Intra-seasonal variation of the wintertime Polar/Eurasia pattern

Abstract WE investigated the intra-seasonal variation of the winter Polar/Eurasia (PEU) pattern, the dominant circulation pattern over the Eurasian continent, during the period 1979/80–2021/22. The PEU events have centers of action over western Europe, the Urals and the Siberian–Mongolian region. Th...
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Autor*in:	Jiang, Yongru [verfasserIn] Cheung, Ho-Nam Li, Yana Yang, Song

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2022

Schlagwörter:	Polar/Eurasia pattern Teleconnection Intra-seasonal variation Diagnostic analysis

Anmerkung:	© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 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.

Übergeordnetes Werk:	Enthalten in: Climate dynamics - Berlin : Springer, 1986, 61(2022), 1-2 vom: 07. Dez., Seite 813-830
Übergeordnetes Werk:	volume:61 ; year:2022 ; number:1-2 ; day:07 ; month:12 ; pages:813-830

Links:	Volltext

DOI / URN:	10.1007/s00382-022-06612-7

Katalog-ID:	SPR051958260

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520			\|a Abstract WE investigated the intra-seasonal variation of the winter Polar/Eurasia (PEU) pattern, the dominant circulation pattern over the Eurasian continent, during the period 1979/80–2021/22. The PEU events have centers of action over western Europe, the Urals and the Siberian–Mongolian region. The development of PEU events is associated with a Rossby wave train triggered by anomalous horizontal divergent winds over the North Atlantic and the European continent. Diagnostic analysis based on the quasi-geostrophic geopotential height tendency equation suggests that the cross-frequency dynamics play an important role in the formation and decay of the western Europe center, as well as the formation of the Siberian–Mongolian center. The sole effect of the low-frequency forcing primarily contributes to the life cycle of the Urals center and the decay of the Siberian–Mongolian center. The effect of the cross-frequency forcing and the low-frequency forcing on the PEU centers of action is predominantly due to their advection component. The cross-frequency forcing in Europe involves an interaction between the extratropical storm activity and the low-frequency flow, where the development and decay of PEU events are associated with contrasting storm track anomalies extending from the North Atlantic to the European continent. Overall, the evolution of the intra-seasonal PEU pattern is mainly due to the internal dynamic processes over the extratropics.
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700	1		\|a Yang, Song \|4 aut
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allfields	10.1007/s00382-022-06612-7 doi (DE-627)SPR051958260 (SPR)s00382-022-06612-7-e DE-627 ger DE-627 rakwb eng Jiang, Yongru verfasserin aut Intra-seasonal variation of the wintertime Polar/Eurasia pattern 2022 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 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 WE investigated the intra-seasonal variation of the winter Polar/Eurasia (PEU) pattern, the dominant circulation pattern over the Eurasian continent, during the period 1979/80–2021/22. The PEU events have centers of action over western Europe, the Urals and the Siberian–Mongolian region. The development of PEU events is associated with a Rossby wave train triggered by anomalous horizontal divergent winds over the North Atlantic and the European continent. Diagnostic analysis based on the quasi-geostrophic geopotential height tendency equation suggests that the cross-frequency dynamics play an important role in the formation and decay of the western Europe center, as well as the formation of the Siberian–Mongolian center. The sole effect of the low-frequency forcing primarily contributes to the life cycle of the Urals center and the decay of the Siberian–Mongolian center. The effect of the cross-frequency forcing and the low-frequency forcing on the PEU centers of action is predominantly due to their advection component. The cross-frequency forcing in Europe involves an interaction between the extratropical storm activity and the low-frequency flow, where the development and decay of PEU events are associated with contrasting storm track anomalies extending from the North Atlantic to the European continent. Overall, the evolution of the intra-seasonal PEU pattern is mainly due to the internal dynamic processes over the extratropics. Polar/Eurasia pattern (dpeaa)DE-He213 Teleconnection (dpeaa)DE-He213 Intra-seasonal variation (dpeaa)DE-He213 Diagnostic analysis (dpeaa)DE-He213 Cheung, Ho-Nam aut Li, Yana aut Yang, Song aut Enthalten in Climate dynamics Berlin : Springer, 1986 61(2022), 1-2 vom: 07. Dez., Seite 813-830 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:61 year:2022 number:1-2 day:07 month:12 pages:813-830 https://dx.doi.org/10.1007/s00382-022-06612-7 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_206 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_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 61 2022 1-2 07 12 813-830
