Latitudinal and Seasonal Variations in Tropical Cyclone-Induced Ocean Surface Cooling in the Tropical Western North Pacific
Abstract The passage of tropical cyclones induces ocean surface cooling through vertical mixing, upwelling, and surface heat loss. The dependence of tropical cyclone-induced ocean surface cooling on the intensity and translation speed of tropical cyclones has been documented in previous studies. The...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Jin, Mengxi [verfasserIn] |
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Englisch |
| Erschienen: |
2023 |
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© The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2023 |
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Enthalten in: Acta Meteorologica Sinica - The Chinese Meteorological Society, 2011, 37(2023), 6 vom: Dez., Seite 790-801 |
|---|---|
| Übergeordnetes Werk: |
volume:37 ; year:2023 ; number:6 ; month:12 ; pages:790-801 |
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10.1007/s13351-023-3040-7 |
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| 520 | |a Abstract The passage of tropical cyclones induces ocean surface cooling through vertical mixing, upwelling, and surface heat loss. The dependence of tropical cyclone-induced ocean surface cooling on the intensity and translation speed of tropical cyclones has been documented in previous studies. The present study investigates the latitudinal and seasonal variations in tropical cyclone-induced ocean surface cooling in the tropical western North Pacific based on data for the 2001–2020 period. Our analysis focuses on the open ocean (0°–25°N, 130°E–180°) to reduce the interference of coastal topography so that the obtained results better represent the influences of the intensity and translation speed of tropical cyclones. Our analysis confirms the dependence on the intensity and translation speed of tropical cyclone-induced cooling. The new findings are as follows. First, the time to reach the maximum cooling increases with the magnitude of the maximum cooling. Second, the magnitude of ocean surface cooling increases with latitude in the tropical region for tropical cyclones with different intensities and translation speeds. Third, the ocean surface cooling is larger in summer and autumn than in spring for tropical cyclones with different intensities and translation speeds. Fourth, the dependence of ocean surface cooling on the translation speed is more obvious at higher latitudes in the tropics and less apparent in spring. These new findings add to the existing knowledge of the impacts of tropical cyclone intensity and translation speed on ocean surface cooling. | ||
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| 700 | 1 | |a Zhu, Peijun |4 aut | |
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10.1007/s13351-023-3040-7 doi (DE-627)SPR054327261 (SPR)s13351-023-3040-7-e DE-627 ger DE-627 rakwb eng Jin, Mengxi verfasserin aut Latitudinal and Seasonal Variations in Tropical Cyclone-Induced Ocean Surface Cooling in the Tropical Western North Pacific 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2023 Abstract The passage of tropical cyclones induces ocean surface cooling through vertical mixing, upwelling, and surface heat loss. The dependence of tropical cyclone-induced ocean surface cooling on the intensity and translation speed of tropical cyclones has been documented in previous studies. The present study investigates the latitudinal and seasonal variations in tropical cyclone-induced ocean surface cooling in the tropical western North Pacific based on data for the 2001–2020 period. Our analysis focuses on the open ocean (0°–25°N, 130°E–180°) to reduce the interference of coastal topography so that the obtained results better represent the influences of the intensity and translation speed of tropical cyclones. Our analysis confirms the dependence on the intensity and translation speed of tropical cyclone-induced cooling. The new findings are as follows. First, the time to reach the maximum cooling increases with the magnitude of the maximum cooling. Second, the magnitude of ocean surface cooling increases with latitude in the tropical region for tropical cyclones with different intensities and translation speeds. Third, the ocean surface cooling is larger in summer and autumn than in spring for tropical cyclones with different intensities and translation speeds. Fourth, the dependence of ocean surface cooling on the translation speed is more obvious at higher latitudes in the tropics and less apparent in spring. These new findings add to the existing knowledge of the impacts of tropical cyclone intensity and translation speed on ocean surface cooling. Zhao, Ziyuan aut Wu, Renguang aut Zhu, Peijun aut Enthalten in Acta Meteorologica Sinica The Chinese Meteorological Society, 2011 37(2023), 6 vom: Dez., Seite 790-801 (DE-627)SPR031424376 nnns volume:37 year:2023 number:6 month:12 pages:790-801 https://dx.doi.org/10.1007/s13351-023-3040-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER AR 37 2023 6 12 790-801 |
