Change of boreal winter dominant ENSO teleconnection modulated by the East Asian westerly jet strength

Abstract This study reveals an interdecadal change in boreal winter dominant ENSO atmospheric teleconnection and demonstrates its underlying physical mechanism. During the period 1960–2020, the ENSO teleconnection was characterized by the Western Pacific (WP) pattern and the Pacific–North American (...
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Gespeichert in:

Autor*in:	Mao, Jingdan [verfasserIn] Zhu, Zhiwei [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2024

Schlagwörter:	Pacific–North American pattern Western Pacific pattern Westerly jet stream ENSO teleconnection

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.

Übergeordnetes Werk:	Enthalten in: Climate dynamics - Springer Berlin Heidelberg, 1986, 62(2024), 7 vom: 06. Mai, Seite 6985-7000
Übergeordnetes Werk:	volume:62 ; year:2024 ; number:7 ; day:06 ; month:05 ; pages:6985-7000

Links:	Volltext

DOI / URN:	10.1007/s00382-024-07261-8

Katalog-ID:	SPR057423202

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912			\|a GBV_ILN_213
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912			\|a GBV_ILN_281
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author_variant	j m jm z z zz
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bklnumber	38.80
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allfields	10.1007/s00382-024-07261-8 doi (DE-627)SPR057423202 (SPR)s00382-024-07261-8-e DE-627 ger DE-627 rakwb eng 550 VZ 38.80 bkl Mao, Jingdan verfasserin aut Change of boreal winter dominant ENSO teleconnection modulated by the East Asian westerly jet strength 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 This study reveals an interdecadal change in boreal winter dominant ENSO atmospheric teleconnection and demonstrates its underlying physical mechanism. During the period 1960–2020, the ENSO teleconnection was characterized by the Western Pacific (WP) pattern and the Pacific–North American (PNA) pattern, but the dominant pattern of ENSO teleconnection witnessed an alternation at around early 1980s. In the first epoch of 1960–1979 (E1), the ENSO teleconnection was mainly dominated by the WP pattern with an inhibited PNA pattern, whereas in the second epoch of 1987–2020 (E2), the ENSO teleconnection was dominated by the PNA pattern without a prominent WP pattern. It is further suggested that the changing strength of the westerly jet, rather than the pattern of the ENSO-related tropical convection, played the critical role in the alternation of the winter dominant ENSO teleconnection. During E1, because the westerly jet stream in the East Asia–North Pacific sector was relatively weak, poleward propagation of the Rossby wave train from the western Pacific was evident, forming the dominant WP pattern related to ENSO. In E2, because the westerly jet in the region largely strengthened, the PNA pattern was dominant owing to the enhanced zonal waveguide of the westerly jet. Evidence from a set of numerical experiments and the simulations of CMIP6 models supports the important role of the westerly jet strength in shaping the ENSO teleconnection. Pacific–North American pattern (dpeaa)DE-He213 Western Pacific pattern (dpeaa)DE-He213 Westerly jet stream (dpeaa)DE-He213 ENSO teleconnection (dpeaa)DE-He213 Zhu, Zhiwei verfasserin (orcid)0000-0002-4885-1299 aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 62(2024), 7 vom: 06. Mai, Seite 6985-7000 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:62 year:2024 number:7 day:06 month:05 pages:6985-7000 https://dx.doi.org/10.1007/s00382-024-07261-8 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 7 06 05 6985-7000
spelling	10.1007/s00382-024-07261-8 doi (DE-627)SPR057423202 (SPR)s00382-024-07261-8-e DE-627 ger DE-627 rakwb eng 550 VZ 38.80 bkl Mao, Jingdan verfasserin aut Change of boreal winter dominant ENSO teleconnection modulated by the East Asian westerly jet strength 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 This study reveals an interdecadal change in boreal winter dominant ENSO atmospheric teleconnection and demonstrates its underlying physical mechanism. During the period 1960–2020, the ENSO teleconnection was characterized by the Western Pacific (WP) pattern and the Pacific–North American (PNA) pattern, but the dominant pattern of ENSO teleconnection witnessed an alternation at around early 1980s. In the first epoch of 1960–1979 (E1), the ENSO teleconnection was mainly dominated by the WP pattern with an inhibited PNA pattern, whereas in the second epoch of 1987–2020 (E2), the ENSO teleconnection was dominated by the PNA pattern without a prominent WP pattern. It is further suggested that the changing strength of the westerly jet, rather than the pattern of the ENSO-related tropical convection, played the critical role in the alternation of the winter dominant ENSO teleconnection. During E1, because the westerly jet stream in the East Asia–North Pacific sector was relatively