spelling	10.1007/s00382-022-06612-7 doi (DE-627)SPR051958260 (SPR)s00382-022-06612-7-e DE-627 ger DE-627 rakwb eng Jiang, Yongru verfasserin aut Intra-seasonal variation of the wintertime Polar/Eurasia pattern 2022 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 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 WE investigated the intra-seasonal variation of the winter Polar/Eurasia (PEU) pattern, the dominant circulation pattern over the Eurasian continent, during the period 1979/80–2021/22. The PEU events have centers of action over western Europe, the Urals and the Siberian–Mongolian region. The development of PEU events is associated with a Rossby wave train triggered by anomalous horizontal divergent winds over the North Atlantic and the European continent. Diagnostic analysis based on the quasi-geostrophic geopotential height tendency equation suggests that the cross-frequency dynamics play an important role in the formation and decay of the western Europe center, as well as the formation of the Siberian–Mongolian center. The sole effect of the low-frequency forcing primarily contributes to the life cycle of the Urals center and the decay of the Siberian–Mongolian center. The effect of the cross-frequency forcing and the low-frequency forcing on the PEU centers of action is predominantly due to their advection component. The cross-frequency forcing in Europe involves an interaction between the extratropical storm activity and the low-frequency flow, where the development and decay of PEU events are associated with contrasting storm track anomalies extending from the North Atlantic to the European continent. Overall, the evolution of the intra-seasonal PEU pattern is mainly due to the internal dynamic processes over the extratropics. Polar/Eurasia pattern (dpeaa)DE-He213 Teleconnection (dpeaa)DE-He213 Intra-seasonal variation (dpeaa)DE-He213 Diagnostic analysis (dpeaa)DE-He213 Cheung, Ho-Nam aut Li, Yana aut Yang, Song aut Enthalten in Climate dynamics Berlin : Springer, 1986 61(2022), 1-2 vom: 07. Dez., Seite 813-830 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:61 year:2022 number:1-2 day:07 month:12 pages:813-830 https://dx.doi.org/10.1007/s00382-022-06612-7 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_206 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_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 61 2022 1-2 07 12 813-830
allfields_unstemmed	10.1007/s00382-022-06612-7 doi (DE-627)SPR051958260 (SPR)s00382-022-06612-7-e DE-627 ger DE-627 rakwb eng Jiang, Yongru verfasserin aut Intra-seasonal variation of the wintertime Polar/Eurasia pattern 2022 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 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 WE investigated the intra-seasonal variation of the winter Polar/Eurasia (PEU) pattern, the dominant circulation pattern over the Eurasian continent, during the period 1979/80–2021/22. The PEU events have centers of action over western Europe, the Urals and the Siberian–Mongolian region. The development of PEU events is associated with a Rossby wave train triggered by anomalous horizontal divergent winds over the North Atlantic and the European continent. Diagnostic analysis based on the quasi-geostrophic geopotential height tendency equation suggests that the cross-frequency dynamics play an important role in the formation and decay of the western Europe center, as well as the formation of the Siberian–Mongolian center. The sole effect of the low-frequency forcing primarily contributes to the life cycle of the Urals center and the decay of the Siberian–Mongolian center. The effect of the cross-frequency forcing and the low-frequency forcing on the PEU centers of action is predominantly due to their advection component. The cross-frequency forcing in Europe involves an interaction between the extratropical storm activity and the low-frequency flow, where the development and decay of PEU events are associated with contrasting storm track anomalies extending from the North Atlantic to the European continent. Overall, the evolution of the intra-seasonal PEU pattern is mainly due to the internal dynamic processes over the extratropics. Polar/Eurasia pattern (dpeaa)DE-He213 Teleconnection (dpeaa)DE-He213 Intra-seasonal variation (dpeaa)DE-He213 Diagnostic analysis (dpeaa)DE-He213 Cheung, Ho-Nam aut Li, Yana aut Yang, Song aut Enthalten in Climate dynamics Berlin : Springer, 1986 61(2022), 1-2 vom: 07. Dez., Seite 813-830 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:61 year:2022 number:1-2 day:07 month:12 pages:813-830 https://dx.doi.org/10.1007/s00382-022-06612-7 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_206 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_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 61 2022 1-2 07 12 813-830