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10.1007/s13351-023-3040-7 doi (DE-627)SPR054327261 (SPR)s13351-023-3040-7-e DE-627 ger DE-627 rakwb eng Jin, Mengxi verfasserin aut Latitudinal and Seasonal Variations in Tropical Cyclone-Induced Ocean Surface Cooling in the Tropical Western North Pacific 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2023 Abstract The passage of tropical cyclones induces ocean surface cooling through vertical mixing, upwelling, and surface heat loss. The dependence of tropical cyclone-induced ocean surface cooling on the intensity and translation speed of tropical cyclones has been documented in previous studies. The present study investigates the latitudinal and seasonal variations in tropical cyclone-induced ocean surface cooling in the tropical western North Pacific based on data for the 2001–2020 period. Our analysis focuses on the open ocean (0°–25°N, 130°E–180°) to reduce the interference of coastal topography so that the obtained results better represent the influences of the intensity and translation speed of tropical cyclones. Our analysis confirms the dependence on the intensity and translation speed of tropical cyclone-induced cooling. The new findings are as follows. First, the time to reach the maximum cooling increases with the magnitude of the maximum cooling. Second, the magnitude of ocean surface cooling increases with latitude in the tropical region for tropical cyclones with different intensities and translation speeds. Third, the ocean surface cooling is larger in summer and autumn than in spring for tropical cyclones with different intensities and translation speeds. Fourth, the dependence of ocean surface cooling on the translation speed is more obvious at higher latitudes in the tropics and less apparent in spring. These new findings add to the existing knowledge of the impacts of tropical cyclone intensity and translation speed on ocean surface cooling. Zhao, Ziyuan aut Wu, Renguang aut Zhu, Peijun aut Enthalten in Acta Meteorologica Sinica The Chinese Meteorological Society, 2011 37(2023), 6 vom: Dez., Seite 790-801 (DE-627)SPR031424376 nnns volume:37 year:2023 number:6 month:12 pages:790-801 https://dx.doi.org/10.1007/s13351-023-3040-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER AR 37 2023 6 12 790-801 |
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10.1007/s13351-023-3040-7 doi (DE-627)SPR054327261 (SPR)s13351-023-3040-7-e DE-627 ger DE-627 rakwb eng Jin, Mengxi verfasserin aut Latitudinal and Seasonal Variations in Tropical Cyclone-Induced Ocean Surface Cooling in the Tropical Western North Pacific 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2023 Abstract The passage of tropical cyclones induces ocean surface cooling through vertical mixing, upwelling, and surface heat loss. The dependence of tropical cyclone-induced ocean surface cooling on the intensity and translation speed of tropical cyclones has been documented in previous studies. The present study investigates the latitudinal and seasonal variations in tropical cyclone-induced ocean surface cooling in the tropical western North Pacific based on data for the 2001–2020 period. Our analysis focuses on the open ocean (0°–25°N, 130°E–180°) to reduce the interference of coastal topography so that the obtained results better represent the influences of the intensity and translation speed of tropical cyclones. Our analysis confirms the dependence on the intensity and translation speed of tropical cyclone-induced cooling. The new findings are as follows. First, the time to reach the maximum cooling increases with the magnitude of the maximum cooling. Second, the magnitude of ocean surface cooling increases with latitude in the tropical region for tropical cyclones with different intensities and translation speeds. Third, the ocean surface cooling is larger in summer and autumn than in spring for tropical cyclones with different intensities and translation speeds. Fourth, the dependence of ocean surface cooling on the translation speed is more obvious at higher latitudes in the tropics and less apparent in spring. These new findings add to the existing knowledge of the impacts of tropical cyclone intensity and translation speed on ocean surface cooling. Zhao, Ziyuan aut Wu, Renguang aut Zhu, Peijun aut Enthalten in Acta Meteorologica Sinica The Chinese Meteorological Society, 2011 37(2023), 6 vom: Dez., Seite 790-801 (DE-627)SPR031424376 nnns volume:37 year:2023 number:6 month:12 pages:790-801 https://dx.doi.org/10.1007/s13351-023-3040-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER AR 37 2023 6 12 790-801 |
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10.1007/s13351-023-3040-7 doi (DE-627)SPR054327261 (SPR)s13351-023-3040-7-e DE-627 ger DE-627 rakwb eng Jin, Mengxi verfasserin aut Latitudinal and Seasonal Variations in Tropical Cyclone-Induced Ocean Surface Cooling in the Tropical Western North Pacific 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2023 Abstract The passage of tropical cyclones induces ocean surface cooling through vertical mixing, upwelling, and surface heat loss. The dependence of tropical cyclone-induced ocean surface cooling on the intensity and translation speed of tropical cyclones has been documented in previous studies. The present study investigates the latitudinal and seasonal variations in tropical cyclone-induced ocean surface cooling in the tropical western North Pacific based on data for the 2001–2020 period. Our analysis focuses on the open ocean (0°–25°N, 130°E–180°) to reduce the interference of coastal topography so that the obtained results better represent the influences of the intensity and translation speed of tropical cyclones. Our analysis confirms the dependence on the intensity and translation speed of tropical cyclone-induced cooling. The new findings are as follows. First, the time to reach the maximum cooling increases with the magnitude of the maximum cooling. Second, the magnitude of ocean surface cooling increases with latitude in the tropical region for tropical cyclones with different intensities and translation speeds. Third, the ocean surface cooling is larger in summer and autumn than in spring for tropical cyclones with different intensities and translation speeds. Fourth, the dependence of ocean surface cooling on the translation speed is more obvious at higher latitudes in the tropics and less apparent in spring. These new findings add to the existing knowledge of the impacts of tropical cyclone intensity and translation speed on ocean surface cooling. Zhao, Ziyuan aut Wu, Renguang aut Zhu, Peijun aut Enthalten in Acta Meteorologica Sinica The Chinese Meteorological Society, 2011 37(2023), 6 vom: Dez., Seite 790-801 (DE-627)SPR031424376 nnns volume:37 year:2023 number:6 month:12 pages:790-801 https://dx.doi.org/10.1007/s13351-023-3040-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER AR 37 2023 6 12 790-801 |
