Impact of the Pacific-Japan pattern on the tropical Indo-western Pacific Ocean surface waves
Abstract The present study examines the impact of the Pacific-Japan (PJ) pattern on tropical Indo–Western Pacific Ocean significant wave heights during the boreal summer season (June through August, JJA) for the first time. The PJ pattern is a dominant teleconnection pattern characterized by meridio...
Ausführliche Beschreibung
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| Autor*in: |
Srinivas, G. [verfasserIn] Remya, P. G. [verfasserIn] Dey, Subhra Prakash [verfasserIn] Chowdary, Jasti S. [verfasserIn] Kumar, Prashant [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2024 |
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| Schlagwörter: |
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| Anmerkung: |
© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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| Übergeordnetes Werk: |
Enthalten in: Climate dynamics - Springer Berlin Heidelberg, 1986, 62(2024), 9 vom: 02. Aug., Seite 8729-8740 |
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| Übergeordnetes Werk: |
volume:62 ; year:2024 ; number:9 ; day:02 ; month:08 ; pages:8729-8740 |
| Links: |
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| DOI / URN: |
10.1007/s00382-024-07357-1 |
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| Katalog-ID: |
SPR057454191 |
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| 520 | |a Abstract The present study examines the impact of the Pacific-Japan (PJ) pattern on tropical Indo–Western Pacific Ocean significant wave heights during the boreal summer season (June through August, JJA) for the first time. The PJ pattern is a dominant teleconnection pattern characterized by meridional propagating Rossby waves over the Western North Pacific (WNP) and East Asia. The strong southwesterly monsoon winds prevail over the North Indian Ocean (NIO) during JJA inducing strong wave heights in the mean state. The regression analysis of significant wave height anomalies on the PJ index exhibits strong negative wave height anomalies over the Bay of Bengal (BoB), the tropical WNP region and slightly weaker negative anomalies over the Arabian Sea (AS) due to a reduction in the wind-wave growth. The weakening of wave heights in the BoB and WNP regions during PJ is attributed to the anomalous low-level anticyclonic circulation accompanied by high sea-level pressure anomalies over the BoB and WNP regions. The anomalous anticyclonic circulation opposes the mean south-westerlies and reduces the wave heights over the NIO and WNP. Further, the composite analysis of positive and negative PJ patterns display significant asymmetries in their signature on the wind and wave parameters. Thus, our findings suggest that the WNP region’s climate conditions strongly modulate the NIO’s surface waves. | ||
| 650 | 4 | |a Significant wave heights |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Pacific-Japan pattern |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Anomalous anticyclonic circulation |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a North Indian Ocean |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Western North Pacific |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Remya, P. G. |e verfasserin |4 aut | |
| 700 | 1 | |a Dey, Subhra Prakash |e verfasserin |4 aut | |
| 700 | 1 | |a Chowdary, Jasti S. |e verfasserin |4 aut | |
| 700 | 1 | |a Kumar, Prashant |e verfasserin |4 aut | |
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10.1007/s00382-024-07357-1 doi (DE-627)SPR057454191 (SPR)s00382-024-07357-1-e DE-627 ger DE-627 rakwb eng 550 VZ 38.80 bkl Srinivas, G. verfasserin aut Impact of the Pacific-Japan pattern on the tropical Indo-western Pacific Ocean surface waves 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract The present study examines the impact of the Pacific-Japan (PJ) pattern on tropical Indo–Western Pacific Ocean significant wave heights during the boreal summer season (June through August, JJA) for the first time. The PJ pattern is a dominant teleconnection pattern characterized by meridional propagating Rossby waves over the Western North Pacific (WNP) and East Asia. The strong southwesterly monsoon winds prevail over the North Indian Ocean (NIO) during JJA inducing strong wave heights in the mean state. The regression analysis of significant wave height anomalies on the PJ index exhibits strong negative wave height anomalies over the Bay of Bengal (BoB), the tropical WNP region and slightly weaker negative anomalies over the Arabian Sea (AS) due to a reduction in the wind-wave growth. The weakening of wave heights in the BoB and WNP regions during PJ is attributed to the anomalous low-level anticyclonic circulation accompanied by high sea-level pressure anomalies over the BoB and