Precipitation Type Specific Radar Reflectivity-rain Rate Relationships for Warsaw, Poland
نویسندگان
چکیده
منابع مشابه
Raindrop size distributions and radar reflectivity–rain rate relationships for radar hydrology*
The conversion of the radar reflectivity factor Z (mm6 m-3) to rain rate R (mm h-1) is a crucial step in the hydrological application of weather radar measurements. It has been common practice for over 50 years now to take for this conversion a simple power law relationship between Z and R. It is the purpose of this paper to explain that the fundamental reason for the existence of such power la...
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A Z-R relation is derived using a data set which consists of nine rain events selected from Singapore’s drop size distribution. Rain events are separated into convective and stratiform types of rain using two methods: the Gamache-Houze method, a simple threshold technique, and the Atlas-Ulbrich method. In the Atlas-Ulbrich method, the variability of the rain integral parameters R, Z, Nw, D0 and...
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متن کامل
Rain Rate-Radar Reflectivity Relationship for Drop Size Distribution and Rain Attenuation Calculation of Ku Band Signals
Mobile no:9573548993, Fax:08645 247249, 3. Professor, Department of ECE, K L University K L University, Vaddeswaram, Guntur, A.P, India 1. [email protected] [email protected] 2. Professor, Department of ECE, K L University 4. Associate Professor, Department of ECE, K L University K L University, Vaddeswaram, Guntur, A.P, India 2. [email protected] [email protected]
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2. Chinese Academy of Meteorological Sciences, Beijing,10086 Abstract Using OTT-Parsivel Laser Particle Spectrometer at Nanjing in East China, several times heavy rain droplet scale & velocity spectral data aquatic from Mt. Lushan weather stations (elevation 1300meters) Compared to the plain deep convective clouds heavy precipitation, the rain droplet size distribution (DSD) with two elevation ...
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ژورنال
عنوان ژورنال: Acta Geophysica
سال: 2016
ISSN: 1895-6572,1895-7455
DOI: 10.1515/acgeo-2016-0071