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Satellite estimation and ground measurements of solar UV index and influence of aerosol in ground based UV data in Kathmandu, Nepal

机译:尼泊尔加德满都的卫星估算和地面测量太阳紫外线指数以及气溶胶对地面紫外线数据的影响

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This paper presents the ground based measurement and satellite estimation of the solar UV Index (UVI) as well as the influence of aerosol in ground based UV data of Kathmandu. Kathmandu (27.720N, 85.320E) is located at an elevation of 1350m from the sea level. The measurements were based on one year data from January to December 2009. The Ground Based (GB) measurement and satellite estimation were performed by NILU-UV irradiance meter and EOS Aura OMI spacecraft. The NILU-UV irradiance meter measures UV radiation in different spectral range whereas the Ozone Monitoring Instrument (OMI) is a spectrometer which monitors the solar radiation in spectral range of 270-500 nm. Besides, the Microtops II Sunphotometer was also used in this study for the measurement of aerosol optical depth (AOD). The relative percentage difference between OMI and GB UVI during pre-monsoon (March, April and May) was 165.5% and that in monsoon (June, July, August and September) was 105.5%. Likewise the monthly mean UVI in April and July was found to be 5.7±1.6 and 7.5±2.5 while the monthly mean AOD for the same months were 1.12 and 0.44 respectively. Meanwhile the correlation between GB UVI and AOD at 500nm before monsoon was -0.69 whereas during monsoon its value was -0.43 . The above mentioned correlation in April was -0.86. During this study the higher values of AODs and OMI estimation were observed during the months of March to May. And this high aerosol content in Kathmandu valley was found capable of modifying the surface UV irradiance.
机译:本文介绍了太阳紫外线指数(UVI)的地面测量和卫星估计,以及气溶胶对加德满都地面紫外线数据的影响。加德满都(27.720N,85.320E)位于海拔1350m处。这些测量是基于2009年1月至2009年12月的一年数据。地面测量(GB)和卫星估算是通过NILU-UV辐照度仪和EOS Aura OMI航天器进行的。 NILU-UV辐照度计可测量不同光谱范围内的紫外线辐射,而臭氧监测仪(OMI)是一种光谱仪,可监测270-500 nm光谱范围内的太阳辐射。此外,Microtops II太阳光度计也用于本研究中的气溶胶光学深度(AOD)的测量。季风前(3月,4月和5月)的OMI和GB UVI的相对百分比差异为165.5%,而季风(6月,7月,8月和9月)的OMI与GB UVI的相对百分比差异为105.5%。同样,4月和7月的月平均UVI分别为5.7±1.6和7.5±2.5,而同月的月平均AOD分别为1.12和0.44。季风前500nm处GB UVI与AOD的相关性为-0.69,季风期间GB-UVI的相关性为-0.43。上述相关系数在4月为-0.86。在这项研究中,在3月到5月的几个月中观察到了较高的AOD和OMI估计值。在加德满都谷地发现如此高的气溶胶含量能够改变表面紫外线辐射。

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