A possible cause for different diurnal variations of warm season rainfall as shown in station observations and TRMM 3B42 data over the southeastern Tibetan plateau-Reference-Cited by-同舟云学术

A possible cause for different diurnal variations of warm season rainfall as shown in station observations and TRMM 3B42 data over the southeastern Tibetan plateau

Published:2011-12-23 Issue:1 Volume:29 Page:193-200
ISSN:0256-1530
Container-title:Advances in Atmospheric Sciences
language:en
Short-container-title:Adv. Atmos. Sci.

Author:

Chen Haoming,Yuan Weihua,Li Jian,Yu Rucong

Publisher

Springer Science and Business Media LLC

Subject

Atmospheric Science

Link

http://link.springer.com/content/pdf/10.1007/s00376-011-0218-1.pdf

Reference24 articles.

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2. Fujinami, H., S. Nomura, and T. Yasunari, 2005: Characteristics of diurnal variations in convection and precipitation over the southern Tibertan Plateau during summer. SOLA, 1, 49–52.

3. Huffman, G. J., and Coauthors, 2007: The TRMM Multisatellite Precipitation Analysis (TMPA): Quasiglobal, multiyear, combined-sensor precipitation estimates at fine scales. J. Hydrometeorology, 8, 38–55.

4. Kuo, H. L., and Y. F. Qian, 1981: Influence of the Tibetian Plateau on cumulative and diurnal changes of weather and climate in summer. Mon. Wea. Rev., 109, 2337–2356.

5. Kuwagata, T., A. Numaguti, and N. Endo, 2001: Diurnal variation of water vapor over the central Tibetan Plateau during summer. J. Meteor. Soc. Japan, 79, 401–418.

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