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Altitude profiles of cloud condensation nuclei characteristics across the Indo-Gangetic Plain prior to the onset of the Indian summer monsoon

机译:在印度夏季季风发作之前,云凝结核特征云凝结核特征的高度概况

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摘要

Concurrent measurements of the altitude profiles of the concentration of cloudcondensation nuclei (CCN), as a function of supersaturation(ranging from 0.2 % to 1.0 %), and aerosol optical properties(scattering and absorption coefficients) were carried out aboard aninstrumented aircraft across the Indo-Gangetic Plain (IGP) just prior to theonset of the Indian summer monsoon (ISM) of 2016. The experiment wasconducted under the aegis of the combined South-West Asian Aerosol–Monsoon Interactions and RegionalAerosol Warming Experiment (SWAAMI–RAWEX) campaign. The measurementscovered coastal, urban and arid environments. In general, the CCNconcentration was highest in the central IGP, decreasing spatially fromeast to west above the planetary boundary layer (PBL), which is∼1.5 km for the IGP during pre-monsoon period. Despite this, the CCNactivation efficiency at 0.4 % supersaturation was, interestingly,the highest over the eastern IGP (∼72 %), followed by thatin the west (∼61 %), and it was the least over thecentral IGP (∼24 %) within the PBL. In general, higheractivation efficiency is noticed above the PBL than below it. The centralIGP showed remarkably low CCN activation efficiency at all altitudes, whichappears to be associated with high black carbon (BC) mass concentrationthere, indicating the role of anthropogenic sources in suppressing the CCNefficiency. These first-ever CCN measurements over the western IGP, encompassing“the Great Indian Desert” also known as “the Thar Desert”, showed high CCNefficiency, ∼61 % at 0.4 % supersaturation, indicating thehygroscopic nature of the dust. The vertical structure of CCN properties isfound to be air mass dependent, with higher activation efficiency even overthe central IGP during the prevalence of marine air mass. Wet scavengingassociated with precipitation episodes seems to have reduced the CCNactivation efficiency below cloud level. An empirical relation has emergedbetween the CCN concentration and the scattering aerosol index (AI), whichwould facilitate the prediction of CCN from aerosol optical properties.
机译:的cloudcondensation核(CCN)的浓度的高度剖面并发测量,过饱和的函数(从0.2%至1.0%),和气溶胶的光学特性(散射和吸收系数)的对面进行搭乘aninstrumented飞机印-Gangetic平原(IGP)就在印度夏季风(ISM)的2016年实验组合西南亚气溶胶季风相互作用和气候变暖RegionalAerosol实验(SWAAMI-RAWEX)运动的支持下wasconducted的theonset之前。该measurementscovered沿海,城市和干旱环境。一般来说,CCNconcentration最高在中央IGP,空间fromeast减小到西行星边界层(PBL),其is~1.5公里用于在预季风期间的IGP上方。尽管如此,在0.4%的过饱和度CCNactivation效率,有趣的是,在最高的东部地区IGP(〜72%),其次是thatin西部(~61%),这是至少在thecentral IGP(~24%)在PBL内。一般而言,higheractivation效率的PBL比它下面注意到上述情况。所述centralIGP显示显着低的CCN活化效率在所有高度,whichappears具有高炭黑(BC)质量concentrationthere相关联,指示人为来源在抑制CCNefficiency的作用。这些第一次测量CCN西部上IGP,围绕“在印度大沙漠”也被称为“塔尔沙漠”,表现出较高的CCNefficiency,在0.4%的过饱和~61%,表明的尘埃thehygroscopic性质。 CCN属性的垂直结构isfound至是空气质量依赖性的,具有更高的活化效率甚至温习中央IGP海洋气团的流行期间。湿降水事件scavengingassociated似乎已经减少到低于云平的CCNactivation效率。经验关系已经emergedbetween的CCN浓度和散射气溶胶指数(AI),whichwould促进CCN的预测从气溶胶的光学性质。

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