Advances in Geosciences: Volume 10: Atmospheric Science (As) by Wing-Huen Ip, Jai-Ho Oh, Gyan Prakash Singh

By Wing-Huen Ip, Jai-Ho Oh, Gyan Prakash Singh

Rainfall over Thailand in the course of ENSO (1997 2000) (Wonlee & Prungchan) Formation of Tropical Cyclone Concentric Eye partitions by way of Wave suggest circulate Interactions (J Y Peng et al.) Anthropogenic Aerosol Radiative Forcing within the INDO-Gangetic Basi (S Dey & S N Tripathi)

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Extra info for Advances in Geosciences: Volume 10: Atmospheric Science (As)

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The positive EASM’s index anomalies cover the mid-lower of Yangtze Valley while negative anomalies cover South China and North China. Westerly anomalies appear in Yangtze River and northerly flows control South China and North China (Fig. 7(c)).

The weak descending motion in front of the monsoon convection helps to preserve the converged moisture near the surface. The air temperature profile observed from AIRS satellite show that a relatively warm center lies in front of the rainfall maximum while a cold one overlapping the rainfall maximum. Therefore, the monsoon rainfall maximum is overlapped and followed by a dry-cold ABL and preceded by a warm–wet one. This provides a favorable condition for the northward migration of the convection from southern to northern SCS.

Zhao, Onset and Evolution of the South China Sea Monsoon and Its Interaction with the Ocean (China Meteor. Press, 1999), p. 381. 11. J. , Acta Ocea. Sin. 22 (2004) 369. 12. D. , Chinese Sci. Bull. 51 (2006) 2413. 13. X. Fu, B. Wang and L. Tao, Geophys. Res. Lett. 33 (2006) L03705. 14. Y. Zhang, Biases of NCEP/NCAR and ECMWF 40-Year Re-Analyses in East Asia, IAMAS 2005 Scientific Assembly, August 2–11, 2005, Beijing, China. 15. B. , J. Atmos. Sci. 63 (2006) 2462. 16. X. Jiang, T. Li and B. Wang, J.

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