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Comparison of UV Index and Total Ozone Column of Aura/OMI and Ground Measurement from Nepal Himalayas

机译:尼泊尔喜马拉雅山Aura / OMI紫外线指数和总臭氧柱的比较以及地面测量

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Ground UV index and total ozone measured from four stations of Nepal Himalaya using NILU UV Multiband Filter Radiometer (MBFR) were compared with that of the Aura/OMI satellite products using the data from October 2008 to December 2010. The main goal of the validation was to find how the satellite products deviate with that of ground measurement in the mountainous sites where the stations have unique set of geographical and environmental conditions. The altitudes of the stations vary from 72 m to 2850 m in a short span of horizontal distance. The comparison was done for clear-sky and cloudy-sky condition using Cloud Transmission Factor (CLT) as a proxy. It was found that UV indices estimated by the satellite have higher values compared to ground instrument. The relative difference (bias) of the four stations are varied from 34.5 ± 24.0% to 47.9 ± 17.4% for cloud free condition and from 106.4 ± 81.44 % to 286.4 ± 254.8% for cloudy condition. The correlation coefficients are more than 0.8 for cloud free condition. The total ozone column comparison showed the mean relative difference (bias) range from -2.17 ± 3.52% to 2.97 ± 3.92% under cloud free condition and -4.42 ± 5.64% to 1.36 ± 6.14% under cloudy condition. The possible factors for this discrepancy are discussed and some important factors are highlighted. DOI: http://dx.doi.org/10.3126/jie.v8i3.5938 JIE 2011; 8(3): 114-129
机译:使用2008年10月至2010年12月的数据,对使用NILU紫外线多波段滤光辐射计(MBFR)在尼泊尔喜马拉雅山四个站点测得的地面紫外线指数和总臭氧与Aura / OMI卫星产品的地面紫外线指数和总臭氧进行了比较。验证的主要目标是在这些站点具有独特的地理和环境条件的山区,找到卫星产品与地面测量的偏差。在短距离的水平距离内,这些站的高度从72 m到2850 m不等。使用“云传输因子”(CLT)作为代理,对晴空条件进行了比较。发现与地面仪器相比,卫星估算的紫外线指数具有更高的值。四个云站的相对差(偏差)在无云情况下从34.5±24.0%变为47.9±17.4%,在阴天情况下从106.4±81.44%到286.4±254.8%。对于无云条件,相关系数大于0.8。臭氧总柱比较显示,在无云条件下,平均相对差异(偏差)范围为-2.17±3.52%至2.97±3.92%,在阴云条件下,平均相对差异范围为-4.42±5.64%至1.36±6.14%。讨论了造成这种差异的可能因素,并突出了一些重要因素。 DOI:http://dx.doi.org/10.3126/jie.v8i3.5938 JIE 2011; 8(3):114-129

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