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  4. Influence of intraseasonal-interannual oscillations on tropical cyclone genesis in the Western North Pacific
 
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Influence of intraseasonal-interannual oscillations on tropical cyclone genesis in the Western North Pacific

Journal
Journal of Climate
Journal Volume
31
Journal Issue
12
Pages
4949-4961
Date Issued
2018
Author(s)
Chen, J.-M.
Wu, C.-H.
Chung, P.-H.
Sui, C.-H.  
DOI
10.1175/JCLI-D-17-0601.1
URI
https://www.scopus.com/inward/record.uri?eid=2-s2.0-85048181684&doi=10.1175%2fJCLI-D-17-0601.1&partnerID=40&md5=45da7051027d5b296268aa0520dffef4
https://scholars.lib.ntu.edu.tw/handle/123456789/406272
Abstract
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.
Subjects
ENSO; Madden-Julian oscillation; Tropical cyclones
SDGs

[SDGs]SDG13

Other Subjects
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)
Type
journal article

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