https://scholars.lib.ntu.edu.tw/handle/123456789/571828
標題: | Relative roles of energy and momentum fluxes in the tropical response to extratropical Thermal Forcing | 作者: | Hwang Y.-T Tseng H.-Y Li K.-C Kang S.M Chen Y.-J Chiang J.C.H. YEN-TING HWANG |
關鍵字: | Budget control; Cells; Clouds; Cytology; Oceanography; Surface waters; Time measurement; Transient analysis; Tropics; American meteorological societies; Circulation changes; Copyright informations; Eddy momentum flux; Intertropical convergence zone; Meridional temperature gradient; Mixed layer depths; Sea surface temperature (SST); Momentum; air-sea interaction; climate forcing; energy flux; extratropical environment; Hadley cell; mixed layer; momentum; momentum transfer; teleconnection; temperature effect; temperature gradient | 公開日期: | 2021 | 卷: | 34 | 期: | 10 | 起(迄)頁: | 3771-3786 | 來源出版物: | Journal of Climate | 摘要: | This study investigates the transient responses of atmospheric energy and momentum fluxes to a time-invariant extratropical thermal heating in an atmospheric model coupled to an aquaplanet mixed layer ocean with the goal of understanding the mechanisms and time scales governing the extratropical-to-tropical connection. Two distinct stages are observed in the teleconnection: 1) A decrease in the meridional temperature gradient in midlatitudes leads to a rapid weakening of the eddy momentum flux and a slight reduction of the Hadley cell strength in the forced hemisphere. 2) The subtropical trades in the forced hemisphere decrease and reduce evaporation. The resulting change to sea surface temperature leads to the development of a cross-equatorial Hadley cell, and the intertropical convergence zone shifts to the warmer hemisphere. The Hadley cell weakening in the first stage is related to decreased eddy momentum flux divergence, and the response time scale is independent of the mixed layer depth. In contrast, the time taken for the development of the cross-equatorial cell in the latter stage increases as the mixed layer depth increases. Once developed, the deep tropical cross-equatorial cell response is an order of magnitude stronger than the initial subtropical response and dominates the anomalous circulation. The analysis combines the momentum and energetic perspectives on this extratropical-to-tropical teleconnection and moreover shows that the subtropical circulation changes associated with the momentum budget occur with a time scale that is distinct from the deep tropical response determined by the thermal inertia of the tropical ocean. ? 2021 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy |
URI: | https://www.scopus.com/inward/record.uri?eid=2-s2.0-85105336578&doi=10.1175%2fJCLI-D-20-0151.1&partnerID=40&md5=77a9ee30442ee7d7b1ee497ecd27b821 https://scholars.lib.ntu.edu.tw/handle/123456789/571828 |
ISSN: | 8948755 | DOI: | 10.1175/JCLI-D-20-0151.1 | SDG/關鍵字: | Budget control; Cells; Clouds; Cytology; Oceanography; Surface waters; Time measurement; Transient analysis; Tropics; American meteorological societies; Circulation changes; Copyright informations; Eddy momentum flux; Intertropical convergence zone; Meridional temperature gradient; Mixed layer depths; Sea surface temperature (SST); Momentum; air-sea interaction; climate forcing; energy flux; extratropical environment; Hadley cell; mixed layer; momentum; momentum transfer; teleconnection; temperature effect; temperature gradient |
顯示於: | 大氣科學系 |
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