WNP regions. The anomalous anticyclonic circulation opposes the mean south-westerlies and reduces the wave heights over the NIO and WNP. Further, the composite analysis of positive and negative PJ patterns display significant asymmetries in their signature on the wind and wave parameters. Thus, our findings suggest that the WNP region’s climate conditions strongly modulate the NIO’s surface waves. Significant wave heights (dpeaa)DE-He213 Pacific-Japan pattern (dpeaa)DE-He213 Anomalous anticyclonic circulation (dpeaa)DE-He213 North Indian Ocean (dpeaa)DE-He213 Western North Pacific (dpeaa)DE-He213 Remya, P. G. verfasserin aut Dey, Subhra Prakash verfasserin aut Chowdary, Jasti S. verfasserin aut Kumar, Prashant verfasserin aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 62(2024), 9 vom: 02. Aug., Seite 8729-8740 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:62 year:2024 number:9 day:02 month:08 pages:8729-8740 https://dx.doi.org/10.1007/s00382-024-07357-1 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_72 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_612 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2574 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 VZ AR 62 2024 9 02 08 8729-8740 |
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10.1007/s00382-024-07357-1 doi (DE-627)SPR057454191 (SPR)s00382-024-07357-1-e DE-627 ger DE-627 rakwb eng 550 VZ 38.80 bkl Srinivas, G. verfasserin aut Impact of the Pacific-Japan pattern on the tropical Indo-western Pacific Ocean surface waves 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract The present study examines the impact of the Pacific-Japan (PJ) pattern on tropical Indo–Western Pacific Ocean significant wave heights during the boreal summer season (June through August, JJA) for the first time. The PJ pattern is a dominant teleconnection pattern characterized by meridional propagating Rossby waves over the Western North Pacific (WNP) and East Asia. The strong southwesterly monsoon winds prevail over the North Indian Ocean (NIO) during JJA inducing strong wave heights in the mean state. The regression analysis of significant wave height anomalies on the PJ index exhibits strong negative wave height anomalies over the Bay of Bengal (BoB), the tropical WNP region and slightly weaker negative anomalies over the Arabian Sea (AS) due to a reduction in the wind-wave growth. The weakening of wave heights in the BoB and WNP regions during PJ is attributed to the anomalous low-level anticyclonic circulation accompanied by high sea-level pressure anomalies over the BoB and WNP regions. The anomalous anticyclonic circulation opposes the mean south-westerlies and reduces the wave heights over the NIO and WNP. Further, the composite analysis of positive and negative PJ patterns display significant asymmetries in their signature on the wind and wave parameters. Thus, our findings suggest that the WNP region’s climate conditions strongly modulate the NIO’s surface waves. Significant wave heights (dpeaa)DE-He213 Pacific-Japan pattern (dpeaa)DE-He213 Anomalous anticyclonic circulation (dpeaa)DE-He213 North Indian Ocean (dpeaa)DE-He213 Western North Pacific (dpeaa)DE-He213 Remya, P. G. verfasserin aut Dey, Subhra Prakash verfasserin aut Chowdary, Jasti S. verfasserin aut Kumar, Prashant verfasserin aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 62(2024), 9 vom: 02. Aug., Seite 8729-8740 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:62 year:2024 number:9 day:02 month:08 pages:8729-8740 https://dx.doi.org/10.1007/s00382-024-07357-1 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_72 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_612 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2574 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 VZ AR 62 2024 9 02 08 8729-8740 |
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10.1007/s00382-024-07357-1 doi (DE-627)SPR057454191 (SPR)s00382-024-07357-1-e DE-627 ger DE-627 rakwb eng 550 VZ 38.80 bkl Srinivas, G. verfasserin aut Impact of the Pacific-Japan pattern on the tropical Indo-western Pacific Ocean surface waves 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract The present study examines the impact of the Pacific-Japan (PJ) pattern on tropical Indo–Western Pacific Ocean significant wave heights during the boreal summer season (June through August, JJA) for the first time. The PJ pattern is a dominant teleconnection pattern characterized by meridional propagating Rossby waves over the Western North Pacific (WNP) and East Asia. The strong southwesterly monsoon winds prevail over the North Indian Ocean (NIO) during JJA inducing strong wave heights in the mean state. The regression analysis of significant wave height anomalies on the PJ index exhibits strong negative wave height anomalies over the Bay of Bengal (BoB), the tropical