首页> 外文期刊>International Journal of Engineering Science and Technology >MEASUREMENTS OF RAIN DROP SIZE DISTRBUTION FROM RADAR REFLECTIVITY AND ASSOCIATED RAIN ATTENUATION OF RADIO WAVES
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MEASUREMENTS OF RAIN DROP SIZE DISTRBUTION FROM RADAR REFLECTIVITY AND ASSOCIATED RAIN ATTENUATION OF RADIO WAVES

机译:雷达反射率和无线电波相关的雨衰引起的雨滴尺寸分布的测量

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Radar measurements of rainfall at different climatological conditions have been taken into account emphasizing rain rate and associated radar reflectivity. It is observed from the analysis that the reflectivity measurement is being consistent at high rain intensities. From the knowledge of radar reflectivity, the rain drop size distribution is examined. The most probable drop size diameter and rain rate have been calculated wherefrom it appears that the most probable rain drop size vary exponentially with radar reflectivity and also with rain rate. The theoretical model implemented by using the measured rain drop sizes over the tropical sites also show similar kind of variation. For estimating rain attenuation two important parameters, viz., the point rainfall rates and the vertical and horizontal structures of rain have been considered. The elevation angle we have chosen is ~ 560 as most of the stations in India have that value of elevation angle with geostationary satellite. Taking the frequencies 11 to 14 GHz separately and 00 C isotherm height as 5.0 km, the effective rain height values are determined. The attenuation of radio waves due to rain are calculated for different rain rates assigning different ?-values. The attenuation is found to vary significantly with the ?-values. Also the attenuation curves are closer when the ?-values are of low order. An increase in attenuation with the ?-values is found to be more prominent for higher rain rates.
机译:已考虑了雷达在不同气候条件下的降雨测量结果,重点是降雨率和相关的雷达反射率。从分析中可以看出,在高降雨强度下反射率测量是一致的。根据雷达反射率的知识,检查了雨滴的大小分布。计算出最可能的水滴尺寸直径和降雨率,从中看来,最可能的水滴尺寸随雷达反射率以及降雨率呈指数变化。通过使用热带地区测得的雨滴大小实现的理论模型也显示出类似的变化。为了估算降雨衰减,已经考虑了两个重要参数,即点降雨率和降雨的垂直和水平结构。我们选择的仰角约为560,因为印度的大多数台站都具有地球静止卫星的仰角值。分别将11至14 GHz的频率和等温线00 C的高度设为5.0 km,可以确定有效的降雨高度值。针对分配了不同的α值的不同降雨率,计算了由于降雨造成的无线电波衰减。发现衰减随α值而显着变化。当α值低阶时,衰减曲线也更接近。发现随着α值的增加,衰减率的增加对于较高的降雨率更为显着。

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