Summer climate variability over Korea in association with diverse features of ENSO evolution
Abstract This study investigates the summer climate variability over Korea that is associated with diverse features of El Niño-Southern Oscillation (ENSO) evolution. Four different ENSO evolution features were analyzed, and the related Korean climate variability during July and August are investigat...
Ausführliche Beschreibung
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| Autor*in: |
Yeo, Sae-Rim [verfasserIn] Kim, Seon Tae [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2021 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Climate dynamics - Berlin : Springer, 1986, 56(2021), 9-10 vom: 16. Jan., Seite 2823-2838 |
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| Übergeordnetes Werk: |
volume:56 ; year:2021 ; number:9-10 ; day:16 ; month:01 ; pages:2823-2838 |
| Links: |
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| DOI / URN: |
10.1007/s00382-020-05612-9 |
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SPR043902332 |
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| 245 | 1 | 0 | |a Summer climate variability over Korea in association with diverse features of ENSO evolution |
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| 520 | |a Abstract This study investigates the summer climate variability over Korea that is associated with diverse features of El Niño-Southern Oscillation (ENSO) evolution. Four different ENSO evolution features were analyzed, and the related Korean climate variability during July and August are investigated. The two evolution phases in which El Niño transitions into La Niña and El Niño develops from a neutral state show roughly similar circulation features in affecting the Korean summer climate, but with opposite signs. During the transition of El Niño into La Niña (after El Niño develops from a neutral state), the positive (negative) western North Pacific anticyclonic circulation anomaly directly affects Korea in August, producing a significant warm (cold) surface air temperature (SAT) anomaly in Korea. Notably, the SAT that occurs in July generally exhibits an opposite tendency to that of August in Korea, displaying subseasonal variations. However, the persistent phases of La Niña and El Niño exhibit distinctive features from the two transition phases mentioned. During the persistent La Niña phase, the Pacific-Japan like atmospheric circulation pattern affects Korea, showing a significant warm SAT anomaly over Korea in July, and a roughly similar situation with opposite signs is observed in the persistent El Niño phase. In these cases, the Korean SAT in August exhibits similar anomalies to July. The distinctive variability in the summer climate of Korea during the diverse ENSO evolution phases presented in this study provides a statistical basis for understanding the Korean summer climate in relation to ENSO. | ||
| 650 | 4 | |a ENSO evolution |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Summer climate over Korea |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Western North Pacific anticyclonic circulation |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Pacific-Japan pattern |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Kim, Seon Tae |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Climate dynamics |d Berlin : Springer, 1986 |g 56(2021), 9-10 vom: 16. Jan., Seite 2823-2838 |w (DE-627)268128561 |w (DE-600)1471747-5 |x 1432-0894 |7 nnns |
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| 856 | 4 | 0 | |u https://dx.doi.org/10.1007/s00382-020-05612-9 |z lizenzpflichtig |3 Volltext |
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10.1007/s00382-020-05612-9 doi (DE-627)SPR043902332 (DE-599)SPRs00382-020-05612-9-e (SPR)s00382-020-05612-9-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl Yeo, Sae-Rim verfasserin aut Summer climate variability over Korea in association with diverse features of ENSO evolution 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract This study investigates the summer climate variability over Korea that is associated with diverse features of El Niño-Southern Oscillation (ENSO) evolution. Four different ENSO evolution features were analyzed, and the related Korean climate variability during July and August are investigated. The two evolution phases in which El Niño transitions into La Niña and El Niño develops from a neutral state show roughly similar circulation features in affecting the Korean summer climate, but with opposite signs. During the transition of El Niño into La Niña (after El Niño develops from a neutral state), the positive (negative) western North Pacific anticyclonic circulation anomaly directly affects Korea in August, producing a significant warm (cold) surface air temperature (SAT) anomaly in Korea. Notably, the SAT that occurs in July generally exhibits an opposite tendency to that of August in Korea, displaying subseasonal variations. However, the persistent phases of La Niña and El Niño exhibit distinctive features from the two transition phases mentioned. During the persistent La Niña phase, the Pacific-Japan like atmospheric circulation pattern affects Korea, showing a significant warm SAT anomaly over Korea in July, and a roughly similar situation with opposite signs is observed