Statistical analysis of environmental parameters on the occurrences of tropical cyclones and earthquakes: an example from West North Pacific region
Abstract The nature of earthquake events and atmospheric factors’ response to the tropical cyclones (TCs) frequency during the boreal summer (June–July–August: JJA) season in the West North Pacific (WNP) is investigated using a 45-year (1977–2021) monthly dataset. The WNP is the most cyclonically ac...
Ausführliche Beschreibung
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| Autor*in: |
Pandey, Ravi Shankar [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2022 |
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| Schlagwörter: |
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| Anmerkung: |
© The Author(s), under exclusive licence to Springer Nature B.V. 2022. 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: Marine geophysical research - Dordrecht [u.a.] : Springer Science + Business Media B.V., 1970, 43(2022), 4 vom: 20. Nov. |
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| Übergeordnetes Werk: |
volume:43 ; year:2022 ; number:4 ; day:20 ; month:11 |
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| DOI / URN: |
10.1007/s11001-022-09505-w |
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| Katalog-ID: |
SPR048682128 |
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10.1007/s11001-022-09505-w doi (DE-627)SPR048682128 (SPR)s11001-022-09505-w-e DE-627 ger DE-627 rakwb eng Pandey, Ravi Shankar verfasserin aut Statistical analysis of environmental parameters on the occurrences of tropical cyclones and earthquakes: an example from West North Pacific region 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2022. 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 nature of earthquake events and atmospheric factors’ response to the tropical cyclones (TCs) frequency during the boreal summer (June–July–August: JJA) season in the West North Pacific (WNP) is investigated using a 45-year (1977–2021) monthly dataset. The WNP is the most cyclonically active basin on the globe and boreal summer alone accounts for its 42% of share. The WNP region encompasses the subduction zones between the Pacific and Philippine Sea plates, where 32% of boreal summer TCs cross these plates’ boundaries. Here I conduct statistical and GIS analyses of many environmental parameters on the occurrence of TCs in the WNP and seismicity along the plates’ boundaries. Years with frequent TCs in the WNP correlate with statistically significantly high seismicity in the lithosphere, assuming a 75 km (correl: 0.75) and a 120 km (correl: 0.75) lithospheres, respectively. TCs do not need to cross the plates’ boundaries to increase the seismicity (correl: 0.47 and 0.43 for 75 km and 120 km lithosphere, respectively), possibly due to the large spatial areas affected by each TC. Among the environmental parameters investigated, relative vorticity is strongly linked with TC frequency in the WNP in boreal summer showing a maximum percentage of variation during both extremely high and low TC years. Higher-level tropospheric winds (200 hPa) and vertical shear are found more dominant in extremely high-TC years while middle level tropospheric winds (850 hPa) and vertical velocity (omega) are found more commanding in extremely low-TC years. Other factors like sea surface temperature, relative humidity, outgoing longwave radiation, sea level pressure, etc. are also found mutually connected through the environmental and dynamical processes and as a result influence cyclogenesis. Results from this work suggest that few environmental parameters may dominantly control the extreme cyclogenesis, which then influences seismicity along submerged plates’ boundaries. Having the earthquakes and TCs as two major destruction casing natural hazards in the region, the presented results are very valuable. West North Pacific (dpeaa)DE-He213 Plate boundary (dpeaa)DE-He213 Tropical cyclone (dpeaa)DE-He213 Boreal summer (dpeaa)DE-He213 Cyclogenesis (dpeaa)DE-He213 Enthalten in Marine geophysical research Dordrecht [u.a.] : Springer Science + Business Media B.V., 1970 43(2022), 4 vom: 20. Nov. (DE-627)270930442 (DE-600)1478200-5 1573-0581 nnns volume:43 year:2022 number:4 day:20 month:11 https://dx.doi.org/10.1007/s11001-022-09505-w lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_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_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 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_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 AR 43 2022 4 20 11 |
