globalchange  > 气候减缓与适应
DOI: 10.1175/JCLI-D-17-0118.1
Scopus记录号: 2-s2.0-85043238575
论文题名:
Regime change behavior during Asian monsoon onset
作者: Geen R.; Lambert F.H.; Vallis G.K.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2018
卷: 31, 期:8
起始页码: 3327
结束页码: 3348
语种: 英语
英文关键词: Climate classification/regimes ; Dynamics ; Hadley circulation ; Intertropical convergence zone ; Monsoons
Scopus关键词: Budget control ; Cells ; Cytology ; Dynamics ; Vorticity ; Absolute vorticity ; Climate classification/regimes ; Hadley circulation ; Intertropical convergence zone ; Monsoons ; Overturning circulation ; Primitive equations ; Southern Hemisphere ; Atmospheric thermodynamics
英文摘要: As the ITCZ moves off the equator on an aquaplanet, the Hadley circulation transitions from an equinoctial regime with two near-symmetric, significantly eddy-driven cells to a monsoon-like regime with a strong, thermally direct cross-equatorial cell, intense low-latitude precipitation, and a weak summer hemisphere cell. Dynamical feedbacks appear to accelerate the transition. This study investigates the relevance of this behavior to monsoon onset by using primitive equation model simulations ranging from aquaplanets to more realistic configurations with Earth's continents and topography. A change in the relationship between ITCZ latitude and overturning strength is identified once the ITCZ moves poleward of approximately 7°. Monsoon onset is associated with off-equatorial ascent in regions of nonnegligible planetary vorticity, and this is found to generate a vortex stretching tendency that reduces upper-level absolute vorticity. In an aquaplanet, this causes a transition to the cross-equatorial, thermally direct regime, intensifying the overturning circulation. Analysis of the zonal momentum budget suggests that a stationary wave, driven by topography and land-sea contrast, can trigger a similar transition in the more realistic model configuration, with the wave extending the ascent region of the Southern Hemisphere Hadley cell northward, and enhanced overturning then developing to the south. These two elements of the circulation resemble the East and South Asian monsoons. © 2018 American Meteorological Society.
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/111580
Appears in Collections:气候减缓与适应

Files in This Item:

There are no files associated with this item.


作者单位: College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, United Kingdom

Recommended Citation:
Geen R.,Lambert F.H.,Vallis G.K.. Regime change behavior during Asian monsoon onset[J]. Journal of Climate,2018-01-01,31(8)
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Geen R.]'s Articles
[Lambert F.H.]'s Articles
[Vallis G.K.]'s Articles
百度学术
Similar articles in Baidu Scholar
[Geen R.]'s Articles
[Lambert F.H.]'s Articles
[Vallis G.K.]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Geen R.]‘s Articles
[Lambert F.H.]‘s Articles
[Vallis G.K.]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.