Ocean response to typhoon Nuri (2008) in western Pacific and South China Sea
Abstract Typhoon Nuri formed on 18 August 2008 in the western North Pacific east of the Philippines and traversed northwestward over the Kuroshio in the Luzon Strait where it intensified to a category 3 typhoon. The storm weakened as it passed over South China Sea (SCS) and made landfall in Hong Kon...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Sun, Jingru [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer-Verlag Berlin Heidelberg 2015 |
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| Übergeordnetes Werk: |
Enthalten in: Ocean dynamics - Springer Berlin Heidelberg, 2001, 65(2015), 5 vom: 20. März, Seite 735-749 |
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| Übergeordnetes Werk: |
volume:65 ; year:2015 ; number:5 ; day:20 ; month:03 ; pages:735-749 |
| Links: |
|---|
| DOI / URN: |
10.1007/s10236-015-0823-0 |
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OLC2070863700 |
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| 520 | |a Abstract Typhoon Nuri formed on 18 August 2008 in the western North Pacific east of the Philippines and traversed northwestward over the Kuroshio in the Luzon Strait where it intensified to a category 3 typhoon. The storm weakened as it passed over South China Sea (SCS) and made landfall in Hong Kong as a category 1 typhoon on 22 August. Despite the storm’s modest strength, the change in typhoon Nuri’s intensity was unique in that it strongly depended on the upper ocean. This study examines the ocean response to typhoon Nuri using the Princeton Ocean Model. An ocean state accounting for the sea-surface temperature (SST) and mesoscale eddy field prior to Nuri was constructed by assimilating satellite SST and altimetry data 12 days before the storm. The simulation then continued without further data assimilation, so that the ocean response to the strong wind can be used to understand processes. It is found that the SST cooling was biased to the right of the storm’s track due to inertial currents that rotated in the same sense as the wind vector, as has previously been found in the literature. However, despite the comparable wind speeds while the storm was in western Pacific and SCS, the SST cooling was much more intense in SCS. The reason was because in SCS, the surface layer was thinner, the vorticity field of the Kuroshio was cyclonic, and moreover a combination of larger Coriolis frequency as the storm moved northward and the typhoon’s slower translational speed produced a stronger resonance between wind and current, resulting in strong shears and entrainment of cool subsurface waters in the upper ocean. | ||
| 650 | 4 | |a Typhoon Nuri | |
| 650 | 4 | |a Upper ocean response | |
| 650 | 4 | |a Inertial currents | |
| 650 | 4 | |a Resonance between wind and ocean current | |
| 650 | 4 | |a South China Sea | |
| 650 | 4 | |a Western North Pacific Ocean | |
| 650 | 4 | |a Near-inertial internal waves | |
| 700 | 1 | |a Oey, Lie-Yauw |4 aut | |
| 700 | 1 | |a Chang, Roger |4 aut | |
| 700 | 1 | |a Xu, Fanghua |4 aut | |
| 700 | 1 | |a Huang, Shih-Ming |4 aut | |
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10.1007/s10236-015-0823-0 doi (DE-627)OLC2070863700 (DE-He213)s10236-015-0823-0-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn 38.90$jOzeanologie$jOzeanographie bkl Sun, Jingru verfasserin aut Ocean response to typhoon Nuri (2008) in western Pacific and South China Sea 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Berlin Heidelberg 2015 Abstract Typhoon Nuri formed on 18 August 2008 in the western North Pacific east of the Philippines and traversed northwestward over the Kuroshio in the Luzon Strait where it intensified to a category 3 typhoon. The storm weakened as it passed over South China Sea (SCS) and made landfall in Hong Kong as a category 1 typhoon on 22 August. Despite the storm’s modest strength, the change in typhoon Nuri’s intensity was unique in that it strongly depended on the upper ocean. This study examines the ocean response to typhoon Nuri using the Princeton Ocean Model. An ocean state accounting for the sea-surface temperature (SST) and mesoscale eddy field prior to Nuri was constructed by assimilating satellite SST and altimetry data 12 days before the storm. The simulation then continued without further data assimilation, so that the ocean response to the strong wind can be used to understand processes. It is found that the SST cooling was biased to the right