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Aerosol Characterization over a High Altitude Location in Central Himalayas

机译:喜马拉雅中部高海拔地区的气溶胶特征

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Our climate is strongly influenced by the manner in which solar radiation is absorbed and scattered in the Earth’s atmosphere. Atmospheric aerosols play an important role in modifying the radiation budget of the earth-atmosphere system. Aerosols have a direct impact on the atmosphere as they scatter and absorb solar and infrared radiations and indirectly affect the size distribution of cloud droplets. Hence, the knowledge of aerosols’ characteristics is the basic requirement for understanding the impact of aerosols on our environment. In order to delineate the optical and physical properties of aerosols, the collocated measurements of aerosols are carried out at Manora Peak (29.36 N; 79.45 E, altitude ~ 1960 meters), Nainital: a high altitude location in central Himalayas. Since the observing site is located geographically in the free troposphere, thus the aerosol measurements from such a region have the importance for providing a sort of background level of aerosol-parameters against which the impact of aerosol-loading from far-off low laying regions can be assessed. The retrieved parameters of aerosols at ARIES are comprised of aerosol optical depth, massumber concentrations of composite aerosols, BC mass concentration, total suspended particulate matter, total columnar ozone and water vapor content, meteorological parameters, traces gases etc. The analyzed results have been summarized in the present talk. DOI: http://dx.doi.org/10.3126/jie.v8i3.5935 JIE 2011; 8(3): 87-93
机译:太阳辐射在地球大气层中的吸收和散布方式强烈影响着我们的气候。大气气溶胶在改变地球大气系统的辐射预算方面起着重要作用。气溶胶散射并吸收太阳和红外辐射,并间接影响云滴的大小分布,因此对大气有直接影响。因此,了解气溶胶的特性是了解气溶胶对环境的影响的基本要求。为了描述气溶胶的光学和物理特性,对气溶胶的并置测量是在奈尼塔尔马诺拉峰(29.36 N; 79.45 E,海拔〜1960米)上进行的:奈米塔尔:喜马拉雅山中部的一个高海拔位置。由于观测地点在地理上位于对流层的自由空间中,因此,从该区域进行的气溶胶测量对于提供某种背景水平的气溶胶参数具有重要意义,而远距离低产卵地区的气溶胶装载量可对其产生影响被评估。在ARIES检索到的气溶胶参数包括气溶胶光学深度,复合气溶胶的质量/数量浓度,BC质量浓度,总悬浮颗粒物,总柱状臭氧和水蒸气含量,气象参数,微量气体等。分析结果包括在本次演讲中进行了总结。 DOI:http://dx.doi.org/10.3126/jie.v8i3.5935 JIE 2011; 8(3):87-93

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