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10.1007/s11001-022-09505-w doi (DE-627)SPR048682128 (SPR)s11001-022-09505-w-e DE-627 ger DE-627 rakwb eng Pandey, Ravi Shankar verfasserin aut Statistical analysis of environmental parameters on the occurrences of tropical cyclones and earthquakes: an example from West North Pacific region 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2022. 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 nature of earthquake events and atmospheric factors’ response to the tropical cyclones (TCs) frequency during the boreal summer (June–July–August: JJA) season in the West North Pacific (WNP) is investigated using a 45-year (1977–2021) monthly dataset. The WNP is the most cyclonically active basin on the globe and boreal summer alone accounts for its 42% of share. The WNP region encompasses the subduction zones between the Pacific and Philippine Sea plates, where 32% of boreal summer TCs cross these plates’ boundaries. Here I conduct statistical and GIS analyses of many environmental parameters on the occurrence of TCs in the WNP and seismicity along the plates’ boundaries. Years with frequent TCs in the WNP correlate with statistically significantly high seismicity in the lithosphere, assuming a 75 km (correl: 0.75) and a 120 km (correl: 0.75) lithospheres, respectively. TCs do not need to cross the plates’ boundaries to increase the seismicity (correl: 0.47 and 0.43 for 75 km and 120 km lithosphere, respectively), possibly due to the large spatial areas affected by each TC. Among the environmental parameters investigated, relative vorticity is strongly linked with TC frequency in the WNP in boreal summer showing a maximum percentage of variation during both extremely high and low TC years. Higher-level tropospheric winds (200 hPa) and vertical shear are found more dominant in extremely high-TC years while middle level tropospheric winds (850 hPa) and vertical velocity (omega) are found more commanding in extremely low-TC years. Other factors like sea surface temperature, relative humidity, outgoing longwave radiation, sea level pressure, etc. are also found mutually connected through the environmental and dynamical processes and as a result influence cyclogenesis. Results from this work suggest that few environmental parameters may dominantly control the extreme cyclogenesis, which then influences seismicity along submerged plates’ boundaries. Having the earthquakes and TCs as two major destruction casing natural hazards in the region, the presented results are very valuable. West North Pacific (dpeaa)DE-He213 Plate boundary (dpeaa)DE-He213 Tropical cyclone (dpeaa)DE-He213 Boreal summer (dpeaa)DE-He213 Cyclogenesis (dpeaa)DE-He213 Enthalten in Marine geophysical research Dordrecht [u.a.] : Springer Science + Business Media B.V., 1970 43(2022), 4 vom: 20. Nov. (DE-627)270930442 (DE-600)1478200-5 1573-0581 nnns volume:43 year:2022 number:4 day:20 month:11 https://dx.doi.org/10.1007/s11001-022-09505-w lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_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_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 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_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 AR 43 2022 4 20 11 |
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10.1007/s11001-022-09505-w doi (DE-627)SPR048682128 (SPR)s11001-022-09505-w-e DE-627 ger DE-627 rakwb eng Pandey, Ravi Shankar verfasserin aut Statistical analysis of environmental parameters on the occurrences of tropical cyclones and earthquakes: an example from West North Pacific region 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2022. 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 nature of earthquake events and atmospheric factors’ response to the tropical cyclones (TCs) frequency during the boreal summer (June–July–August: JJA) season in the West North Pacific (WNP) is investigated using a 45-year (1977–2021) monthly dataset. The WNP is the most cyclonically active basin on the globe and boreal summer alone accounts for its 42% of share. The WNP region encompasses the subduction zones between the Pacific and Philippine Sea plates, where 32% of boreal summer TCs cross these plates’ boundaries. Here I conduct statistical and GIS analyses of many environmental parameters on the occurrence of TCs in the WNP and seismicity along the plates’ boundaries. Years with frequent TCs in the WNP correlate with statistically significantly high seismicity in the lithosphere, assuming a 75 km (correl: 0.75) and a 120 km (correl: 0.75) lithospheres, respectively. TCs do not need to cross the plates’ boundaries to increase the seismicity (correl: 0.47 and 0.43 for 75 km and 120 km lithosphere, respectively), possibly due to the large spatial areas affected by each TC. Among the environmental parameters investigated, relative vorticity is strongly linked with TC frequency in the WNP in boreal summer showing a maximum percentage of variation during both extremely high and low TC years. Higher-level tropospheric winds (200 hPa) and vertical shear are found more dominant in extremely high-TC years while middle level tropospheric winds (850 hPa) and vertical velocity (omega) are found more commanding in extremely low-TC years. Other factors like sea surface temperature, relative humidity, outgoing longwave radiation, sea level pressure, etc. are also found mutually connected through the environmental and dynamical processes and as a result influence cyclogenesis. Results from this work suggest that few environmental parameters may dominantly control the extreme cyclogenesis, which then influences seismicity along submerged plates’ boundaries. Having the earthquakes and TCs as two major destruction casing natural hazards in the region, the presented results are very valuable. West North Pacific (dpeaa)DE-He213 Plate boundary (dpeaa)DE-He213 Tropical cyclone (dpeaa)DE-He213 Boreal summer (dpeaa)DE-He213 Cyclogenesis (dpeaa)DE-He213 Enthalten in Marine geophysical research Dordrecht [u.a.] : Springer Science + Business Media B.V., 1970 43(2022), 4 vom: 20. Nov. (DE-627)270930442 (DE-600)1478200-5 1573-0581 nnns volume:43 year:2022 number:4 day:20 month:11 https://dx.doi.org/10.1007/s11001-022-09505-w lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_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_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 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_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 AR 43 2022 4 20 11 |