of the storm’s track due to inertial currents that rotated in the same sense as the wind vector, as has previously been found in the literature. However, despite the comparable wind speeds while the storm was in western Pacific and SCS, the SST cooling was much more intense in SCS. The reason was because in SCS, the surface layer was thinner, the vorticity field of the Kuroshio was cyclonic, and moreover a combination of larger Coriolis frequency as the storm moved northward and the typhoon’s slower translational speed produced a stronger resonance between wind and current, resulting in strong shears and entrainment of cool subsurface waters in the upper ocean. Typhoon Nuri Upper ocean response Inertial currents Resonance between wind and ocean current South China Sea Western North Pacific Ocean Near-inertial internal waves Oey, Lie-Yauw aut Chang, Roger aut Xu, Fanghua aut Huang, Shih-Ming aut Enthalten in Ocean dynamics Springer Berlin Heidelberg, 2001 65(2015), 5 vom: 20. März, Seite 735-749 (DE-627)335936091 (DE-600)2060148-7 (DE-576)096704470 1616-7341 nnns volume:65 year:2015 number:5 day:20 month:03 pages:735-749 https://doi.org/10.1007/s10236-015-0823-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-GGO SSG-OPC-GGO GBV_ILN_62 GBV_ILN_70 GBV_ILN_183 GBV_ILN_600 GBV_ILN_2018 GBV_ILN_4277 GBV_ILN_4305 38.90$jOzeanologie$jOzeanographie VZ 106421921 (DE-625)106421921 AR 65 2015 5 20 03 735-749 |
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10.1007/s10236-015-0823-0 doi (DE-627)OLC2070863700 (DE-He213)s10236-015-0823-0-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn 38.90$jOzeanologie$jOzeanographie bkl Sun, Jingru verfasserin aut Ocean response to typhoon Nuri (2008) in western Pacific and South China Sea 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Berlin Heidelberg 2015 Abstract Typhoon Nuri formed on 18 August 2008 in the western North Pacific east of the Philippines and traversed northwestward over the Kuroshio in the Luzon Strait where it intensified to a category 3 typhoon. The storm weakened as it passed over South China Sea (SCS) and made landfall in Hong Kong as a category 1 typhoon on 22 August. Despite the storm’s modest strength, the change in typhoon Nuri’s intensity was unique in that it strongly depended on the upper ocean. This study examines the ocean response to typhoon Nuri using the Princeton Ocean Model. An ocean state accounting for the sea-surface temperature (SST) and mesoscale eddy field prior to Nuri was constructed by assimilating satellite SST and altimetry data 12 days before the storm. The simulation then continued without further data assimilation, so that the ocean response to the strong wind can be used to understand processes. It is found that the SST cooling was biased to the right of the storm’s track due to inertial currents that rotated in the same sense as the wind vector, as has previously been found in the literature. However, despite the comparable wind speeds while the storm was in western Pacific and SCS, the SST cooling was much more intense in SCS. The reason was because in SCS, the surface layer was thinner, the vorticity field of the Kuroshio was cyclonic, and moreover a combination of larger Coriolis frequency as the storm moved northward and the typhoon’s slower translational speed produced a stronger resonance between wind and current, resulting in strong shears and entrainment of cool subsurface waters in the upper ocean. Typhoon Nuri Upper ocean response Inertial currents Resonance between wind and ocean current South China Sea Western North Pacific Ocean Near-inertial internal waves Oey, Lie-Yauw aut Chang, Roger aut Xu, Fanghua aut Huang, Shih-Ming aut Enthalten in Ocean dynamics Springer Berlin Heidelberg, 2001 65(2015), 5 vom: 20. März, Seite 735-749 (DE-627)335936091 (DE-600)2060148-7 (DE-576)096704470 1616-7341 nnns volume:65 year:2015 number:5 day:20 month:03 pages:735-749 https://doi.org/10.1007/s10236-015-0823-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-GGO SSG-OPC-GGO GBV_ILN_62 GBV_ILN_70 GBV_ILN_183 GBV_ILN_600 GBV_ILN_2018 GBV_ILN_4277 GBV_ILN_4305 38.90$jOzeanologie$jOzeanographie VZ 106421921 (DE-625)106421921 AR 65 2015 5 20 03 735-749 |
