generated within the North Sea. However the use of this boundary condition leads to an error in the magnitude of the computed North Sea surge when the disturbance is generated externally. It is demonstrated that when surge residuals computed by the shelf model—together with observed residuals from Wick—are used as input along the northern boundary of the North Sea model, the error in the computed surge arising from the use of the hydrostatic law along this boundary is reduced. © Deutsches Hydrographisches Institut 1977 |
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SYSFLAG_0 GBV_SPRINGER GBV_ILN_23 GBV_ILN_30 GBV_ILN_63 GBV_ILN_118 GBV_ILN_122 GBV_ILN_140 GBV_ILN_264 GBV_ILN_2057 GBV_ILN_2403 |
| container_issue |
5 |
| title_short |
Computation of the storm surge of 1 to 6 April 1973 using numerical models of the North West European continental shelf and the North Sea |
| url |
https://dx.doi.org/10.1007/BF02226974 |
| remote_bool |
true |
| author2 |
Flather, R. A. |
| author2Str |
Flather, R. A. |
| ppnlink |
1820839486 |
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c |
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| doi_str |
10.1007/BF02226974 |
| up_date |
2024-07-03T17:33:13.990Z |
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1803580073828155392 |
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