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10.1007/s13351-023-3040-7 doi (DE-627)SPR054327261 (SPR)s13351-023-3040-7-e DE-627 ger DE-627 rakwb eng Jin, Mengxi verfasserin aut Latitudinal and Seasonal Variations in Tropical Cyclone-Induced Ocean Surface Cooling in the Tropical Western North Pacific 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2023 Abstract The passage of tropical cyclones induces ocean surface cooling through vertical mixing, upwelling, and surface heat loss. The dependence of tropical cyclone-induced ocean surface cooling on the intensity and translation speed of tropical cyclones has been documented in previous studies. The present study investigates the latitudinal and seasonal variations in tropical cyclone-induced ocean surface cooling in the tropical western North Pacific based on data for the 2001–2020 period. Our analysis focuses on the open ocean (0°–25°N, 130°E–180°) to reduce the interference of coastal topography so that the obtained results better represent the influences of the intensity and translation speed of tropical cyclones. Our analysis confirms the dependence on the intensity and translation speed of tropical cyclone-induced cooling. The new findings are as follows. First, the time to reach the maximum cooling increases with the magnitude of the maximum cooling. Second, the magnitude of ocean surface cooling increases with latitude in the tropical region for tropical cyclones with different intensities and translation speeds. Third, the ocean surface cooling is larger in summer and autumn than in spring for tropical cyclones with different intensities and translation speeds. Fourth, the dependence of ocean surface cooling on the translation speed is more obvious at higher latitudes in the tropics and less apparent in spring. These new findings add to the existing knowledge of the impacts of tropical cyclone intensity and translation speed on ocean surface cooling. Zhao, Ziyuan aut Wu, Renguang aut Zhu, Peijun aut Enthalten in Acta Meteorologica Sinica The Chinese Meteorological Society, 2011 37(2023), 6 vom: Dez., Seite 790-801 (DE-627)SPR031424376 nnns volume:37 year:2023 number:6 month:12 pages:790-801 https://dx.doi.org/10.1007/s13351-023-3040-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER AR 37 2023 6 12 790-801 |
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Latitudinal and Seasonal Variations in Tropical Cyclone-Induced Ocean Surface Cooling in the Tropical Western North Pacific |
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Abstract The passage of tropical cyclones induces ocean surface cooling through vertical mixing, upwelling, and surface heat loss. The dependence of tropical cyclone-induced ocean surface cooling on the intensity and translation speed of tropical cyclones has been documented in previous studies. The present study investigates the latitudinal and seasonal variations in tropical cyclone-induced ocean surface cooling in the tropical western North Pacific based on data for the 2001–2020 period. Our analysis focuses on the open ocean (0°–25°N, 130°E–180°) to reduce the interference of coastal topography so that the obtained results better represent the influences of the intensity and translation speed of tropical cyclones. Our analysis confirms the dependence on the intensity and translation speed of tropical cyclone-induced cooling. The new findings are as follows. First, the time to reach the maximum cooling increases with the magnitude of the maximum cooling. Second, the magnitude of ocean surface cooling increases with latitude in the tropical region for tropical cyclones with different intensities and translation speeds. Third, the ocean surface cooling is larger in summer and autumn than in spring for tropical cyclones with different intensities and translation speeds. Fourth, the dependence of ocean surface cooling on the translation speed is more obvious at higher latitudes in the tropics and less apparent in spring. These new findings add to the existing knowledge of the impacts of tropical cyclone intensity and translation speed on ocean surface cooling. © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2023 |
