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

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

ISBN-10: 981283611X

ISBN-13: 9789812836113

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

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

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Y. Ding, C. Li and Y. Liu, Adv. Atmos. Sci. 21 (2004) 343. 8. R. Huang, L. Gu, L. Zhou and S. Wu, Adv. Atmos. Sci. 23 (2006) 909. 9. P. C. -P. Chang, Adv. Atmos. Sci. 14 (1997) 195. 10. 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.

Relatively, large echo appeared under the cloud till 7:00 (local time) in the morning. On that day, temperature and humidity largely changed at 7:00 (local time). Wind direction was northwest, and its speed was 8 m/s. The 10-h cloud elevation indicates the passage of highly developed low pressure. Figure 3 is the result observed during 0–12 on September 18, 2006. It was a windy day. Low clouds of less than 1 km altitude appeared during 0–5 h. They raised the altitude up to 2 km during 5–8 h. The lidar echo from these clouds was sparse and largely fluctuating in altitude.

Lu, X. Zhang and J. Chen Fig. 3. Same as Fig. 2 except for the distribution of the rainfall in China average for 1958–2001. Season over South China comes into the peak period and the heavy storms occur in South China frequently (Fig. 3(a)). 2. EASM strengthen and jump northward to the mid-lower of Yangtze Valley At the 33rd pentad, as the West Pacific subtropical high jump northward at first time, the southeasterly flows from the western subtropical high join the southwesterly flows from SCS at the mid-lower of Yangtze Valley and southwest of Japan (Fig.

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