DOI: 10.1016/j.atmosres.2017.10.013
Scopus记录号: 2-s2.0-85033448603
论文题名: Enhancement of orographic precipitation in Jeju Island during the passage of Typhoon Khanun (2012)
作者: Lee J.-T. ; Ko K.-Y. ; Lee D.-I. ; You C.-H. ; Liou Y.-C.
刊名: Atmospheric Research
ISSN: 1698095
出版年: 2018
卷: 201 起始页码: 58
结束页码: 71
语种: 英语
英文关键词: Hydraulic jump
; Jeju Island
; Khanun
; Orographic precipitation
; Seeder-feeder
Scopus关键词: Atmospheric movements
; Doppler radar
; Feeding
; Hurricanes
; Hydraulic jump
; Landforms
; Radar
; Reflection
; Accumulated rainfall
; Cloud resolving model
; Enhancement mechanism
; Geophysical conditions
; Jeju island
; Khanun
; Orographic precipitation
; Seeder-feeder
; Rain
; airflow
; computer simulation
; hydrometeorology
; mountain region
; numerical model
; orographic effect
; precipitation assessment
; raindrop
; rainfall
; typhoon
; vertical profile
; Cheju [Cheju (PRV/ISL)]
; Cheju [South Korea]
; South Korea
; Halla
英文摘要: Typhoon Khanun caused over 226 mm of accumulated rainfall for 6 h (0700 to 1300 UTC), localized around the summit of Mt. Halla (height 1950 m), with a slanted rainfall pattern to the northeast. In this study, we investigated the enhancement mechanism for precipitation near the mountains as the typhoon passed over Jeju Island via dual-Doppler radar analysis and simple trajectory of passive tracers using a retrieved wind field. The analysis of vertical profiles of the mountain region show marked features matching the geophysical conditions. In the central mountain region, a strong wind (≥ 7 m s− 1) helps to lift low-level air up the mountain. The time taken for lifting is longer than the theoretical time required for raindrop growth via condensation. The falling particles (seeder) from the upper cloud were also one of the reasons for an increase in rainfall via the accretion process from uplifted cloud water (feeder). The lifted air and falling particles both contributed to the heavy rainfall in the central region. In contrast, on the leeward side, the seeder-feeder mechanism was important in the formation of strong radar reflectivity. The snow particles (above 5 km) were accelerated by strong downward winds (≤−6 m s− 1). Meanwhile, the nonlinear jumping flow (hydraulic jump) raised feeders (shifted from the windward side) to the upper level where particles fall. To support these development processes, a numerical simulation using cloud-resolving model theoretically carried out. The accreting of hydrometeors may be one of the key reasons why the lee side has strong radar reflectivity, and a lee side weighted rainfall pattern even though lee side includes no strong upward air motion. © 2017 The Authors Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/108991
Appears in Collections: 影响、适应和脆弱性 气候变化事实与影响
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作者单位: Division of Earth Environmental System Science, Pukyong National University, Busan, South Korea; Numerical Modeling Center, Korea Meteorological Administration, Seoul, South Korea; Department of Environmental Atmospheric Sciences, Pukyong National University, Busan, South Korea; National Research Center for Disaster-free and Safe Ocean City, Dong-A University, Busan, South Korea; Department of Atmospheric Sciences, National Central University, Jhongli City, Taiwan
Recommended Citation:
Lee J.-T.,Ko K.-Y.,Lee D.-I.,et al. Enhancement of orographic precipitation in Jeju Island during the passage of Typhoon Khanun (2012)[J]. Atmospheric Research,2018-01-01,201