WNP region and slightly weaker negative anomalies over the Arabian Sea (AS) due to a reduction in the wind-wave growth. The weakening of wave heights in the BoB and WNP regions during PJ is attributed to the anomalous low-level anticyclonic circulation accompanied by high sea-level pressure anomalies over the BoB and WNP regions. The anomalous anticyclonic circulation opposes the mean south-westerlies and reduces the wave heights over the NIO and WNP. Further, the composite analysis of positive and negative PJ patterns display significant asymmetries in their signature on the wind and wave parameters. Thus, our findings suggest that the WNP region’s climate conditions strongly modulate the NIO’s surface waves. Significant wave heights (dpeaa)DE-He213 Pacific-Japan pattern (dpeaa)DE-He213 Anomalous anticyclonic circulation (dpeaa)DE-He213 North Indian Ocean (dpeaa)DE-He213 Western North Pacific (dpeaa)DE-He213 Remya, P. G. verfasserin aut Dey, Subhra Prakash verfasserin aut Chowdary, Jasti S. verfasserin aut Kumar, Prashant verfasserin aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 62(2024), 9 vom: 02. Aug., Seite 8729-8740 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:62 year:2024 number:9 day:02 month:08 pages:8729-8740 https://dx.doi.org/10.1007/s00382-024-07357-1 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_72 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_612 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2574 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 VZ AR 62 2024 9 02 08 8729-8740 |
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10.1007/s00382-024-07357-1 doi (DE-627)SPR057454191 (SPR)s00382-024-07357-1-e DE-627 ger DE-627 rakwb eng 550 VZ 38.80 bkl Srinivas, G. verfasserin aut Impact of the Pacific-Japan pattern on the tropical Indo-western Pacific Ocean surface waves 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract The present study examines the impact of the Pacific-Japan (PJ) pattern on tropical Indo–Western Pacific Ocean significant wave heights during the boreal summer season (June through August, JJA) for the first time. The PJ pattern is a dominant teleconnection pattern characterized by meridional propagating Rossby waves over the Western North Pacific (WNP) and East Asia. The strong southwesterly monsoon winds prevail over the North Indian Ocean (NIO) during JJA inducing strong wave heights in the mean state. The regression analysis of significant wave height anomalies on the PJ index exhibits strong negative wave height anomalies over the Bay of Bengal (BoB), the tropical WNP region and slightly weaker negative anomalies over the Arabian Sea (AS) due to a reduction in the wind-wave growth. The weakening of wave heights in the BoB and WNP regions during PJ is attributed to the anomalous low-level anticyclonic circulation accompanied by high sea-level pressure anomalies over the BoB and WNP regions. The anomalous anticyclonic circulation opposes the mean south-westerlies and reduces the wave heights over the NIO and WNP. Further, the composite analysis of positive and negative PJ patterns display significant asymmetries in their signature on the wind and wave parameters. Thus, our findings suggest that the WNP region’s climate conditions strongly modulate the NIO’s surface waves. Significant wave heights (dpeaa)DE-He213 Pacific-Japan pattern (dpeaa)DE-He213 Anomalous anticyclonic circulation (dpeaa)DE-He213 North Indian Ocean (dpeaa)DE-He213 Western North Pacific (dpeaa)DE-He213 Remya, P. G. verfasserin aut Dey, Subhra Prakash verfasserin aut Chowdary, Jasti S. verfasserin aut Kumar, Prashant verfasserin aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 62(2024), 9 vom: 02. Aug., Seite 8729-8740 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:62 year:2024 number:9 day:02 month:08 pages:8729-8740 https://dx.doi.org/10.1007/s00382-024-07357-1 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_72 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_612 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2574 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 VZ AR 62 2024 9 02 08 8729-8740 |
