2015年7月
Does convection vary in different cloud disturbances?
ATMOSPHERIC SCIENCE LETTERS
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- 巻
- 16
- 号
- 3
- 開始ページ
- 305
- 終了ページ
- 309
- 記述言語
- 英語
- 掲載種別
- 研究論文(学術雑誌)
- DOI
- 10.1002/asl2.558
- 出版者・発行元
- WILEY-BLACKWELL
Deep moist convection is an element of cloud disturbances such as Madden-Julian oscillation (MJO), tropical cyclones (TCs), mid-latitudinal low depressions (MDL), and fronts (FRT). However, differences in convection characteristics in disturbances remain unclear. We first clarified the statistical features of the convection (structure, intensity, and environmental parameters) in various disturbances simulated by a global simulation with a sub-kilometre grid spacing. The convection in MJO (TC) was tall with a strong (weak) upward motion, and was driven by large convective available potential energy (strong low-level convergence). The convection in MDL and FRT was shorter and characterized by a strong vertical wind shear.
- リンク情報
- ID情報
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- DOI : 10.1002/asl2.558
- ISSN : 1530-261X
- ORCIDのPut Code : 33149621
- Web of Science ID : WOS:000358020000018
- ORCIDで取得されたその他外部ID : a:1:{i:0;a:1:{s:8:"other-id";s:19:"WOS:000358020000018";}}