allfieldsGer	10.1007/s00382-022-06612-7 doi (DE-627)SPR051958260 (SPR)s00382-022-06612-7-e DE-627 ger DE-627 rakwb eng Jiang, Yongru verfasserin aut Intra-seasonal variation of the wintertime Polar/Eurasia pattern 2022 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 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 WE investigated the intra-seasonal variation of the winter Polar/Eurasia (PEU) pattern, the dominant circulation pattern over the Eurasian continent, during the period 1979/80–2021/22. The PEU events have centers of action over western Europe, the Urals and the Siberian–Mongolian region. The development of PEU events is associated with a Rossby wave train triggered by anomalous horizontal divergent winds over the North Atlantic and the European continent. Diagnostic analysis based on the quasi-geostrophic geopotential height tendency equation suggests that the cross-frequency dynamics play an important role in the formation and decay of the western Europe center, as well as the formation of the Siberian–Mongolian center. The sole effect of the low-frequency forcing primarily contributes to the life cycle of the Urals center and the decay of the Siberian–Mongolian center. The effect of the cross-frequency forcing and the low-frequency forcing on the PEU centers of action is predominantly due to their advection component. The cross-frequency forcing in Europe involves an interaction between the extratropical storm activity and the low-frequency flow, where the development and decay of PEU events are associated with contrasting storm track anomalies extending from the North Atlantic to the European continent. Overall, the evolution of the intra-seasonal PEU pattern is mainly due to the internal dynamic processes over the extratropics. Polar/Eurasia pattern (dpeaa)DE-He213 Teleconnection (dpeaa)DE-He213 Intra-seasonal variation (dpeaa)DE-He213 Diagnostic analysis (dpeaa)DE-He213 Cheung, Ho-Nam aut Li, Yana aut Yang, Song aut Enthalten in Climate dynamics Berlin : Springer, 1986 61(2022), 1-2 vom: 07. Dez., Seite 813-830 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:61 year:2022 number:1-2 day:07 month:12 pages:813-830 https://dx.doi.org/10.1007/s00382-022-06612-7 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_206 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_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 61 2022 1-2 07 12 813-830
allfieldsSound	10.1007/s00382-022-06612-7 doi (DE-627)SPR051958260 (SPR)s00382-022-06612-7-e DE-627 ger DE-627 rakwb eng Jiang, Yongru verfasserin aut Intra-seasonal variation of the wintertime Polar/Eurasia pattern 2022 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 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 WE investigated the intra-seasonal variation of the winter Polar/Eurasia (PEU) pattern, the dominant circulation pattern over the Eurasian continent, during the period 1979/80–2021/22. The PEU events have centers of action over western Europe, the Urals and the Siberian–Mongolian region. The development of PEU events is associated with a Rossby wave train triggered by anomalous horizontal divergent winds over the North Atlantic and the European continent. Diagnostic analysis based on the quasi-geostrophic geopotential height tendency equation suggests that the cross-frequency dynamics play an important role in the formation and decay of the western Europe center, as well as the formation of the Siberian–Mongolian center. The sole effect of the low-frequency forcing primarily contributes to the life cycle of the Urals center and the decay of the Siberian–Mongolian center. The effect of the cross-frequency forcing and the low-frequency forcing on the PEU centers of action is predominantly due to their advection component. The cross-frequency forcing in Europe involves an interaction between the extratropical storm activity and the low-frequency flow, where the development and decay of PEU events are