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10.1007/s11001-022-09505-w doi (DE-627)SPR048682128 (SPR)s11001-022-09505-w-e DE-627 ger DE-627 rakwb eng Pandey, Ravi Shankar verfasserin aut Statistical analysis of environmental parameters on the occurrences of tropical cyclones and earthquakes: an example from West North Pacific region 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2022. 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 nature of earthquake events and atmospheric factors’ response to the tropical cyclones (TCs) frequency during the boreal summer (June–July–August: JJA) season in the West North Pacific (WNP) is investigated using a 45-year (1977–2021) monthly dataset. The WNP is the most cyclonically active basin on the globe and boreal summer alone accounts for its 42% of share. The WNP region encompasses the subduction zones between the Pacific and Philippine Sea plates, where 32% of boreal summer TCs cross these plates’ boundaries. Here I conduct statistical and GIS analyses of many environmental parameters on the occurrence of TCs in the WNP and seismicity along the plates’ boundaries. Years with frequent TCs in the WNP correlate with statistically significantly high seismicity in the lithosphere, assuming a 75 km (correl: 0.75) and a 120 km (correl: 0.75) lithospheres, respectively. TCs do not need to cross the plates’ boundaries to increase the seismicity (correl: 0.47 and 0.43 for 75 km and 120 km lithosphere, respectively), possibly due to the large spatial areas affected by each TC. Among the environmental parameters investigated, relative vorticity is strongly linked with TC frequency in the WNP in boreal summer showing a maximum percentage of variation during both extremely high and low TC years. Higher-level tropospheric winds (200 hPa) and vertical shear are found more dominant in extremely high-TC years while middle level tropospheric winds (850 hPa) and vertical velocity (omega) are found more commanding in extremely low-TC years. Other factors like sea surface temperature, relative humidity, outgoing longwave radiation, sea level pressure, etc. are also found mutually connected through the environmental and dynamical processes and as a result influence cyclogenesis. Results from this work suggest that few environmental parameters may dominantly control the extreme cyclogenesis, which then influences seismicity along submerged plates’ boundaries. Having the earthquakes and TCs as two major destruction casing natural hazards in the region, the presented results are very valuable. West North Pacific (dpeaa)DE-He213 Plate boundary (dpeaa)DE-He213 Tropical cyclone (dpeaa)DE-He213 Boreal summer (dpeaa)DE-He213 Cyclogenesis (dpeaa)DE-He213 Enthalten in Marine geophysical research Dordrecht [u.a.] : Springer Science + Business Media B.V., 1970 43(2022), 4 vom: 20. Nov. (DE-627)270930442 (DE-600)1478200-5 1573-0581 nnns volume:43 year:2022 number:4 day:20 month:11 https://dx.doi.org/10.1007/s11001-022-09505-w lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_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_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 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_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 AR 43 2022 4 20 11 |
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10.1007/s11001-022-09505-w doi (DE-627)SPR048682128 (SPR)s11001-022-09505-w-e DE-627 ger DE-627 rakwb eng Pandey, Ravi Shankar verfasserin aut Statistical analysis of environmental parameters on the occurrences of tropical cyclones and earthquakes: an example from West North Pacific region 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2022. 