weak, poleward propagation of the Rossby wave train from the western Pacific was evident, forming the dominant WP pattern related to ENSO. In E2, because the westerly jet in the region largely strengthened, the PNA pattern was dominant owing to the enhanced zonal waveguide of the westerly jet. Evidence from a set of numerical experiments and the simulations of CMIP6 models supports the important role of the westerly jet strength in shaping the ENSO teleconnection. Pacific–North American pattern (dpeaa)DE-He213 Western Pacific pattern (dpeaa)DE-He213 Westerly jet stream (dpeaa)DE-He213 ENSO teleconnection (dpeaa)DE-He213 Zhu, Zhiwei verfasserin (orcid)0000-0002-4885-1299 aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 62(2024), 7 vom: 06. Mai, Seite 6985-7000 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:62 year:2024 number:7 day:06 month:05 pages:6985-7000 https://dx.doi.org/10.1007/s00382-024-07261-8 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 7 06 05 6985-7000
allfields_unstemmed	10.1007/s00382-024-07261-8 doi (DE-627)SPR057423202 (SPR)s00382-024-07261-8-e DE-627 ger DE-627 rakwb eng 550 VZ 38.80 bkl Mao, Jingdan verfasserin aut Change of boreal winter dominant ENSO teleconnection modulated by the East Asian westerly jet strength 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 This study reveals an interdecadal change in boreal winter dominant ENSO atmospheric teleconnection and demonstrates its underlying physical mechanism. During the period 1960–2020, the ENSO teleconnection was characterized by the Western Pacific (WP) pattern and the Pacific–North American (PNA) pattern, but the dominant pattern of ENSO teleconnection witnessed an alternation at around early 1980s. In the first epoch of 1960–1979 (E1), the ENSO teleconnection was mainly dominated by the WP pattern with an inhibited PNA pattern, whereas in the second epoch of 1987–2020 (E2), the ENSO teleconnection was dominated by the PNA pattern without a prominent WP pattern. It is further suggested that the changing strength of the westerly jet, rather than the pattern of the ENSO-related tropical convection, played the critical role in the alternation of the winter dominant ENSO teleconnection. During E1, because the westerly jet stream in the East Asia–North Pacific sector was relatively weak, poleward propagation of the Rossby wave train from the western Pacific was evident, forming the dominant WP pattern related to ENSO. In E2, because the westerly jet in the region largely strengthened, the PNA pattern was dominant owing to the enhanced zonal waveguide of the westerly jet. Evidence from a set of numerical experiments and the simulations of CMIP6 models supports the important role of the westerly jet strength in shaping the ENSO teleconnection. Pacific–North American pattern (dpeaa)DE-He213 Western Pacific pattern (dpeaa)DE-He213 Westerly jet stream (dpeaa)DE-He213 ENSO teleconnection (dpeaa)DE-He213 Zhu, Zhiwei verfasserin (orcid)0000-0002-4885-1299 aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 62(2024), 7 vom: 06. Mai, Seite 6985-7000 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:62 year:2024 number:7 day:06 month:05 pages:6985-7000 https://dx.doi.org/10.1007/s00382-024-07261-8 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 7 06 05 6985-7000
allfieldsGer	10.1007/s00382-024-07261-8 doi (DE-627)SPR057423202 (SPR)s00382-024-07261-8-e DE-627 ger DE-627 rakwb eng 550 VZ 38.80 bkl Mao, Jingdan verfasserin aut Change of boreal winter dominant ENSO teleconnection modulated by the East Asian westerly jet strength 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 This study reveals an interdecadal change in boreal winter dominant ENSO atmospheric teleconnection and demonstrates its underlying physical mechanism. During the period 1960–2020, the ENSO teleconnection was characterized by the Western Pacific (WP) pattern and the Pacific–North American (PNA) pattern, but the dominant pattern of ENSO teleconnection witnessed an alternation at around early 1980s. In the first epoch of 1960–1979 (E1), the ENSO teleconnection was mainly dominated by the WP pattern with an inhibited PNA pattern, whereas in the second epoch of 1987–2020 (E2), the ENSO teleconnection was dominated by the PNA pattern without a prominent WP pattern. It is further suggested that the changing strength of the westerly jet, rather than the pattern of the ENSO-related tropical convection, played the critical role in the alternation of the winter dominant ENSO teleconnection. During E1, because the westerly jet stream in the East Asia–North Pacific sector was relatively weak, poleward propagation of the Rossby wave train from the western Pacific was evident, forming the dominant WP pattern related to ENSO. In E2, because the westerly jet in the region largely strengthened, the PNA pattern was dominant owing to the enhanced zonal waveguide of the westerly jet. Evidence from a set of numerical experiments and the simulations of CMIP6 models supports the important role of the westerly jet strength in shaping the ENSO teleconnection. Pacific–North American pattern (dpeaa)DE-He213 Western Pacific pattern (dpeaa)DE-He213 Westerly jet stream (dpeaa)DE-He213 ENSO teleconnection (dpeaa)DE-He213 Zhu, Zhiwei verfasserin (orcid)0000-0002-4885-1299 aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 62(2024), 7 vom: 06. Mai, Seite 6985-7000 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:62 year:2024 number:7 day:06 month:05 pages:6985-7000 https://dx.doi.org/10.1007/s00382-024-07261-8 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 7 06 05 6985-7000
