Different El Niño types and intense typhoons in the Western North Pacific
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| 008 | 210128e20150601xx s 000 0 eng | ||
| 024 | 7 | 0 | |a 10.1007/s00382-014-2446-4 |2 doi |
| 035 | |a (NATIONALLICENCE)springer-10.1007/s00382-014-2446-4 | ||
| 245 | 0 | 0 | |a Different El Niño types and intense typhoons in the Western North Pacific |h [Elektronische Daten] |c [Wei Zhang, Yee Leung, Klaus Fraedrich] |
| 520 | 3 | |a This study shows that the occurrence of intense typhoons in the western North Pacific is significantly higher in the autumns of the Central Pacific (CP), compared to Eastern Pacific El Niño years. Specifically, (1) The higher occurrence of intense typhoons in CP El Niño autumns is related to a longer typhoon lifespan, maximum potential intensity, ocean heat content, vertical shear of the zonal wind (850-200hPa), outgoing long-wave radiation, and moist static energy averaged over 1,000-500hPa. (2) A longer typhoon lifespan in CP El Niño autumns is caused by the westward shift of the subtropical high, which tends to steer typhoon to the west and northwest. | |
| 540 | |a Springer-Verlag Berlin Heidelberg, 2015 | ||
| 690 | 7 | |a CP El Niño |2 nationallicence | |
| 690 | 7 | |a EP El Niño |2 nationallicence | |
| 690 | 7 | |a Intense typhoon |2 nationallicence | |
| 690 | 7 | |a Western North Pacific |2 nationallicence | |
| 700 | 1 | |a Zhang |D Wei |u Earth System Modeling Center (ESMC) and Climate Dynamics Research Center, Nanjing International Academy of Meteorological Sciences (NIAMS), Key Laboratory of Meteorological Disaster, Ministry of Education and Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology, 210044, Nanjing, China |4 aut | |
| 700 | 1 | |a Leung |D Yee |u Department of Geography and Resource Management, The Chinese University of Hong Kong, Shatin, Hong Kong, China |4 aut | |
| 700 | 1 | |a Fraedrich |D Klaus |u Max Planck Institute for Meteorology, KlimaCampus, Hamburg, Germany |4 aut | |
| 773 | 0 | |t Climate Dynamics |d Springer Berlin Heidelberg |g 44/11-12(2015-06-01), 2965-2977 |x 0930-7575 |q 44:11-12<2965 |1 2015 |2 44 |o 382 | |
| 856 | 4 | 0 | |u https://doi.org/10.1007/s00382-014-2446-4 |q text/html |z Onlinezugriff via DOI |
| 898 | |a BK010053 |b XK010053 |c XK010000 | ||
| 900 | 7 | |a Metadata rights reserved |b Springer special CC-BY-NC licence |2 nationallicence | |
| 908 | |D 1 |a research-article |2 jats | ||
| 949 | |B NATIONALLICENCE |F NATIONALLICENCE |b NL-springer | ||
| 950 | |B NATIONALLICENCE |P 856 |E 40 |u https://doi.org/10.1007/s00382-014-2446-4 |q text/html |z Onlinezugriff via DOI | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Zhang |D Wei |u Earth System Modeling Center (ESMC) and Climate Dynamics Research Center, Nanjing International Academy of Meteorological Sciences (NIAMS), Key Laboratory of Meteorological Disaster, Ministry of Education and Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science and Technology, 210044, Nanjing, China |4 aut | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Leung |D Yee |u Department of Geography and Resource Management, The Chinese University of Hong Kong, Shatin, Hong Kong, China |4 aut | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Fraedrich |D Klaus |u Max Planck Institute for Meteorology, KlimaCampus, Hamburg, Germany |4 aut | ||
| 950 | |B NATIONALLICENCE |P 773 |E 0- |t Climate Dynamics |d Springer Berlin Heidelberg |g 44/11-12(2015-06-01), 2965-2977 |x 0930-7575 |q 44:11-12<2965 |1 2015 |2 44 |o 382 | ||