in the persistent El Niño phase. In these cases, the Korean SAT in August exhibits similar anomalies to July. The distinctive variability in the summer climate of Korea during the diverse ENSO evolution phases presented in this study provides a statistical basis for understanding the Korean summer climate in relation to ENSO. ENSO evolution (dpeaa)DE-He213 Summer climate over Korea (dpeaa)DE-He213 Western North Pacific anticyclonic circulation (dpeaa)DE-He213 Pacific-Japan pattern (dpeaa)DE-He213 Kim, Seon Tae verfasserin aut Enthalten in Climate dynamics Berlin : Springer, 1986 56(2021), 9-10 vom: 16. Jan., Seite 2823-2838 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:56 year:2021 number:9-10 day:16 month:01 pages:2823-2838 https://dx.doi.org/10.1007/s00382-020-05612-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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 38.80 ASE AR 56 2021 9-10 16 01 2823-2838 |
| spelling |
10.1007/s00382-020-05612-9 doi (DE-627)SPR043902332 (DE-599)SPRs00382-020-05612-9-e (SPR)s00382-020-05612-9-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl Yeo, Sae-Rim verfasserin aut Summer climate variability over Korea in association with diverse features of ENSO evolution 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract This study investigates the summer climate variability over Korea that is associated with diverse features of El Niño-Southern Oscillation (ENSO) evolution. Four different ENSO evolution features were analyzed, and the related Korean climate variability during July and August are investigated. The two evolution phases in which El Niño transitions into La Niña and El Niño develops from a neutral state show roughly similar circulation features in affecting the Korean summer climate, but with opposite signs. During the transition of El Niño into La Niña (after El Niño develops from a neutral state), the positive (negative) western North Pacific anticyclonic circulation anomaly directly affects Korea in August, producing a significant warm (cold) surface air temperature (SAT) anomaly in Korea. Notably, the SAT that occurs in July generally exhibits an opposite tendency to that of August in Korea, displaying subseasonal variations. However, the persistent phases of La Niña and El Niño exhibit distinctive features from the two transition phases mentioned. During the persistent La Niña phase, the Pacific-Japan like atmospheric circulation pattern affects Korea, showing a significant warm SAT anomaly over Korea in July, and a roughly similar situation with opposite signs is observed in the persistent El Niño phase. In these cases, the Korean SAT in August exhibits similar anomalies to July. The distinctive variability in the summer climate of Korea during the diverse ENSO evolution phases presented in this study provides a statistical basis for understanding the Korean summer climate in relation to ENSO. ENSO evolution (dpeaa)DE-He213 Summer climate over Korea (dpeaa)DE-He213 Western North Pacific anticyclonic circulation (dpeaa)DE-He213 Pacific-Japan pattern (dpeaa)DE-He213 Kim, Seon Tae verfasserin aut Enthalten in Climate dynamics Berlin : Springer, 1986 56(2021), 9-10 vom: 16. Jan., Seite 2823-2838 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:56 year:2021 number:9-10 day:16 month:01 pages:2823-2838 https://dx.doi.org/10.1007/s00382-020-05612-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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 38.80 ASE AR 56 2021 9-10 16 01 2823-2838 |
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10.1007/s00382-020-05612-9 doi (DE-627)SPR043902332 (DE-599)SPRs00382-020-05612-9-e (SPR)s00382-020-05612-9-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl Yeo, Sae-Rim verfasserin aut Summer climate variability over Korea in association with diverse features of ENSO evolution 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract This study investigates the summer climate variability over Korea that is associated with diverse features of El Niño-Southern Oscillation (ENSO) evolution. Four different ENSO evolution features were analyzed, and the related Korean climate variability during July and August are investigated. The two evolution phases in which El Niño transitions into La Niña and El Niño develops from a neutral state show roughly similar circulation features in affecting the Korean summer climate, but with opposite signs. During the transition of El Niño into La Niña (after El Niño develops from a neutral state), the positive (negative) western North Pacific anticyclonic circulation anomaly directly affects Korea in August, producing a significant warm (cold) surface air temperature (SAT) anomaly in Korea. Notably, the SAT that occurs in July generally exhibits an opposite tendency to that of August in Korea, displaying subseasonal variations. However, the persistent phases of La Niña and El Niño exhibit distinctive features from the two transition phases mentioned. During the persistent La Niña phase, the Pacific-Japan like atmospheric circulation pattern affects Korea, showing a significant warm SAT anomaly over Korea in July, and a roughly similar situation with opposite signs is observed in the persistent El Niño phase. In these cases, the Korean SAT in August exhibits similar anomalies to July. The distinctive