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 nature of earthquake events and atmospheric factors’ response to the tropical cyclones (TCs) frequency during the boreal summer (June–July–August: JJA) season in the West North Pacific (WNP) is investigated using a 45-year (1977–2021) monthly dataset. The WNP is the most cyclonically active basin on the globe and boreal summer alone accounts for its 42% of share. The WNP region encompasses the subduction zones between the Pacific and Philippine Sea plates, where 32% of boreal summer TCs cross these plates’ boundaries. Here I conduct statistical and GIS analyses of many environmental parameters on the occurrence of TCs in the WNP and seismicity along the plates’ boundaries. Years with frequent TCs in the WNP correlate with statistically significantly high seismicity in the lithosphere, assuming a 75 km (correl: 0.75) and a 120 km (correl: 0.75) lithospheres, respectively. TCs do not need to cross the plates’ boundaries to increase the seismicity (correl: 0.47 and 0.43 for 75 km and 120 km lithosphere, respectively), possibly due to the large spatial areas affected by each TC. Among the environmental parameters investigated, relative vorticity is strongly linked with TC frequency in the WNP in boreal summer showing a maximum percentage of variation during both extremely high and low TC years. Higher-level tropospheric winds (200 hPa) and vertical shear are found more dominant in extremely high-TC years while middle level tropospheric winds (850 hPa) and vertical velocity (omega) are found more commanding in extremely low-TC years. Other factors like sea surface temperature, relative humidity, outgoing longwave radiation, sea level pressure, etc. are also found mutually connected through the environmental and dynamical processes and as a result influence cyclogenesis. Results from this work suggest that few environmental parameters may dominantly control the extreme cyclogenesis, which then influences seismicity along submerged plates’ boundaries. Having the earthquakes and TCs as two major destruction casing natural hazards in the region, the presented results are very valuable. West North Pacific (dpeaa)DE-He213 Plate boundary (dpeaa)DE-He213 Tropical cyclone (dpeaa)DE-He213 Boreal summer (dpeaa)DE-He213 Cyclogenesis (dpeaa)DE-He213 Enthalten in Marine geophysical research Dordrecht [u.a.] : Springer Science + Business Media B.V., 1970 43(2022), 4 vom: 20. Nov. (DE-627)270930442 (DE-600)1478200-5 1573-0581 nnns volume:43 year:2022 number:4 day:20 month:11 https://dx.doi.org/10.1007/s11001-022-09505-w lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER 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_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_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 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_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 AR 43 2022 4 20 11 |
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Pandey, Ravi Shankar |
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Pandey, Ravi Shankar misc West North Pacific misc Plate boundary misc Tropical cyclone misc Boreal summer misc Cyclogenesis Statistical analysis of environmental parameters on the occurrences of tropical cyclones and earthquakes: an example from West North Pacific region |
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Statistical analysis of environmental parameters on the occurrences of tropical cyclones and earthquakes: an example from West North Pacific region West North Pacific (dpeaa)DE-He213 Plate boundary (dpeaa)DE-He213 Tropical cyclone (dpeaa)DE-He213 Boreal summer (dpeaa)DE-He213 Cyclogenesis (dpeaa)DE-He213 |
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statistical analysis of environmental parameters on the occurrences of tropical cyclones and earthquakes: an example from west north pacific region |
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Statistical analysis of environmental parameters on the occurrences of tropical cyclones and earthquakes: an example from West North Pacific region |
| abstract |
Abstract The nature of earthquake events and atmospheric factors’ response to the tropical cyclones (TCs) frequency during the boreal summer (June–July–August: JJA) season in the West North Pacific (WNP) is investigated using a 45-year (1977–2021) monthly dataset. The WNP is the most cyclonically active basin on the globe and boreal summer alone accounts for its 42% of share. The WNP region encompasses the subduction zones between the Pacific and Philippine Sea plates, where 32% of boreal summer TCs cross these plates’ boundaries. Here I conduct statistical and GIS analyses of many environmental parameters on the occurrence of TCs in the WNP and seismicity along the plates’ boundaries. Years with frequent TCs in the WNP correlate with statistically significantly high seismicity in the lithosphere, assuming a 75 km (correl: 0.75) and a 120 km (correl: 0.75) lithospheres, respectively. TCs do not need to cross the plates’ boundaries to increase the seismicity (correl: 0.47 and 0.43 for 75 km and 120 km lithosphere, respectively), possibly due to the large spatial areas affected by each TC. Among the environmental parameters investigated, relative vorticity is strongly linked with TC frequency in the WNP in boreal summer showing a maximum percentage of variation during both extremely high and low TC years. Higher-level tropospheric winds (200 hPa) and vertical shear are found more dominant in extremely high-TC years while middle level tropospheric winds (850 hPa) and vertical velocity (omega) are found more commanding in extremely low-TC years. Other factors like sea surface temperature, relative humidity, outgoing longwave radiation, sea level pressure, etc. are also found mutually connected through the environmental and dynamical processes and as a result influence cyclogenesis. Results from this work suggest that few environmental parameters may dominantly control the extreme cyclogenesis, which then influences seismicity along submerged plates’ boundaries. Having the earthquakes and TCs as two major destruction casing natural hazards in the region, the presented results are very valuable. © The Author(s), under exclusive licence to Springer Nature B.V. 2022. 