DOI: 10.1175/JCLI-D-17-0601.1
Scopus记录号: 2-s2.0-85048181684
论文题名: Influence of intraseasonal-interannual oscillations on tropical cyclone genesis in the Western North Pacific
作者: Chen J.-M. ; Wu C.-H. ; Chung P.-H. ; Sui C.-H.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2018
卷: 31, 期: 12 起始页码: 4949
结束页码: 4961
语种: 英语
英文关键词: ENSO
; Madden-Julian oscillation
; Tropical cyclones
Scopus关键词: Atmospheric pressure
; Hurricanes
; Mechanical waves
; Storms
; Tropics
; Vorticity
; ENSO
; Equatorial Rossby waves
; Madden-Julian oscillation
; Southern oscillation
; Tropical cyclone
; Tropical disturbances
; Vertical wind shear
; Western North Pacific
; Climatology
; annual variation
; climate oscillation
; El Nino-Southern Oscillation
; Madden-Julian oscillation
; Rossby wave
; seasonal variation
; tropical cyclone
; vorticity
; Pacific Ocean
; Pacific Ocean (North)
英文摘要: Influences of intraseasonal-interannual oscillations on tropical cyclone (TC) genesis are evaluated by productivity of TC genesis (PTCG) from the developing (TCd) and nondeveloping (TCn) precursory tropical disturbances (PTDs). A PTD is identified by a cyclonic tropical disturbance with a strong-enough intensity, a large-enough maximum center, and a long-enough lifespan. The percentage value of PTDs evolving into TCd is defined as PTCG. The analysis is performed over the western North Pacific (WNP) basin during the 1990-2014 warm season (May-September). The climatological PTCG in the WNP basin is 0.35. Counted in a common period, mean numbers of PTDs in the favorable and unfavorable conditions of climate oscillations for TC genesis [such as equatorial Rossby waves (ERWs), the Madden-Julian oscillation (MJO), and El Niño-Southern Oscillation (ENSO)], all exhibit a stable value close to the climatological mean [~31 (100 days)-1]. However, PTCG increases (decreases) during the phases of positive-vorticity (negative-vorticity) ERWs, the active (inactive) MJO, and El Niño (La Niña) years. PTCG varies from 0.17 in the most unfavorable environment (La Niña, inactive MJO, and negative-vorticity ERW) to 0.56 in the most favorable environment (El Niño, active MJO, and positive-vorticity ERW). ERWs are most effective in modulating TC genesis, especially in the negative-vorticity phases. Overall, increased PTCG is facilitated with strong and elongated 850-hPa relative vorticity overlapping a cyclonic shear line pattern, while decreased PTCG is related to weak relative vorticity. Relative vorticity acts as the most important factor to modulate PTCG, when compared with vertical wind shear and 700-hPa relative humidity. © 2018 American Meteorological Society. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/111508
Appears in Collections: 气候减缓与适应
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作者单位: Department of Maritime Information and Technology, National Kaohsiung Marine University, Kaohsiung, Taiwan; Department of Atmospheric Science, National Taiwan University, Taipei, Taiwan; Department of History and Geography, University of Taipei, Taipei, Taiwan
Recommended Citation:
Chen J.-M.,Wu C.-H.,Chung P.-H.,et al. Influence of intraseasonal-interannual oscillations on tropical cyclone genesis in the Western North Pacific[J]. Journal of Climate,2018-01-01,31(12)