Modern Climatology by S. Wang, R. Gillies
By S. Wang, R. Gillies
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Extra info for Modern Climatology
2010), Improving the Australian tropical cyclone database: Extension of GMS satellite image archive. In Indian Ocean Tropical Cyclones and Climate Change, Y. ), pp. 1007/978-90-481-3109-9_24. 40 Modern Climatology Camargo, S. A. , (2007), Use of a genesis potential index to diagnose ENSO effects of tropical cyclone genesis. Journal of Climate, 20, pp. 48194834. , (2000) Tropical cyclone activity over the western North Pacific associated with El Niño and La Niña events. J. Climate, 13, 2960-2972.
During the ENSO cold phase (Fig. 12b), the zone of relatively weak wind shear moves westwards with a minimum centre at about 160°E to 175°E. The contour of 10 m-1 moves southwards to about 15°S to 20°S across the whole basin. This spatial distribution of vertical wind shear contributes to increased TC activity over the area west of the dateline and shifting area of enhanced cyclogenesis and TC development closer to Australia during La Niña seasons. Southern Hemisphere Tropical Cyclone Climatology (a) (b) Fig.
Forecasting, 18, 345-356. 2 Indian Monsoon Depression: Climatology and Variability Jin-Ho Yoon1,* and Wan-Ru (Judy) Huang2 1Pacific Northwest National Laboratory, Richland, WA Carpenter Asia-Pacific Climate Impact Centre School of Energy and Environment, City University of Hong Kong, Hong Kong 1USA 2China 2Guy 1. , Krishnamurti 1979). Most importantly this rainfall is the major source of fresh water to various human activities such as agriculture. 1) with the monsoon trough extended from northern India across Indochina to the Western Tropical Pacific (WTP).