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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Extra info for Advances in Geosciences: Volume 10: Atmospheric Science (As)
The center is located on the east of Tokyo bay, about 10 km south of Chiba University. There is an industrial area and a busy load on the seaside (west of the center). 3. PAL Observation The main advantage of the continuous and long-term observation is capturing the local weather change that takes place in a time scale of several hours. Especially, the system can monitor the onset and recovery of bad weather conditions and changes in polluted airs. These features are largely dependent on the site locations and conditions (urban/rural/mountains/ waters).
Acknowledgments TL was supported by ONR grants N000140710145 and N000140210532 and NRL subcontract N00173-06-1-G031. The International Paciﬁc Research Center is partially sponsored by the Japan Agency for MarineEarth Science and Technology (JAMSTEC). April 10, 2009 12:4 AOGS 2007 - AS Volume 9in x 6in Satellite-Observed 3D Moisture Structure b672-V10-ch04 39 References 1. S. Y. Tao and L. X. Chen, Monsoon Meteorology (Oxford University Press, 1987), p. 60. 2. K. M. Lau and S. Yang, Adv. Atmos. Sci.
Singh c World Scientiﬁc Publishing Company SATELLITE-OBSERVED 3D MOISTURE STRUCTURE AND AIR–SEA INTERACTIONS DURING SUMMER MONSOON ONSET IN THE SOUTH CHINA SEA YONGSHENG ZHANG International Pacific Research Center, SOEST, University of Hawaii at Manoa, POST Bldg. 401, 1680 East-West Road, Honolulu, Hawaii 96822, USA TIM LI International Pacific Research Center and Department of Meteorology, SOEST, University of Hawaii at Manoa, POST Bldg 401, 1680 East-West Road, Honolulu, Hawaii 96822, USA In this chapter, water vapor and air temperature proﬁles observed by the Atmospheric Infrared Sounder (AIRS), sea surface temperature (SST) and rain rate observed by TRMM Microwave Imager (TMI), and QuikSCAT surface wind for 2003–2006 are used to identify the 3D moisture structure and air–sea interaction processes during the onset of the South China Sea summer monsoon (SCSSM).