Abstract
The precipitation mechanisms of typhoon Naru (2001) revealed by radar observation was studied. A quality control sequence was applied to 12 hrs raw disdrometer data to get the drop size distribution. The disdrometer, integrated sounding system, rain gage network and dual-Doppler radar data were collected during Nari's landfall. The terrain following dual Doppler synthesis wind field shows the structure change of circulation and the topographic influence.
Original language | English |
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Pages | 138-139 |
Number of pages | 2 |
State | Published - 2004 |
Event | 26th Conference on Hurricanes and Tropical Meteorolgy - Miami, FL., United States Duration: 3 May 2004 → 7 May 2004 |
Conference
Conference | 26th Conference on Hurricanes and Tropical Meteorolgy |
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Country/Territory | United States |
City | Miami, FL. |
Period | 3/05/04 → 7/05/04 |