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10.1007/s00382-024-07357-1 doi (DE-627)SPR057454191 (SPR)s00382-024-07357-1-e DE-627 ger DE-627 rakwb eng 550 VZ 38.80 bkl Srinivas, G. verfasserin aut Impact of the Pacific-Japan pattern on the tropical Indo-western Pacific Ocean surface waves 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract The present study examines the impact of the Pacific-Japan (PJ) pattern on tropical Indo–Western Pacific Ocean significant wave heights during the boreal summer season (June through August, JJA) for the first time. The PJ pattern is a dominant teleconnection pattern characterized by meridional propagating Rossby waves over the Western North Pacific (WNP) and East Asia. The strong southwesterly monsoon winds prevail over the North Indian Ocean (NIO) during JJA inducing strong wave heights in the mean state. The regression analysis of significant wave height anomalies on the PJ index exhibits strong negative wave height anomalies over the Bay of Bengal (BoB), the tropical WNP region and slightly weaker negative anomalies over the Arabian Sea (AS) due to a reduction in the wind-wave growth. The weakening of wave heights in the BoB and WNP regions during PJ is attributed to the anomalous low-level anticyclonic circulation accompanied by high sea-level pressure anomalies over the BoB and WNP regions. The anomalous anticyclonic circulation opposes the mean south-westerlies and reduces the wave heights over the NIO and WNP. Further, the composite analysis of positive and negative PJ patterns display significant asymmetries in their signature on the wind and wave parameters. Thus, our findings suggest that the WNP region’s climate conditions strongly modulate the NIO’s surface waves. Significant wave heights (dpeaa)DE-He213 Pacific-Japan pattern (dpeaa)DE-He213 Anomalous anticyclonic circulation (dpeaa)DE-He213 North Indian Ocean (dpeaa)DE-He213 Western North Pacific (dpeaa)DE-He213 Remya, P. G. verfasserin aut Dey, Subhra Prakash verfasserin aut Chowdary, Jasti S. verfasserin aut Kumar, Prashant verfasserin aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 62(2024), 9 vom: 02. Aug., Seite 8729-8740 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:62 year:2024 number:9 day:02 month:08 pages:8729-8740 https://dx.doi.org/10.1007/s00382-024-07357-1 X:SPRINGER Resolving-System lizenzpflichtig Volltext SYSFLAG_0 GBV_SPRINGER SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_72 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_612 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_2574 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.80 VZ AR 62 2024 9 02 08 8729-8740 |
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Srinivas, G. @@aut@@ Remya, P. G. @@aut@@ Dey, Subhra Prakash @@aut@@ Chowdary, Jasti S. @@aut@@ Kumar, Prashant @@aut@@ |
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Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The present study examines the impact of the Pacific-Japan (PJ) pattern on tropical Indo–Western Pacific Ocean significant wave heights during the boreal summer season (June through August, JJA) for the first time. The PJ pattern is a dominant teleconnection pattern characterized by meridional propagating Rossby waves over the Western North Pacific (WNP) and East Asia. The strong southwesterly monsoon winds prevail over the North Indian Ocean (NIO) during JJA inducing strong wave heights in the mean state. The regression analysis of significant wave height anomalies on the PJ index exhibits strong negative wave height anomalies over the Bay of Bengal (BoB), the tropical WNP region and slightly weaker negative anomalies over the Arabian Sea (AS) due to a reduction in the wind-wave growth. The weakening of wave heights in the BoB and WNP regions during PJ is attributed to the anomalous low-level anticyclonic circulation accompanied by high sea-level pressure anomalies over the BoB and WNP regions. The anomalous anticyclonic circulation opposes the mean south-westerlies and reduces the wave heights over the NIO and WNP. Further, the composite analysis of positive and negative PJ patterns display significant asymmetries in their signature on the wind and wave parameters. 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Srinivas, G. |
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Srinivas, G. ddc 550 bkl 38.80 misc Significant wave heights misc Pacific-Japan pattern misc Anomalous anticyclonic circulation misc North Indian Ocean misc Western North Pacific Impact of the Pacific-Japan pattern on the tropical Indo-western Pacific Ocean surface waves |
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550 VZ 38.80 bkl Impact of the Pacific-Japan pattern on the tropical Indo-western Pacific Ocean surface waves Significant wave heights (dpeaa)DE-He213 Pacific-Japan pattern (dpeaa)DE-He213 Anomalous anticyclonic circulation (dpeaa)DE-He213 North Indian Ocean (dpeaa)DE-He213 Western North Pacific (dpeaa)DE-He213 |
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Impact of the Pacific-Japan pattern on the tropical Indo-western Pacific Ocean surface waves |
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Impact of the Pacific-Japan pattern on the tropical Indo-western Pacific Ocean surface waves |
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Srinivas, G. Remya, P. G. Dey, Subhra Prakash Chowdary, Jasti S. Kumar, Prashant |
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impact of the pacific-japan pattern on the tropical indo-western pacific ocean surface waves |