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10.1007/s10236-015-0823-0 doi (DE-627)OLC2070863700 (DE-He213)s10236-015-0823-0-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn 38.90$jOzeanologie$jOzeanographie bkl Sun, Jingru verfasserin aut Ocean response to typhoon Nuri (2008) in western Pacific and South China Sea 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Berlin Heidelberg 2015 Abstract Typhoon Nuri formed on 18 August 2008 in the western North Pacific east of the Philippines and traversed northwestward over the Kuroshio in the Luzon Strait where it intensified to a category 3 typhoon. The storm weakened as it passed over South China Sea (SCS) and made landfall in Hong Kong as a category 1 typhoon on 22 August. Despite the storm’s modest strength, the change in typhoon Nuri’s intensity was unique in that it strongly depended on the upper ocean. This study examines the ocean response to typhoon Nuri using the Princeton Ocean Model. An ocean state accounting for the sea-surface temperature (SST) and mesoscale eddy field prior to Nuri was constructed by assimilating satellite SST and altimetry data 12 days before the storm. The simulation then continued without further data assimilation, so that the ocean response to the strong wind can be used to understand processes. It is found that the SST cooling was biased to the right of the storm’s track due to inertial currents that rotated in the same sense as the wind vector, as has previously been found in the literature. However, despite the comparable wind speeds while the storm was in western Pacific and SCS, the SST cooling was much more intense in SCS. The reason was because in SCS, the surface layer was thinner, the vorticity field of the Kuroshio was cyclonic, and moreover a combination of larger Coriolis frequency as the storm moved northward and the typhoon’s slower translational speed produced a stronger resonance between wind and current, resulting in strong shears and entrainment of cool subsurface waters in the upper ocean. Typhoon Nuri Upper ocean response Inertial currents Resonance between wind and ocean current South China Sea Western North Pacific Ocean Near-inertial internal waves Oey, Lie-Yauw aut Chang, Roger aut Xu, Fanghua aut Huang, Shih-Ming aut Enthalten in Ocean dynamics Springer Berlin Heidelberg, 2001 65(2015), 5 vom: 20. März, Seite 735-749 (DE-627)335936091 (DE-600)2060148-7 (DE-576)096704470 1616-7341 nnns volume:65 year:2015 number:5 day:20 month:03 pages:735-749 https://doi.org/10.1007/s10236-015-0823-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-GGO SSG-OPC-GGO GBV_ILN_62 GBV_ILN_70 GBV_ILN_183 GBV_ILN_600 GBV_ILN_2018 GBV_ILN_4277 GBV_ILN_4305 38.90$jOzeanologie$jOzeanographie VZ 106421921 (DE-625)106421921 AR 65 2015 5 20 03 735-749 |
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10.1007/s10236-015-0823-0 doi (DE-627)OLC2070863700 (DE-He213)s10236-015-0823-0-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn 38.90$jOzeanologie$jOzeanographie bkl Sun, Jingru verfasserin aut Ocean response to typhoon Nuri (2008) in western Pacific and South China Sea 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Berlin Heidelberg 2015 Abstract Typhoon Nuri formed on 18 August 2008 in the western North Pacific east of the Philippines and traversed northwestward over the Kuroshio in the Luzon Strait where it intensified to a category 3 typhoon. The storm weakened as it passed over South China Sea (SCS) and made landfall in Hong Kong as a category 1 typhoon on 22 August. Despite the storm’s modest strength, the change in typhoon Nuri’s intensity was unique in that it strongly depended on the upper ocean. This study examines the ocean response to typhoon Nuri using the Princeton Ocean Model. An ocean state accounting for the sea-surface temperature (SST) and mesoscale eddy field prior to Nuri was constructed by assimilating satellite SST and altimetry data 12 days before the storm. The simulation then continued without further data assimilation, so that the ocean response to the strong wind can be used to understand processes. It is found that the SST cooling was biased to the right of the storm’s track due to inertial currents that rotated in the same sense as the wind vector, as has previously been found in the literature. However, despite the comparable wind speeds while the storm was in western Pacific and SCS, the SST cooling was much more intense in SCS. The reason was because in SCS, the surface layer was thinner, the vorticity field of the Kuroshio was cyclonic, and moreover a combination of larger Coriolis frequency as the storm moved northward and the typhoon’s slower translational speed produced a stronger resonance between wind and current, resulting in strong shears and entrainment of cool subsurface waters in the upper ocean. Typhoon