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 nature of earthquake events and atmospheric factors’ response to the tropical cyclones (TCs) frequency during the boreal summer (June–July–August: JJA) season in the West North Pacific (WNP) is investigated using a 45-year (1977–2021) monthly dataset. The WNP is the most cyclonically active basin on the globe and boreal summer alone accounts for its 42% of share. The WNP region encompasses the subduction zones between the Pacific and Philippine Sea plates, where 32% of boreal summer TCs cross these plates’ boundaries. Here I conduct statistical and GIS analyses of many environmental parameters on the occurrence of TCs in the WNP and seismicity along the plates’ boundaries. Years with frequent TCs in the WNP correlate with statistically significantly high seismicity in the lithosphere, assuming a 75 km (correl: 0.75) and a 120 km (correl: 0.75) lithospheres, respectively. TCs do not need to cross the plates’ boundaries to increase the seismicity (correl: 0.47 and 0.43 for 75 km and 120 km lithosphere, respectively), possibly due to the large spatial areas affected by each TC. Among the environmental parameters investigated, relative vorticity is strongly linked with TC frequency in the WNP in boreal summer showing a maximum percentage of variation during both extremely high and low TC years. Higher-level tropospheric winds (200 hPa) and vertical shear are found more dominant in extremely high-TC years while middle level tropospheric winds (850 hPa) and vertical velocity (omega) are found more commanding in extremely low-TC years. Other factors like sea surface temperature, relative humidity, outgoing longwave radiation, sea level pressure, etc. are also found mutually connected through the environmental and dynamical processes and as a result influence cyclogenesis. Results from this work suggest that few environmental parameters may dominantly control the extreme cyclogenesis, which then influences seismicity along submerged plates’ boundaries. Having the earthquakes and TCs as two major destruction casing natural hazards in the region, the presented results are very valuable. © The Author(s), under exclusive licence to Springer Nature B.V. 2022. 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 nature of earthquake events and atmospheric factors’ response to the tropical cyclones (TCs) frequency during the boreal summer (June–July–August: JJA) season in the West North Pacific (WNP) is investigated using a 45-year (1977–2021) monthly dataset. The WNP is the most cyclonically active basin on the globe and boreal summer alone accounts for its 42% of share. The WNP region encompasses the subduction zones between the Pacific and Philippine Sea plates, where 32% of boreal summer TCs cross these plates’ boundaries. Here I conduct statistical and GIS analyses of many environmental parameters on the occurrence of TCs in the WNP and seismicity along the plates’ boundaries. Years with frequent TCs in the WNP correlate with statistically significantly high seismicity in the lithosphere, assuming a 75 km (correl: 0.75) and a 120 km (correl: 0.75) lithospheres, respectively. TCs do not need to cross the plates’ boundaries to increase the seismicity (correl: 0.47 and 0.43 for 75 km and 120 km lithosphere, respectively), possibly due to the large spatial areas affected by each TC. Among the environmental parameters investigated, relative vorticity is strongly linked with TC frequency in the WNP in boreal summer showing a maximum percentage of variation during both extremely high and low TC years. Higher-level tropospheric winds (200 hPa) and vertical shear are found more dominant in extremely high-TC years while middle level tropospheric winds (850 hPa) and vertical velocity (omega) are found more commanding in extremely low-TC years. Other factors like sea surface temperature, relative humidity, outgoing longwave radiation, sea level pressure, etc. are also found mutually connected through the environmental and dynamical processes and as a result influence cyclogenesis. Results from this work suggest that few environmental parameters may dominantly control the extreme cyclogenesis, which then influences seismicity along submerged plates’ boundaries. Having the earthquakes and TCs as two major destruction casing natural hazards in the region, the presented results are very valuable. © The Author(s), under exclusive licence to Springer Nature B.V. 2022. 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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Statistical analysis of environmental parameters on the occurrences of tropical cyclones and earthquakes: an example from West North Pacific region |
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https://dx.doi.org/10.1007/s11001-022-09505-w |
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| score |
7.400876 |