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Comparison of Ground Based Measurements of Solar UV Index with Satellite Estimation at Four Sites of Nepal

机译:尼泊尔四个地点的地面太阳紫外线指数测量与卫星估计的比较

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The main objective of this study is to compare the ground based measurements and satellite estimation of solar UV index in four sites namely, Kathmandu, Pokhara, Biratnagar and Lukla. Kathmandu (27.72°N, 85.32°E), Pokhara (28.22°N, 83.32°E) Biratnagar (26.45°N, 87.27° E) and Lukla ( 27.69°N, 86.73°E) and are located at an elevation of 1350m, 800m, 72m and 2850m respectively from the sea level. The ground based measurements and satellite estimation were performed by NILUUV irradiance meter and EOS Aura OMI satellite. The NILUUV irradiance meter is a six channel radiometer designed to measure hemispherical irradiances on a flat surface. The Ozone Monitoring Instrument (OMI) on board, the NASA EOS Aura space craft is a nadir viewing spectrometer that measures solar reflected and back scattered light in ultraviolet and visible spectrum. The study shows that OMI overestimate the ground based data before monsoon by 71.28%, 47.29%, 27.92% and 35.83% respectively at Kathmandu, Pokhara, Biratnagar and Lukla. However during the monsoon period the same comes down to 8.55%, 15.63%, 10.74%, and 11.33% respectively. The main reason behind these discrepancies might be due to the spatial resolution of the satellite which estimates the UV Index on the basis of 13×24 km2 in nadir where as the ground measurement is for a single point. The correlation between satellite derived and ground measured ozone column was found to be 91 % and 89% for Kathmandu and Lukla respectively. DOI: http://dx.doi.org/10.3126/jie.v8i3.5932 JIE 2011; 8(3): 58-71
机译:这项研究的主要目的是比较加德满都,博克拉,比拉特纳加尔和卢克拉四个地点的地面测量结果和卫星对太阳紫外线指数的估计。加德满都(27.72°N,85.32°E),博克拉(28.22°N,83.32°E)比拉特纳加尔(26.45°N,87.27°E)和卢克拉(27.69°N,86.73°E)都位于海拔1350m距海平面分别为800m,72m和2850m。通过NILUUV辐照度仪和EOS Aura OMI卫星进行地面测量和卫星估计。 NILUUV辐照度计是六通道辐射计,设计用于测量平面上的半球辐照度。 NASA EOS Aura太空船上的臭氧监测仪(OMI)是一种天底观察光谱仪,可测量紫外线和可见光谱中的太阳反射光和向后散射的光。研究显示,OMI在加德满都,博克拉,比拉特纳加尔和卢克拉的季风前地面数据分别高估了71.28%,47.29%,27.92%和35.83%。但是,在季风期间,分别下降到8.55%,15.63%,10.74%和11.33%。这些差异背后的主要原因可能是由于卫星的空间分辨率,该分辨率根据最低点的13×24 km2估算了紫外线指数,而地面测量是针对单个点的。发现加德满都和卢克拉的卫星衍生臭氧和地面实测臭氧柱之间的相关性分别为91%和89%。 DOI:http://dx.doi.org/10.3126/jie.v8i3.5932 JIE 2011; 8(3):58-71

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