Nuri Upper ocean response Inertial currents Resonance between wind and ocean current South China Sea Western North Pacific Ocean Near-inertial internal waves Oey, Lie-Yauw aut Chang, Roger aut Xu, Fanghua aut Huang, Shih-Ming aut Enthalten in Ocean dynamics Springer Berlin Heidelberg, 2001 65(2015), 5 vom: 20. März, Seite 735-749 (DE-627)335936091 (DE-600)2060148-7 (DE-576)096704470 1616-7341 nnns volume:65 year:2015 number:5 day:20 month:03 pages:735-749 https://doi.org/10.1007/s10236-015-0823-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-GGO SSG-OPC-GGO GBV_ILN_62 GBV_ILN_70 GBV_ILN_183 GBV_ILN_600 GBV_ILN_2018 GBV_ILN_4277 GBV_ILN_4305 38.90$jOzeanologie$jOzeanographie VZ 106421921 (DE-625)106421921 AR 65 2015 5 20 03 735-749 |
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10.1007/s10236-015-0823-0 doi (DE-627)OLC2070863700 (DE-He213)s10236-015-0823-0-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn 38.90$jOzeanologie$jOzeanographie bkl Sun, Jingru verfasserin aut Ocean response to typhoon Nuri (2008) in western Pacific and South China Sea 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Berlin Heidelberg 2015 Abstract Typhoon Nuri formed on 18 August 2008 in the western North Pacific east of the Philippines and traversed northwestward over the Kuroshio in the Luzon Strait where it intensified to a category 3 typhoon. The storm weakened as it passed over South China Sea (SCS) and made landfall in Hong Kong as a category 1 typhoon on 22 August. Despite the storm’s modest strength, the change in typhoon Nuri’s intensity was unique in that it strongly depended on the upper ocean. This study examines the ocean response to typhoon Nuri using the Princeton Ocean Model. An ocean state accounting for the sea-surface temperature (SST) and mesoscale eddy field prior to Nuri was constructed by assimilating satellite SST and altimetry data 12 days before the storm. The simulation then continued without further data assimilation, so that the ocean response to the strong wind can be used to understand processes. It is found that the SST cooling was biased to the right of the storm’s track due to inertial currents that rotated in the same sense as the wind vector, as has previously been found in the literature. However, despite the comparable wind speeds while the storm was in western Pacific and SCS, the SST cooling was much more intense in SCS. The reason was because in SCS, the surface layer was thinner, the vorticity field of the Kuroshio was cyclonic, and moreover a combination of larger Coriolis frequency as the storm moved northward and the typhoon’s slower translational speed produced a stronger resonance between wind and current, resulting in strong shears and entrainment of cool subsurface waters in the upper ocean. Typhoon Nuri Upper ocean response Inertial currents Resonance between wind and ocean current South China Sea Western North Pacific Ocean Near-inertial internal waves Oey, Lie-Yauw aut Chang, Roger aut Xu, Fanghua aut Huang, Shih-Ming aut Enthalten in Ocean dynamics Springer Berlin Heidelberg, 2001 65(2015), 5 vom: 20. März, Seite 735-749 (DE-627)335936091 (DE-600)2060148-7 (DE-576)096704470 1616-7341 nnns volume:65 year:2015 number:5 day:20 month:03 pages:735-749 https://doi.org/10.1007/s10236-015-0823-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OLC-GGO SSG-OPC-GGO GBV_ILN_62 GBV_ILN_70 GBV_ILN_183 GBV_ILN_600 GBV_ILN_2018 GBV_ILN_4277 GBV_ILN_4305 38.90$jOzeanologie$jOzeanographie VZ 106421921 (DE-625)106421921 AR 65 2015 5 20 03 735-749 |
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ocean response to typhoon nuri (2008) in western pacific and south china sea |
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Ocean response to typhoon Nuri (2008) in western Pacific and South China Sea |
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Abstract Typhoon Nuri formed on 18 August 2008 in the western North Pacific east of the Philippines and traversed northwestward over the Kuroshio in the Luzon Strait where it intensified to a category 3 typhoon. The storm weakened as it passed over South China Sea (SCS) and made landfall in Hong Kong as a category 1 typhoon on 22 August. Despite the storm’s modest strength, the change in typhoon Nuri’s intensity was unique in that it strongly depended on the upper ocean. This study examines the ocean response to typhoon Nuri using the Princeton Ocean Model. An ocean state accounting for the sea-surface temperature (SST) and mesoscale eddy field prior