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Study of Atmospheric Scattering and Absorbing Aerosols at 550nm over nearby Western Indian Tropical sites of Thar Desert effected Region

机译:近距离西部印地安区热带地区550nm的大气散射和吸收气溶胶的研究

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The first time experimental results based on spaced satellite observations of different kinds of aerosols properties have been described over two different contrast environmental conditions locations in western tropical Indian region specifically first at Jaisalmer (26.90°N, 69.90°E, 220 m above mean sea level (amsl)) located in central Thar dessert vicinity of western Indian site over Indian Thar Desert region and another at Udaipur (24.6° N, 73.7° E, 560 m amsl) site concerning to semi-urban and semi arid place of hilly areas. The daily values of aerosols optical depth absorption at 500nm (AOD abs 500nm), aerosols optical depth extinction at 500nm (AOD ext 500nm) along with aerosols optical depth at 500nmon (AOD 500nm) of eleven year period from Jan., 2004 to Dec., 2014 are basis of primary database of the present investigation. From the synthesis if the above database and the basis of rigorous statistical approach, following some of interesting facts are noted (i) larger annual monthly AOD variation of 0.93 is noted over JSM when compared to observed annual monthly change in AOD cycle, over UDP, of only 0.50 clearly indicating the more impact of desert influence activities about more than double times over JSM than UDP (ii) The higher abundance of absorbing aerosols occurrences about two time higher are seen in JSM in comparison to UDP. It indicates the clear evidence of strong optical absorption properties of useful solar mid visible wavelength at 550nm as the results of presence of more availability of dust aerosols as mineral natural type in pre-monsoon to post-monsoon over JSM which is also more predominant over JSM than the UDP region located far away from desert activity regime (iii) The greater sharing of extinction solar radiation effect on aerosols are more effective in pre-monsoon in UDP in reference to over JSM, where as in case of UDP, the aerosols effect through the scattering mechanism gradually reduce from monsoon to winter months as compared to observed over JSM. The more detailed analysis other important results are also discussed thoroughly in this paper.
机译:基于间隔卫星观测的第一次实验结果已经在斋沙默尔(26.90°N,69.90°E,220米上方平均海平面上)(26.90°N,69.90°E)在西部热带印度地区的两个不同造影环境条件下描述了不同类型的气溶胶性能的实验结果。 (AMSL))位于印度印度景点的中央塔尔甜点附近,在印度塔尔沙漠地区,另一个关于丘陵地区的半城市和半城区干旱地区的Udaipur(24.6°N,73.7°E,560 M个AMSL)的另一个地方。 500nm(AOD ABS 500nm),500nm(Aod ext 500nm)的烟雾光学深度消光处的每日气溶胶光学深度吸收和500nmon(Aod 500nm)的Aerosols光学深度从2004年1月至12月到Dec. ,2014年是本调查的主要数据库的基础。从合成如果上述数据库和严格的统计方法的基础,请注意一些有趣的事实(i)与观察到的AOD周期的年每月变化,超过UDP时,JSM将指出0.93的年度月度每月AOD变化。只有0.50明显表明沙漠影响的影响超过JSM超过UDP(II)的多次较多的次数(ii),与UDP相比,JSM在JSM中看到了大约两次的吸收气溶胶的较高丰富。它表明,在550nm处,有用的太阳中可见波长的强光学吸收性能的明显证据是在季风前代矿物天然型作为矿物天然型矿物天然型的存在的结果,其在JSM上也更为占主导地位而不是远离沙漠活动的UDP地区(III),在UDP中,在UDP中,在UDP的前季隆的灭绝太阳辐射效应的较大分享在JSM中,在UDP的情况下,气溶胶效果与JSM相比,散射机制逐渐从季风到冬季逐渐减少。本文还讨论了其他重要结果的详细分析。

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