Characteristics of thermal and geopotential height differences between continent and ocean and its role in the strength of the Asian summer monsoon
Author:
Publisher
Springer Science and Business Media LLC
Subject
Ocean Engineering,Oceanography
Link
http://link.springer.com/content/pdf/10.1007/s11802-005-0058-7.pdf
Reference13 articles.
1. Chang, C.P., Y. Zhang, and T. Li, 2000. Interannual and interdecadal variations of the East Asian summer monsoon and tropical Pacific SSTs. Part 2: Meridional structure of the monsoon. J. Clim., 13(24): 4326–4340.
2. Chou, C, 2003. Land-sea heating contrast in an idealized Asian summer monsoon. Clim. Dyn., 21; 11–25.
3. Fielder, P. C, 2002. Environmental change in the eastern tropical Pacific Ocean: review of ENSO and decadal variability. Mar. Ecol. Prog. Ser., 244: 265–283.
4. Fu, C, and J.O. Fletcher, 1985. The relationship between Tibet-tropical ocean thermal contrast and interannual variability of Indian monsoon rainfall. J. Clim. Appl. Meteor., 24: 841–847.
5. Gedalof, Z., and D.J. Smith, 2001. Interdecadal climate variability and regime-scale shifts in Pacific North America. Geophys. Res. Lett., 28: 1515–1518.
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1. Rapid Changes in Land‐Sea Thermal Contrast Across China's Coastal Zone in a Warming Climate;Journal of Geophysical Research: Atmospheres;2019-02-26
2. Thermal Contrast between the Middle-Latitude Asian Continent and Adjacent Ocean and Its Connection to the East Asian Summer Precipitation;Journal of Climate;2008-10-01
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