Study on the rain structure using spaceborne rain radar
Study on the rain structure using spaceborne rain radar
批准号:
11440139
负责人:
NAKAMURA Kenji
金额:
$8.19万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (B)
财政年份:
1999
资助国家:
日本
项目状态:
已结题
起止时间:
1999 至 2001
中文摘要
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英文摘要
Rain distribution and structure were investigated using satellite-borne rain radar. The satellite is the Tropical Rainfall Measuring Mission one (TRMM) which is equipped with the world-first spacebome rain radar. Using the radar data we found :( 1 ) shallow precipitation system commonly appears over vast ocean. Over the Pacific Ocean, the height is high for west part and low for east part. Over the land, the shallow precipitation system is not significant.( 2 ) Diurnal variation of rain is significant for tropical regions where the land-ocean contrast is strong, especially, around the maritime continent.( 3 ) In the Asian monsoon season, weak but persistent rain appears around the west side of the Indochina Peninsula, and high and strong rain systems appear over the central and east side of the peninsula.( 4 ) High precipitation system with a downward decreasing rain profile likely appear in the transition region of wet and dry regions over India. Similar characteristics appears over Afiica.Another objective is the study to the atmospheric structure over India which is the key region for the Asian monsoon. We performed radiosonde observation in the south of India in August and September 2000. Lower atmosphere wind profiler (WP) data were also analyzed. From WP data, distinct diurnal variation of the planetary boundary layer was detected. The sonde data also showed the diurnal variation of the planetary boundary layer. They also showed that the planetary boundary layer is high compared with that in Japan.
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Krishna Reddy, K., T. Kozu, K. Nakamura, Y. Ohno, P. Srinebasulu, V. Koomath, A. Ram Jain, P. Bajarama Rao, R. Ranga Rao, G. Viswanthan and D. Narayana Rao: "Lower atmospheric wind profiler at Gadanki, tropical India : Initial results"Meteorologische Zeit
Krishna Reddy、K.、T. Kozu、K. Nakamura、Y. Ohno、P. Srinebasulu、V. Koomath、A. Ram Jain、P. Bajarama Rao、R. Ranga Rao、G. Viswanthan 和 D. Narayana Rao:
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Short, D and K. Nakamura: "TRMM radar observations of shallow precipitation over the tropical oceans"J. Climate. 13(23). 4107-4124 (2000)
Short, D 和 K. Nakamura:“热带海洋浅层降水的 TRMM 雷达观测”J。
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Krishna Reddy, K., T.Kozu, K.Nakamura, et al.: "Lower atmospheric wind profiler at Gadanki, tropical India : Initial results"Meteorologische Zeitschrift. 10(6). 457-468 (2001)
Krishna Reddy, K.、T.Kozu、K.Nakamura 等人:“热带印度 Gadanki 的低层大气风廓线仪:初步结果”Meteorologische Zeitschrift。
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Krishna Reddy, K., T.Kozu, Y.Ohno, K.Nakamura, A.Higuchi, et al.: "Planetary boundary layer and precipitation studies Using Lower Atmospheric Wind Profiler over Tropical India"Radio Science. (accepted). (2002)
Krishna Reddy、K.、T.Kozu、Y.Ohno、K.Nakamura、A.Higuchi 等人:“利用热带印度低层大气风廓线仪进行行星边界层和降水研究”无线电科学。
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Krishna Reddy, K., T. Kozu, Y. Ohno, K. Nakamura, A. Higuchi, K. M. Chandra Reddy, V.K. Anandan, P. Srinivasula, A.R. Jain, P.B. Rao, R. Ranga Rao, G. Viswanathan and D. Narayana Rao: "Planetary boundary layer and precipitation studies Using Lower Atmosph
Krishna Reddy、K.、T. Kozu、Y. Ohno、K. Nakamura、A. Higuchi、K. M. Chandra Reddy、V.K.
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