Impacts of Four Types of ENSO Events on Tropical Cyclones Making Landfall over China's Mainland Based on Three Best-track Datasets  被引量:6

Impacts of Four Types of ENSO Events on Tropical Cyclones Making Landfall over China's Mainland Based on Three Best-track Datasets

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作  者:ZHANG Han GUAN Yuping 

机构地区:[1]State Key Laboratory of Tropical Oceanography,South China Sea Institute of Oceanology, Chinese Academy of Sciences [2]Graduate University of Chinese Academy of Sciences

出  处:《Advances in Atmospheric Sciences》2014年第1期154-164,共11页大气科学进展(英文版)

基  金:supported by The National Natural Science Foundation of China(Grant No.40976011);the Public Science and Technology Research Funds Projects of Ocean(Grant No.201105018);the National Key Basic Research Program of China(Grant No.2013CB430300)

摘  要:Impacts of EI Nino Modoki (ENM), La Nina Modoki (LNM), canonical EI Nifio (CEN) and canonical La Nifia (CLN) on tropical cyclones (TCs) that made landfall over China's Mainland during 1951-2011 are analysed using best-track data from China, the USA and Japan. Relative to cold phase years (LNM and CLN), landfalling TCs in warm years (ENM and CEN) have a farther east genesis location, as well as longer track lengths and durations, both in total and before landfall. ENM demonstrates the highest landfall frequency, most northerly mean landfall position, and shortest after-landfall sustainability (track length and duration), which indicate a more frequent and extensive coverage of China's Mainland by TCs, but with shorter after-landfall influence. CEN has low landfall frequency and the most southerly mean landfall location. LNM has the most westerly genesis location, being significantly farther west than the 1951-2011 average and leading to short mean track lengths and durations both in total or before landfall, all of which are significantly shorter than the 1951-2011 average. Variations in the low-level wind anomaly, vertical wind shear, mid-level relative humidity, steering flow, the monsoon trough and the western Pacific subtropical high (WPSH) can to some extent account for the features of frequency, location, track length and duration of landfalling TCs. Since ENSO Modoki is expected to become more frequent in the near future, the results for ENSO Modoki presented in this paper are of particular significance.Impacts of EI Nino Modoki (ENM), La Nina Modoki (LNM), canonical EI Nifio (CEN) and canonical La Nifia (CLN) on tropical cyclones (TCs) that made landfall over China's Mainland during 1951-2011 are analysed using best-track data from China, the USA and Japan. Relative to cold phase years (LNM and CLN), landfalling TCs in warm years (ENM and CEN) have a farther east genesis location, as well as longer track lengths and durations, both in total and before landfall. ENM demonstrates the highest landfall frequency, most northerly mean landfall position, and shortest after-landfall sustainability (track length and duration), which indicate a more frequent and extensive coverage of China's Mainland by TCs, but with shorter after-landfall influence. CEN has low landfall frequency and the most southerly mean landfall location. LNM has the most westerly genesis location, being significantly farther west than the 1951-2011 average and leading to short mean track lengths and durations both in total or before landfall, all of which are significantly shorter than the 1951-2011 average. Variations in the low-level wind anomaly, vertical wind shear, mid-level relative humidity, steering flow, the monsoon trough and the western Pacific subtropical high (WPSH) can to some extent account for the features of frequency, location, track length and duration of landfalling TCs. Since ENSO Modoki is expected to become more frequent in the near future, the results for ENSO Modoki presented in this paper are of particular significance.

关 键 词:EI Nino-Southern Oscillation tropical Pacific anomaly tropical storm coastal China thermodynamic and dy-namic analysis 

分 类 号:P444[天文地球—大气科学及气象学]

 

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