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Abstract The passage of tropical cyclones induces ocean surface cooling through vertical mixing, upwelling, and surface heat loss. The dependence of tropical cyclone-induced ocean surface cooling on the intensity and translation speed of tropical cyclones has been documented in previous studies. The present study investigates the latitudinal and seasonal variations in tropical cyclone-induced ocean surface cooling in the tropical western North Pacific based on data for the 2001–2020 period. Our analysis focuses on the open ocean (0°–25°N, 130°E–180°) to reduce the interference of coastal topography so that the obtained results better represent the influences of the intensity and translation speed of tropical cyclones. Our analysis confirms the dependence on the intensity and translation speed of tropical cyclone-induced cooling. The new findings are as follows. First, the time to reach the maximum cooling increases with the magnitude of the maximum cooling. Second, the magnitude of ocean surface cooling increases with latitude in the tropical region for tropical cyclones with different intensities and translation speeds. Third, the ocean surface cooling is larger in summer and autumn than in spring for tropical cyclones with different intensities and translation speeds. Fourth, the dependence of ocean surface cooling on the translation speed is more obvious at higher latitudes in the tropics and less apparent in spring. These new findings add to the existing knowledge of the impacts of tropical cyclone intensity and translation speed on ocean surface cooling. © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2023 |
| abstract_unstemmed |
Abstract The passage of tropical cyclones induces ocean surface cooling through vertical mixing, upwelling, and surface heat loss. The dependence of tropical cyclone-induced ocean surface cooling on the intensity and translation speed of tropical cyclones has been documented in previous studies. The present study investigates the latitudinal and seasonal variations in tropical cyclone-induced ocean surface cooling in the tropical western North Pacific based on data for the 2001–2020 period. Our analysis focuses on the open ocean (0°–25°N, 130°E–180°) to reduce the interference of coastal topography so that the obtained results better represent the influences of the intensity and translation speed of tropical cyclones. Our analysis confirms the dependence on the intensity and translation speed of tropical cyclone-induced cooling. The new findings are as follows. First, the time to reach the maximum cooling increases with the magnitude of the maximum cooling. Second, the magnitude of ocean surface cooling increases with latitude in the tropical region for tropical cyclones with different intensities and translation speeds. Third, the ocean surface cooling is larger in summer and autumn than in spring for tropical cyclones with different intensities and translation speeds. Fourth, the dependence of ocean surface cooling on the translation speed is more obvious at higher latitudes in the tropics and less apparent in spring. These new findings add to the existing knowledge of the impacts of tropical cyclone intensity and translation speed on ocean surface cooling. © The Chinese Meteorological Society and Springer-Verlag Berlin Heidelberg 2023 |
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Zhao, Ziyuan Wu, Renguang Zhu, Peijun |
| author2Str |
Zhao, Ziyuan Wu, Renguang Zhu, Peijun |
| ppnlink |
SPR031424376 |
| mediatype_str_mv |
c |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1007/s13351-023-3040-7 |
| up_date |
2024-07-04T01:05:03.607Z |
| _version_ |
1803608500321910784 |
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The dependence of tropical cyclone-induced ocean surface cooling on the intensity and translation speed of tropical cyclones has been documented in previous studies. The present study investigates the latitudinal and seasonal variations in tropical cyclone-induced ocean surface cooling in the tropical western North Pacific based on data for the 2001–2020 period. Our analysis focuses on the open ocean (0°–25°N, 130°E–180°) to reduce the interference of coastal topography so that the obtained results better represent the influences of the intensity and translation speed of tropical cyclones. Our analysis confirms the dependence on the intensity and translation speed of tropical cyclone-induced cooling. The new findings are as follows. First, the time to reach the maximum cooling increases with the magnitude of the maximum cooling. Second, the magnitude of ocean surface cooling increases with latitude in the tropical region for tropical cyclones with different intensities and translation speeds. Third, the ocean surface cooling is larger in summer and autumn than in spring for tropical cyclones with different intensities and translation speeds. Fourth, the dependence of ocean surface cooling on the translation speed is more obvious at higher latitudes in the tropics and less apparent in spring. These new findings add to the existing knowledge of the impacts of tropical cyclone intensity and translation speed on ocean surface cooling.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhao, Ziyuan</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wu, Renguang</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhu, Peijun</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Acta Meteorologica Sinica</subfield><subfield code="d">The Chinese Meteorological Society, 2011</subfield><subfield code="g">37(2023), 6 vom: Dez., Seite 790-801</subfield><subfield code="w">(DE-627)SPR031424376</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:37</subfield><subfield code="g">year:2023</subfield><subfield code="g">number:6</subfield><subfield code="g">month:12</subfield><subfield code="g">pages:790-801</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/s13351-023-3040-7</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_SPRINGER</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">37</subfield><subfield code="j">2023</subfield><subfield code="e">6</subfield><subfield code="c">12</subfield><subfield code="h">790-801</subfield></datafield></record></collection>
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7.402793 |