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DOI | 10.1175/JCLI-D-20-0504.1 |
The detailed dynamics of the Hadley cell. Part II: December-February | |
Hoskins B.J.; Yang G.-Y. | |
发表日期 | 2021 |
ISSN | 0894-8755 |
起始页码 | 805 |
结束页码 | 823 |
卷号 | 34期号:2 |
英文摘要 | This paper complements an earlier paper on the June-August Hadley cell by giving a detailed analysis of the December-February Hadley cell as seen in a 30-yr climatology of ERA-Interim data. The focus is on the dynamics of the upper branch of the Hadley cell. There are significant differences between the Hadley cells in the two solsticial seasons. These are particularly associated with the ITCZs staying north of the equator and with mean westerlies in the equatorial regions of the east Pacific and Atlantic in December-February. The latter enables westward-moving mixed Rossby-gravity waves to be slow moving in those regions and therefore respond strongly to upstream off-equatorial active convection. However, the main result is that in both seasons it is the regions and times of active convection that predominantly lead to upper-tropospheric outflows and structures that average to give the mean flow toward the winter pole, and the steady and transient fluxes of momentum and vorticity that balance the Coriolis terms. The response to active convection in preferred regions is shown by means of regressions on the data from the climatology and by synoptic examples from one season. Eddies with tropical origin are seen to be important in their own right and also in their interaction with higher-latitude systems. There is support for the relevance of a new conceptual model of the Hadley cell based on the sporadic nature of active tropical convection in time and space. © 2020 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses). |
英文关键词 | Climatology; Clouds; Cytology; Tropics; Conceptual model; Coriolis terms; Equatorial regions; Higher latitudes; Rossby-gravity wave; Steady and transient; Tropical convection; Tropical origins; Cells; atmospheric convection; atmospheric wave; eddy; gravity wave; Hadley cell; intertropical convergence zone; potential vorticity; Rossby wave; vortex; westerly; Atlantic Ocean; Pacific Ocean; Pacific Ocean (East) |
语种 | 英语 |
来源期刊 | Journal of Climate
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/170956 |
作者单位 | Department of Meteorology, University of Reading, Reading, United Kingdom; Grantham Institute for Climate Change, Imperial College, London, United Kingdom; Climate Directorate, National Centre for Atmospheric Science, University of Reading, Reading, United Kingdom |
推荐引用方式 GB/T 7714 | Hoskins B.J.,Yang G.-Y.. The detailed dynamics of the Hadley cell. Part II: December-February[J],2021,34(2). |
APA | Hoskins B.J.,&Yang G.-Y..(2021).The detailed dynamics of the Hadley cell. Part II: December-February.Journal of Climate,34(2). |
MLA | Hoskins B.J.,et al."The detailed dynamics of the Hadley cell. Part II: December-February".Journal of Climate 34.2(2021). |
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