variability in the summer climate of Korea during the diverse ENSO evolution phases presented in this study provides a statistical basis for understanding the Korean summer climate in relation to ENSO. ENSO evolution (dpeaa)DE-He213 Summer climate over Korea (dpeaa)DE-He213 Western North Pacific anticyclonic circulation (dpeaa)DE-He213 Pacific-Japan pattern (dpeaa)DE-He213 Kim, Seon Tae verfasserin aut Enthalten in Climate dynamics Berlin : Springer, 1986 56(2021), 9-10 vom: 16. Jan., Seite 2823-2838 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:56 year:2021 number:9-10 day:16 month:01 pages:2823-2838 https://dx.doi.org/10.1007/s00382-020-05612-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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 38.80 ASE AR 56 2021 9-10 16 01 2823-2838 |
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10.1007/s00382-020-05612-9 doi (DE-627)SPR043902332 (DE-599)SPRs00382-020-05612-9-e (SPR)s00382-020-05612-9-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl Yeo, Sae-Rim verfasserin aut Summer climate variability over Korea in association with diverse features of ENSO evolution 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract This study investigates the summer climate variability over Korea that is associated with diverse features of El Niño-Southern Oscillation (ENSO) evolution. Four different ENSO evolution features were analyzed, and the related Korean climate variability during July and August are investigated. The two evolution phases in which El Niño transitions into La Niña and El Niño develops from a neutral state show roughly similar circulation features in affecting the Korean summer climate, but with opposite signs. During the transition of El Niño into La Niña (after El Niño develops from a neutral state), the positive (negative) western North Pacific anticyclonic circulation anomaly directly affects Korea in August, producing a significant warm (cold) surface air temperature (SAT) anomaly in Korea. Notably, the SAT that occurs in July generally exhibits an opposite tendency to that of August in Korea, displaying subseasonal variations. However, the persistent phases of La Niña and El Niño exhibit distinctive features from the two transition phases mentioned. During the persistent La Niña phase, the Pacific-Japan like atmospheric circulation pattern affects Korea, showing a significant warm SAT anomaly over Korea in July, and a roughly similar situation with opposite signs is observed in the persistent El Niño phase. In these cases, the Korean SAT in August exhibits similar anomalies to July. The distinctive variability in the summer climate of Korea during the diverse ENSO evolution phases presented in this study provides a statistical basis for understanding the Korean summer climate in relation to ENSO. ENSO evolution (dpeaa)DE-He213 Summer climate over Korea (dpeaa)DE-He213 Western North Pacific anticyclonic circulation (dpeaa)DE-He213 Pacific-Japan pattern (dpeaa)DE-He213 Kim, Seon Tae verfasserin aut Enthalten in Climate dynamics Berlin : Springer, 1986 56(2021), 9-10 vom: 16. Jan., Seite 2823-2838 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:56 year:2021 number:9-10 day:16 month:01 pages:2823-2838 https://dx.doi.org/10.1007/s00382-020-05612-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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 38.80 ASE AR 56 2021 9-10 16 01 2823-2838 |
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10.1007/s00382-020-05612-9 doi (DE-627)SPR043902332 (DE-599)SPRs00382-020-05612-9-e (SPR)s00382-020-05612-9-e DE-627 ger DE-627 rakwb eng 550 ASE 38.80 bkl Yeo, Sae-Rim verfasserin aut Summer climate variability over Korea in association with diverse features of ENSO evolution 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract This study investigates the summer climate variability over Korea that is associated with diverse features of El Niño-Southern Oscillation (ENSO) evolution. Four different ENSO evolution features were analyzed, and the related Korean climate variability during July and August are investigated. The two evolution phases in which El Niño transitions into La Niña and El Niño develops from a neutral state show roughly similar circulation features in affecting the Korean summer climate, but with opposite signs. During the transition of El Niño into La Niña (after El Niño develops from a neutral state), the positive (negative) western North Pacific anticyclonic circulation anomaly directly affects Korea in August, producing a significant warm (cold) surface air temperature (SAT) anomaly in Korea. Notably, the SAT that occurs in July generally exhibits an opposite tendency to that of August in Korea, displaying subseasonal variations. However, the persistent phases of La Niña and El Niño exhibit distinctive features from the two transition phases mentioned. During the persistent La Niña phase, the Pacific-Japan like atmospheric circulation pattern affects Korea, showing a significant warm SAT anomaly over Korea in July, and a roughly similar situation with opposite signs is observed in the persistent El Niño phase. In these cases, the Korean SAT in August exhibits similar anomalies to July. The distinctive variability in the summer climate of Korea during the diverse ENSO evolution phases