associated with contrasting storm track anomalies extending from the North Atlantic to the European continent. Overall, the evolution of the intra-seasonal PEU pattern is mainly due to the internal dynamic processes over the extratropics. Polar/Eurasia pattern (dpeaa)DE-He213 Teleconnection (dpeaa)DE-He213 Intra-seasonal variation (dpeaa)DE-He213 Diagnostic analysis (dpeaa)DE-He213 Cheung, Ho-Nam aut Li, Yana aut Yang, Song aut Enthalten in Climate dynamics Berlin : Springer, 1986 61(2022), 1-2 vom: 07. Dez., Seite 813-830 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:61 year:2022 number:1-2 day:07 month:12 pages:813-830 https://dx.doi.org/10.1007/s00382-022-06612-7 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_206 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_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 61 2022 1-2 07 12 813-830
language	English
source	Enthalten in Climate dynamics 61(2022), 1-2 vom: 07. Dez., Seite 813-830 volume:61 year:2022 number:1-2 day:07 month:12 pages:813-830
sourceStr	Enthalten in Climate dynamics 61(2022), 1-2 vom: 07. Dez., Seite 813-830 volume:61 year:2022 number:1-2 day:07 month:12 pages:813-830
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Polar/Eurasia pattern Teleconnection Intra-seasonal variation Diagnostic analysis
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container_title	Climate dynamics
authorswithroles_txt_mv	Jiang, Yongru @@aut@@ Cheung, Ho-Nam @@aut@@ Li, Yana @@aut@@ Yang, Song @@aut@@
publishDateDaySort_date	2022-12-07T00:00:00Z
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author	Jiang, Yongru
spellingShingle	Jiang, Yongru misc Polar/Eurasia pattern misc Teleconnection misc Intra-seasonal variation misc Diagnostic analysis Intra-seasonal variation of the wintertime Polar/Eurasia pattern
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topic_title	Intra-seasonal variation of the wintertime Polar/Eurasia pattern Polar/Eurasia pattern (dpeaa)DE-He213 Teleconnection (dpeaa)DE-He213 Intra-seasonal variation (dpeaa)DE-He213 Diagnostic analysis (dpeaa)DE-He213
topic	misc Polar/Eurasia pattern misc Teleconnection misc Intra-seasonal variation misc Diagnostic analysis
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title	Intra-seasonal variation of the wintertime Polar/Eurasia pattern
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title_full	Intra-seasonal variation of the wintertime Polar/Eurasia pattern
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author_browse	Jiang, Yongru Cheung, Ho-Nam Li, Yana Yang, Song
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doi_str_mv	10.1007/s00382-022-06612-7
title_sort	intra-seasonal variation of the wintertime polar/eurasia pattern
title_auth	Intra-seasonal variation of the wintertime Polar/Eurasia pattern
abstract	Abstract WE investigated the intra-seasonal variation of the winter Polar/Eurasia (PEU) pattern, the dominant circulation pattern over the Eurasian continent, during the period 1979/80–2021/22. The PEU events have centers of action over western Europe, the Urals and the Siberian–Mongolian region. The development of PEU events is associated with a Rossby wave train triggered by anomalous horizontal divergent winds over the North Atlantic and the European continent. Diagnostic analysis based on the quasi-geostrophic geopotential height tendency equation suggests that the cross-frequency dynamics play an important role in the formation and decay of the western Europe center, as well as the formation of the Siberian–Mongolian center. The sole effect of the low-frequency forcing primarily contributes to the life cycle of the Urals center and the decay of the Siberian–Mongolian center. The effect of the cross-frequency forcing and the low-frequency forcing on the PEU centers of action is predominantly due to their advection component. The cross-frequency forcing in Europe involves an interaction between the extratropical storm activity and the low-frequency flow, where the development and decay of PEU events are associated with contrasting storm track anomalies extending from the North Atlantic to the European continent. Overall, the evolution of the intra-seasonal PEU pattern is mainly due to the internal dynamic processes over the extratropics. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 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 WE investigated the intra-seasonal variation of the winter Polar/Eurasia (PEU) pattern, the dominant circulation pattern over the Eurasian continent, during the period 1979/80–2021/22. The PEU events have centers of action over western Europe, the Urals and the Siberian–Mongolian region. The development of PEU events is associated with a Rossby wave train triggered by anomalous horizontal divergent winds over the North Atlantic and the European continent. Diagnostic analysis based on the quasi-geostrophic geopotential height tendency equation suggests that the cross-frequency dynamics play an important role in the formation and decay of the western Europe center, as well as the formation of the Siberian–Mongolian center. The sole effect of the low-frequency forcing primarily contributes to the life cycle of the Urals center and the decay of the Siberian–Mongolian center. The effect of the cross-frequency forcing and the low-frequency forcing on the PEU centers of action is predominantly due to their advection component. The cross-frequency forcing in Europe involves an interaction between the extratropical storm activity and the low-frequency flow, where the development and decay of PEU events are associated with contrasting storm track anomalies extending from the North Atlantic to the European continent. Overall, the evolution of the intra-seasonal PEU pattern is mainly due to the internal dynamic processes over the extratropics. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 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 WE investigated the intra-seasonal variation of the winter Polar/Eurasia (PEU) pattern, the dominant circulation pattern over the Eurasian continent, during the period 1979/80–2021/22. The PEU events have centers of action over western Europe, the Urals and the Siberian–Mongolian region. The development of PEU events is associated with a Rossby wave train triggered by anomalous horizontal divergent winds over the North Atlantic and the European continent. Diagnostic analysis based on the quasi-geostrophic geopotential height tendency equation suggests that the cross-frequency dynamics play an important role in the formation and decay of the western Europe center, as well as the formation of the Siberian–Mongolian center. The sole effect of the low-frequency forcing primarily contributes to the life cycle of the Urals center and the decay of the Siberian–Mongolian center. The effect of the cross-frequency forcing and the low-frequency forcing on the PEU centers of action is predominantly due to their advection component. The cross-frequency forcing in Europe involves an interaction between the extratropical storm activity and the low-frequency flow, where the development and decay of PEU events are associated with contrasting storm track anomalies extending from the North Atlantic to the European continent. Overall, the evolution of the intra-seasonal PEU pattern is mainly due to the internal dynamic processes over the extratropics. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 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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title_short	Intra-seasonal variation of the wintertime Polar/Eurasia pattern
url	https://dx.doi.org/10.1007/s00382-022-06612-7
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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 WE investigated the intra-seasonal variation of the winter Polar/Eurasia (PEU) pattern, the dominant circulation pattern over the Eurasian continent, during the period 1979/80–2021/22. The PEU events have centers of action over western Europe, the Urals and the Siberian–Mongolian region. The development of PEU events is associated with a Rossby wave train triggered by anomalous horizontal divergent winds over the North Atlantic and the European continent. Diagnostic analysis based on the quasi-geostrophic geopotential height tendency equation suggests that the cross-frequency dynamics play an important role in the formation and decay of the western Europe center, as well as the formation of the Siberian–Mongolian center. The sole effect of the low-frequency forcing primarily contributes to the life cycle of the Urals center and the decay of the Siberian–Mongolian center. The effect of the cross-frequency forcing and the low-frequency forcing on the PEU centers of action is predominantly due to their advection component. The cross-frequency forcing in Europe involves an interaction between the extratropical storm activity and the low-frequency flow, where the development and decay of PEU events are associated with contrasting storm track anomalies extending from the North Atlantic to the European continent. 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Intra-seasonal variation of the wintertime Polar/Eurasia pattern

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