allfieldsSound	10.1007/s00382-024-07261-8 doi (DE-627)SPR057423202 (SPR)s00382-024-07261-8-e DE-627 ger DE-627 rakwb eng 550 VZ 38.80 bkl Mao, Jingdan verfasserin aut Change of boreal winter dominant ENSO teleconnection modulated by the East Asian westerly jet strength 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 This study reveals an interdecadal change in boreal winter dominant ENSO atmospheric teleconnection and demonstrates its underlying physical mechanism. During the period 1960–2020, the ENSO teleconnection was characterized by the Western Pacific (WP) pattern and the Pacific–North American (PNA) pattern, but the dominant pattern of ENSO teleconnection witnessed an alternation at around early 1980s. In the first epoch of 1960–1979 (E1), the ENSO teleconnection was mainly dominated by the WP pattern with an inhibited PNA pattern, whereas in the second epoch of 1987–2020 (E2), the ENSO teleconnection was dominated by the PNA pattern without a prominent WP pattern. It is further suggested that the changing strength of the westerly jet, rather than the pattern of the ENSO-related tropical convection, played the critical role in the alternation of the winter dominant ENSO teleconnection. During E1, because the westerly jet stream in the East Asia–North Pacific sector was relatively weak, poleward propagation of the Rossby wave train from the western Pacific was evident, forming the dominant WP pattern related to ENSO. In E2, because the westerly jet in the region largely strengthened, the PNA pattern was dominant owing to the enhanced zonal waveguide of the westerly jet. Evidence from a set of numerical experiments and the simulations of CMIP6 models supports the important role of the westerly jet strength in shaping the ENSO teleconnection. Pacific–North American pattern (dpeaa)DE-He213 Western Pacific pattern (dpeaa)DE-He213 Westerly jet stream (dpeaa)DE-He213 ENSO teleconnection (dpeaa)DE-He213 Zhu, Zhiwei verfasserin (orcid)0000-0002-4885-1299 aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 62(2024), 7 vom: 06. Mai, Seite 6985-7000 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:62 year:2024 number:7 day:06 month:05 pages:6985-7000 https://dx.doi.org/10.1007/s00382-024-07261-8 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 7 06 05 6985-7000
language	English
source	Enthalten in Climate dynamics 62(2024), 7 vom: 06. Mai, Seite 6985-7000 volume:62 year:2024 number:7 day:06 month:05 pages:6985-7000
sourceStr	Enthalten in Climate dynamics 62(2024), 7 vom: 06. Mai, Seite 6985-7000 volume:62 year:2024 number:7 day:06 month:05 pages:6985-7000
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Pacific–North American pattern Western Pacific pattern Westerly jet stream ENSO teleconnection
dewey-raw	550
isfreeaccess_bool	false
container_title	Climate dynamics
authorswithroles_txt_mv	Mao, Jingdan @@aut@@ Zhu, Zhiwei @@aut@@
publishDateDaySort_date	2024-05-06T00:00:00Z
hierarchy_top_id	268128561
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author	Mao, Jingdan
spellingShingle	Mao, Jingdan ddc 550 bkl 38.80 misc Pacific–North American pattern misc Western Pacific pattern misc Westerly jet stream misc ENSO teleconnection Change of boreal winter dominant ENSO teleconnection modulated by the East Asian westerly jet strength
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topic_title	550 VZ 38.80 bkl Change of boreal winter dominant ENSO teleconnection modulated by the East Asian westerly jet strength Pacific–North American pattern (dpeaa)DE-He213 Western Pacific pattern (dpeaa)DE-He213 Westerly jet stream (dpeaa)DE-He213 ENSO teleconnection (dpeaa)DE-He213
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title	Change of boreal winter dominant ENSO teleconnection modulated by the East Asian westerly jet strength
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title_full	Change of boreal winter dominant ENSO teleconnection modulated by the East Asian westerly jet strength
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title_sort	change of boreal winter dominant enso teleconnection modulated by the east asian westerly jet strength
title_auth	Change of boreal winter dominant ENSO teleconnection modulated by the East Asian westerly jet strength