to Nuri was constructed by assimilating satellite SST and altimetry data 12 days before the storm. The simulation then continued without further data assimilation, so that the ocean response to the strong wind can be used to understand processes. It is found that the SST cooling was biased to the right of the storm’s track due to inertial currents that rotated in the same sense as the wind vector, as has previously been found in the literature. However, despite the comparable wind speeds while the storm was in western Pacific and SCS, the SST cooling was much more intense in SCS. The reason was because in SCS, the surface layer was thinner, the vorticity field of the Kuroshio was cyclonic, and moreover a combination of larger Coriolis frequency as the storm moved northward and the typhoon’s slower translational speed produced a stronger resonance between wind and current, resulting in strong shears and entrainment of cool subsurface waters in the upper ocean. © Springer-Verlag Berlin Heidelberg 2015 |
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Abstract Typhoon Nuri formed on 18 August 2008 in the western North Pacific east of the Philippines and traversed northwestward over the Kuroshio in the Luzon Strait where it intensified to a category 3 typhoon. The storm weakened as it passed over South China Sea (SCS) and made landfall in Hong Kong as a category 1 typhoon on 22 August. Despite the storm’s modest strength, the change in typhoon Nuri’s intensity was unique in that it strongly depended on the upper ocean. This study examines the ocean response to typhoon Nuri using the Princeton Ocean Model. An ocean state accounting for the sea-surface temperature (SST) and mesoscale eddy field prior to Nuri was constructed by assimilating satellite SST and altimetry data 12 days before the storm. The simulation then continued without further data assimilation, so that the ocean response to the strong wind can be used to understand processes. It is found that the SST cooling was biased to the right of the storm’s track due to inertial currents that rotated in the same sense as the wind vector, as has previously been found in the literature. However, despite the comparable wind speeds while the storm was in western Pacific and SCS, the SST cooling was much more intense in SCS. The reason was because in SCS, the surface layer was thinner, the vorticity field of the Kuroshio was cyclonic, and moreover a combination of larger Coriolis frequency as the storm moved northward and the typhoon’s slower translational speed produced a stronger resonance between wind and current, resulting in strong shears and entrainment of cool subsurface waters in the upper ocean. © Springer-Verlag Berlin Heidelberg 2015 |
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Abstract Typhoon Nuri formed on 18 August 2008 in the western North Pacific east of the Philippines and traversed northwestward over the Kuroshio in the Luzon Strait where it intensified to a category 3 typhoon. The storm weakened as it passed over South China Sea (SCS) and made landfall in Hong Kong as a category 1 typhoon on 22 August. Despite the storm’s modest strength, the change in typhoon Nuri’s intensity was unique in that it strongly depended on the upper ocean. This study examines the ocean response to typhoon Nuri using the Princeton Ocean Model. An ocean state accounting for the sea-surface temperature (SST) and mesoscale eddy field prior to Nuri was constructed by assimilating satellite SST and altimetry data 12 days before the storm. The simulation then continued without further data assimilation, so that the ocean response to the strong wind can be used to understand processes. It is found that the SST cooling was biased to the right of the storm’s track due to inertial currents that rotated in the same sense as the wind vector, as has previously been found in the literature. However, despite the comparable wind speeds while the storm was in western Pacific and SCS, the SST cooling was much more intense in SCS. The reason was because in SCS, the surface layer was thinner, the vorticity field of the Kuroshio was cyclonic, and moreover a combination of larger Coriolis frequency as the storm moved northward and the typhoon’s slower translational speed produced a stronger resonance between wind and current, resulting in strong shears and entrainment of cool subsurface waters in the upper ocean. © Springer-Verlag Berlin Heidelberg 2015 |
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