DOI: 10.1002/jgrd.50640
论文题名: The four cumulus cloud modes and their progression during rainfall events: A C-band polarimetric radar perspective
作者: Kumar V.V. ; Jakob C. ; Protat A. ; May P.T. ; Davies L.
刊名: Journal of Geophysical Research Atmospheres
ISSN: 21698996
出版年: 2013
卷: 118, 期: 15 起始页码: 8375
结束页码: 8389
语种: 英语
英文关键词: cumulus cloud
; shallow to deep transition
; tropics
Scopus关键词: Clouds
; Natural convection
; Polarimeters
; Radar
; Tropics
; Troposphere
; Cloud formation process
; Cumulus cloud
; Cumulus congestus clouds
; Objective definition
; Objective identification
; Polarimetric radars
; shallow to deep transition
; Tropical tropopause layers
; Rain
; cumulus
; data set
; identification method
; radar
; rainfall
; tropopause
; troposphere
英文摘要: There is no objective definition to separate cumulus congestus clouds from the shallow cumulus and deep clouds. This has generated misinterpretation about the role of congestus clouds to promote deep convection through the potential of moistening the middle troposphere. In this study, an objective identification for the different tropical cumulus modes is found by examining the occurrence frequency of the cloud cell top heights (CTHs) and near-ground (at 2.5 km height) rainfall properties of these cells using a three-season database of the Darwin C-band polarimetric radar. Four cumulus modes were identified, namely a shallow cumulus mode with CTH in the trade inversion layer (1-3 km), a congestus mode with tops in the highly stable middle troposphere (3-6.5 km), a deep convective mode with tops in the region of free convection (6.5-15 km), and an overshooting convection mode with tops in the tropical tropopause layer (CTH >15 km). The study also investigates the connections between these cumulus modes during heavy rainfall events. The congestus mode occurs predominantly from ~10 h prior to the peak rainfall event to ~2 h past the event. The deep cloud populations (Modes 3 and 4) have their maxima at and shortly after the time of the rainfall peak, with maximum occurrence just below the tropical tropopause layer. A comparison of the heavy rainfall events occurring in morning (oceanic) conditions against the afternoon (continental) conditions revealed a higher ratio of the shallow to the deep cloud population and a shorter transition time from the shallow to the onset of deep population in the morning-oceanic conditions than the afternoon-land conditions. It is also found through the analysis of the large-scale moisture budget data set that for both the morning and afternoon events, the moistening peaked before the peak in the congestus populations. Key Points Objective definition of four cumulus cloud modes using C-band radar observations Regime characterized by different underlying surfaces affects cloud formation process Congestus cloud moistening is not the main driver of convection transition ©2013. American Geophysical Union. All Rights Reserved. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/63468
Appears in Collections: 影响、适应和脆弱性 气候减缓与适应
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作者单位: School of Mathematical Sciences, Monash University, Melbourne VIC, Australia; Centre for Australian Weather and Climate Research, Australian Bureau of Meteorology, CSIRO, GPO Box 1289, Melbourne, VIC 3001, Australia; ARC Centre of Excellence for Climate System Science, Monash University, Melbourne VIC, Australia
Recommended Citation:
Kumar V.V.,Jakob C.,Protat A.,et al. The four cumulus cloud modes and their progression during rainfall events: A C-band polarimetric radar perspective[J]. Journal of Geophysical Research Atmospheres,2013-01-01,118(15)