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 through 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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5). 1965-1979 1958-1964 50 50 (a) (b) 45 42 39 37 38 40 36 30 35 34 40 45 33 32 31 30 25 42 43 39 46 35 40 44 41 45 4341 35 38 37 30 36 35 40 44 45 34 30 31 25 32 28 33 28 20 20 29 15 15 10 100 105 110 115 120 125 130 135 140 50 10 100 105 110 115 120 125 135 140 55 (c) (d) 50 45 41 40 41 42 43 45 40 40 39 35 38 36 30 30 33 37 32 45 44 34 35 32 25 28 20 15 15 110 115 120 125 130 135 140 10 95 100 105 110 37 35 31 30 31 20 105 36 35 25 10 100 130 1994-2001 1980-1993 39 3845 42 43 44 40 46 33 34 29 28 30 27 115 120 125 130 135 140 Fig.

X. Bai, A. Wu and Y. 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.

3(c), solid thick line) are concurrent with an increase of the latent heat flux (Fig. 3(c)) relevant to a burst of westerly in these two regions (Figs. 2(b) and (c), blue lines), indicating that the moisture change at ABL is not attributed to the surface evaporation. (4) While a strong convection maximum co-locates with a strong convergence near the surface, convergence also occurs in front of the April 10, 2009 12:4 AOGS 2007 - AS Volume 9in x 6in b672-V10-ch04 Y. Zhang and T. Li 34 rainfall maximum, tending to overlap the region of enhanced moisture (Fig.

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