presented in this study provides a statistical basis for understanding the Korean summer climate in relation to ENSO. ENSO evolution (dpeaa)DE-He213 Summer climate over Korea (dpeaa)DE-He213 Western North Pacific anticyclonic circulation (dpeaa)DE-He213 Pacific-Japan pattern (dpeaa)DE-He213 Kim, Seon Tae verfasserin aut Enthalten in Climate dynamics Berlin : Springer, 1986 56(2021), 9-10 vom: 16. Jan., Seite 2823-2838 (DE-627)268128561 (DE-600)1471747-5 1432-0894 nnns volume:56 year:2021 number:9-10 day:16 month:01 pages:2823-2838 https://dx.doi.org/10.1007/s00382-020-05612-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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 38.80 ASE AR 56 2021 9-10 16 01 2823-2838 |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR043902332</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220110175125.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">210430s2021 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00382-020-05612-9</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR043902332</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)SPRs00382-020-05612-9-e</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s00382-020-05612-9-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.80</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Yeo, Sae-Rim</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Summer climate variability over Korea in association with diverse features of ENSO evolution</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2021</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract This study investigates the summer climate variability over Korea that is associated with diverse features of El Niño-Southern Oscillation (ENSO) evolution. Four different ENSO evolution features were analyzed, and the related Korean climate variability during July and August are investigated. The two evolution phases in which El Niño transitions into La Niña and El Niño develops from a neutral state show roughly similar circulation features in affecting the Korean summer climate, but with opposite signs. During the transition of El Niño into La Niña (after El Niño develops from a neutral state), the positive (negative) western North Pacific anticyclonic circulation anomaly directly affects Korea in August, producing a significant warm (cold) surface air temperature (SAT) anomaly in Korea. Notably, the SAT that occurs in July generally exhibits an opposite tendency to that of August in Korea, displaying subseasonal variations. However, the persistent phases of La Niña and El Niño exhibit distinctive features from the two transition phases mentioned. During the persistent La Niña phase, the Pacific-Japan like atmospheric circulation pattern affects Korea, showing a significant warm SAT anomaly over Korea in July, and a roughly similar situation with opposite signs is observed in the persistent El Niño phase. In these cases, the Korean SAT in August exhibits similar anomalies to July. 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Jan., Seite 2823-2838</subfield><subfield code="w">(DE-627)268128561</subfield><subfield code="w">(DE-600)1471747-5</subfield><subfield code="x">1432-0894</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:56</subfield><subfield code="g">year:2021</subfield><subfield code="g">number:9-10</subfield><subfield code="g">day:16</subfield><subfield code="g">month:01</subfield><subfield code="g">pages:2823-2838</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/s00382-020-05612-9</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_SPRINGER</subfield></datafield><datafield 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Yeo, Sae-Rim |
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Yeo, Sae-Rim ddc 550 bkl 38.80 misc ENSO evolution misc Summer climate over Korea misc Western North Pacific anticyclonic circulation misc Pacific-Japan pattern Summer climate variability over Korea in association with diverse features of ENSO evolution |
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550 ASE 38.80 bkl Summer climate variability over Korea in association with diverse features of ENSO evolution ENSO evolution (dpeaa)DE-He213 Summer climate over Korea (dpeaa)DE-He213 Western North Pacific anticyclonic circulation (dpeaa)DE-He213 Pacific-Japan pattern (dpeaa)DE-He213 |
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ddc 550 bkl 38.80 misc ENSO evolution misc Summer climate over Korea misc Western North Pacific anticyclonic circulation misc Pacific-Japan pattern |
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Summer climate variability over Korea in association with diverse features of ENSO evolution |
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Summer climate variability over Korea in association with diverse features of ENSO evolution |
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summer climate variability over korea in association with diverse features of enso evolution |
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Summer climate variability over Korea in association with diverse features of ENSO evolution |
| abstract |