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Impact of the Pacific-Japan pattern on the tropical Indo-western Pacific Ocean surface waves |
| abstract |
Abstract The present study examines the impact of the Pacific-Japan (PJ) pattern on tropical Indo–Western Pacific Ocean significant wave heights during the boreal summer season (June through August, JJA) for the first time. The PJ pattern is a dominant teleconnection pattern characterized by meridional propagating Rossby waves over the Western North Pacific (WNP) and East Asia. The strong southwesterly monsoon winds prevail over the North Indian Ocean (NIO) during JJA inducing strong wave heights in the mean state. The regression analysis of significant wave height anomalies on the PJ index exhibits strong negative wave height anomalies over the Bay of Bengal (BoB), the tropical WNP region and slightly weaker negative anomalies over the Arabian Sea (AS) due to a reduction in the wind-wave growth. The weakening of wave heights in the BoB and WNP regions during PJ is attributed to the anomalous low-level anticyclonic circulation accompanied by high sea-level pressure anomalies over the BoB and WNP regions. The anomalous anticyclonic circulation opposes the mean south-westerlies and reduces the wave heights over the NIO and WNP. Further, the composite analysis of positive and negative PJ patterns display significant asymmetries in their signature on the wind and wave parameters. Thus, our findings suggest that the WNP region’s climate conditions strongly modulate the NIO’s surface waves. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
| abstractGer |
Abstract The present study examines the impact of the Pacific-Japan (PJ) pattern on tropical Indo–Western Pacific Ocean significant wave heights during the boreal summer season (June through August, JJA) for the first time. The PJ pattern is a dominant teleconnection pattern characterized by meridional propagating Rossby waves over the Western North Pacific (WNP) and East Asia. The strong southwesterly monsoon winds prevail over the North Indian Ocean (NIO) during JJA inducing strong wave heights in the mean state. The regression analysis of significant wave height anomalies on the PJ index exhibits strong negative wave height anomalies over the Bay of Bengal (BoB), the tropical WNP region and slightly weaker negative anomalies over the Arabian Sea (AS) due to a reduction in the wind-wave growth. The weakening of wave heights in the BoB and WNP regions during PJ is attributed to the anomalous low-level anticyclonic circulation accompanied by high sea-level pressure anomalies over the BoB and WNP regions. The anomalous anticyclonic circulation opposes the mean south-westerlies and reduces the wave heights over the NIO and WNP. Further, the composite analysis of positive and negative PJ patterns display significant asymmetries in their signature on the wind and wave parameters. Thus, our findings suggest that the WNP region’s climate conditions strongly modulate the NIO’s surface waves. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
| abstract_unstemmed |
Abstract The present study examines the impact of the Pacific-Japan (PJ) pattern on tropical Indo–Western Pacific Ocean significant wave heights during the boreal summer season (June through August, JJA) for the first time. The PJ pattern is a dominant teleconnection pattern characterized by meridional propagating Rossby waves over the Western North Pacific (WNP) and East Asia. The strong southwesterly monsoon winds prevail over the North Indian Ocean (NIO) during JJA inducing strong wave heights in the mean state. The regression analysis of significant wave height anomalies on the PJ index exhibits strong negative wave height anomalies over the Bay of Bengal (BoB), the tropical WNP region and slightly weaker negative anomalies over the Arabian Sea (AS) due to a reduction in the wind-wave growth. The weakening of wave heights in the BoB and WNP regions during PJ is attributed to the anomalous low-level anticyclonic circulation accompanied by high sea-level pressure anomalies over the BoB and WNP regions. The anomalous anticyclonic circulation opposes the mean south-westerlies and reduces the wave heights over the NIO and WNP. Further, the composite analysis of positive and negative PJ patterns display significant asymmetries in their signature on the wind and wave parameters. Thus, our findings suggest that the WNP region’s climate conditions strongly modulate the NIO’s surface waves. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2024. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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Impact of the Pacific-Japan pattern on the tropical Indo-western Pacific Ocean surface waves |
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| score |
7.399678 |