abstract	Abstract This study reveals an interdecadal change in boreal winter dominant ENSO atmospheric teleconnection and demonstrates its underlying physical mechanism. During the period 1960–2020, the ENSO teleconnection was characterized by the Western Pacific (WP) pattern and the Pacific–North American (PNA) pattern, but the dominant pattern of ENSO teleconnection witnessed an alternation at around early 1980s. In the first epoch of 1960–1979 (E1), the ENSO teleconnection was mainly dominated by the WP pattern with an inhibited PNA pattern, whereas in the second epoch of 1987–2020 (E2), the ENSO teleconnection was dominated by the PNA pattern without a prominent WP pattern. It is further suggested that the changing strength of the westerly jet, rather than the pattern of the ENSO-related tropical convection, played the critical role in the alternation of the winter dominant ENSO teleconnection. During E1, because the westerly jet stream in the East Asia–North Pacific sector was relatively weak, poleward propagation of the Rossby wave train from the western Pacific was evident, forming the dominant WP pattern related to ENSO. In E2, because the westerly jet in the region largely strengthened, the PNA pattern was dominant owing to the enhanced zonal waveguide of the westerly jet. Evidence from a set of numerical experiments and the simulations of CMIP6 models supports the important role of the westerly jet strength in shaping the ENSO teleconnection. © 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 This study reveals an interdecadal change in boreal winter dominant ENSO atmospheric teleconnection and demonstrates its underlying physical mechanism. During the period 1960–2020, the ENSO teleconnection was characterized by the Western Pacific (WP) pattern and the Pacific–North American (PNA) pattern, but the dominant pattern of ENSO teleconnection witnessed an alternation at around early 1980s. In the first epoch of 1960–1979 (E1), the ENSO teleconnection was mainly dominated by the WP pattern with an inhibited PNA pattern, whereas in the second epoch of 1987–2020 (E2), the ENSO teleconnection was dominated by the PNA pattern without a prominent WP pattern. It is further suggested that the changing strength of the westerly jet, rather than the pattern of the ENSO-related tropical convection, played the critical role in the alternation of the winter dominant ENSO teleconnection. During E1, because the westerly jet stream in the East Asia–North Pacific sector was relatively weak, poleward propagation of the Rossby wave train from the western Pacific was evident, forming the dominant WP pattern related to ENSO. In E2, because the westerly jet in the region largely strengthened, the PNA pattern was dominant owing to the enhanced zonal waveguide of the westerly jet. Evidence from a set of numerical experiments and the simulations of CMIP6 models supports the important role of the westerly jet strength in shaping the ENSO teleconnection. © 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 This study reveals an interdecadal change in boreal winter dominant ENSO atmospheric teleconnection and demonstrates its underlying physical mechanism. During the period 1960–2020, the ENSO teleconnection was characterized by the Western Pacific (WP) pattern and the Pacific–North American (PNA) pattern, but the dominant pattern of ENSO teleconnection witnessed an alternation at around early 1980s. In the first epoch of 1960–1979 (E1), the ENSO teleconnection was mainly dominated by the WP pattern with an inhibited PNA pattern, whereas in the second epoch of 1987–2020 (E2), the ENSO teleconnection was dominated by the PNA pattern without a prominent WP pattern. It is further suggested that the changing strength of the westerly jet, rather than the pattern of the ENSO-related tropical convection, played the critical role in the alternation of the winter dominant ENSO teleconnection. During E1, because the westerly jet stream in the East Asia–North Pacific sector was relatively weak, poleward propagation of the Rossby wave train from the western Pacific was evident, forming the dominant WP pattern related to ENSO. In E2, because the westerly jet in the region largely strengthened, the PNA pattern was dominant owing to the enhanced zonal waveguide of the westerly jet. Evidence from a set of numerical experiments and the simulations of CMIP6 models supports the important role of the westerly jet strength in shaping the ENSO teleconnection. © 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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container_issue	7
title_short	Change of boreal winter dominant ENSO teleconnection modulated by the East Asian westerly jet strength
url	https://dx.doi.org/10.1007/s00382-024-07261-8
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author2	Zhu, Zhiwei
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doi_str	10.1007/s00382-024-07261-8
up_date	2024-09-25T04:53:38.108Z
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Change of boreal winter dominant ENSO teleconnection modulated by the East Asian westerly jet strength

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