Abstract This study investigates the summer climate variability over Korea that is associated with diverse features of El Niño-Southern Oscillation (ENSO) evolution. Four different ENSO evolution features were analyzed, and the related Korean climate variability during July and August are investigated. The two evolution phases in which El Niño transitions into La Niña and El Niño develops from a neutral state show roughly similar circulation features in affecting the Korean summer climate, but with opposite signs. During the transition of El Niño into La Niña (after El Niño develops from a neutral state), the positive (negative) western North Pacific anticyclonic circulation anomaly directly affects Korea in August, producing a significant warm (cold) surface air temperature (SAT) anomaly in Korea. Notably, the SAT that occurs in July generally exhibits an opposite tendency to that of August in Korea, displaying subseasonal variations. However, the persistent phases of La Niña and El Niño exhibit distinctive features from the two transition phases mentioned. During the persistent La Niña phase, the Pacific-Japan like atmospheric circulation pattern affects Korea, showing a significant warm SAT anomaly over Korea in July, and a roughly similar situation with opposite signs is observed in the persistent El Niño phase. In these cases, the Korean SAT in August exhibits similar anomalies to July. The distinctive variability in the summer climate of Korea during the diverse ENSO evolution phases presented in this study provides a statistical basis for understanding the Korean summer climate in relation to ENSO. |
| abstractGer |
Abstract This study investigates the summer climate variability over Korea that is associated with diverse features of El Niño-Southern Oscillation (ENSO) evolution. Four different ENSO evolution features were analyzed, and the related Korean climate variability during July and August are investigated. The two evolution phases in which El Niño transitions into La Niña and El Niño develops from a neutral state show roughly similar circulation features in affecting the Korean summer climate, but with opposite signs. During the transition of El Niño into La Niña (after El Niño develops from a neutral state), the positive (negative) western North Pacific anticyclonic circulation anomaly directly affects Korea in August, producing a significant warm (cold) surface air temperature (SAT) anomaly in Korea. Notably, the SAT that occurs in July generally exhibits an opposite tendency to that of August in Korea, displaying subseasonal variations. However, the persistent phases of La Niña and El Niño exhibit distinctive features from the two transition phases mentioned. During the persistent La Niña phase, the Pacific-Japan like atmospheric circulation pattern affects Korea, showing a significant warm SAT anomaly over Korea in July, and a roughly similar situation with opposite signs is observed in the persistent El Niño phase. In these cases, the Korean SAT in August exhibits similar anomalies to July. The distinctive variability in the summer climate of Korea during the diverse ENSO evolution phases presented in this study provides a statistical basis for understanding the Korean summer climate in relation to ENSO. |
| abstract_unstemmed |
Abstract This study investigates the summer climate variability over Korea that is associated with diverse features of El Niño-Southern Oscillation (ENSO) evolution. Four different ENSO evolution features were analyzed, and the related Korean climate variability during July and August are investigated. The two evolution phases in which El Niño transitions into La Niña and El Niño develops from a neutral state show roughly similar circulation features in affecting the Korean summer climate, but with opposite signs. During the transition of El Niño into La Niña (after El Niño develops from a neutral state), the positive (negative) western North Pacific anticyclonic circulation anomaly directly affects Korea in August, producing a significant warm (cold) surface air temperature (SAT) anomaly in Korea. Notably, the SAT that occurs in July generally exhibits an opposite tendency to that of August in Korea, displaying subseasonal variations. However, the persistent phases of La Niña and El Niño exhibit distinctive features from the two transition phases mentioned. During the persistent La Niña phase, the Pacific-Japan like atmospheric circulation pattern affects Korea, showing a significant warm SAT anomaly over Korea in July, and a roughly similar situation with opposite signs is observed in the persistent El Niño phase. In these cases, the Korean SAT in August exhibits similar anomalies to July. The distinctive variability in the summer climate of Korea during the diverse ENSO evolution phases presented in this study provides a statistical basis for understanding the Korean summer climate in relation to ENSO. |
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| container_issue |
9-10 |
| title_short |
Summer climate variability over Korea in association with diverse features of ENSO evolution |
| url |
https://dx.doi.org/10.1007/s00382-020-05612-9 |
| remote_bool |
true |
| author2 |
Kim, Seon Tae |
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Kim, Seon Tae |
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| doi_str |
10.1007/s00382-020-05612-9 |
| up_date |
2024-07-03T21:39:49.859Z |
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| score |
7.401026 |