首页> 外文期刊>Atmospheric Chemistry and Physics Discussions >Measurement report: Altitudinal variation of cloud condensation nuclei activation across the Indo-Gangetic Plain prior to monsoon onset and during peak monsoon periods: results from the SWAAMI field campaign
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Measurement report: Altitudinal variation of cloud condensation nuclei activation across the Indo-Gangetic Plain prior to monsoon onset and during peak monsoon periods: results from the SWAAMI field campaign

机译:测量报告:在季风发作之前和峰季蓬松期间,在季蓬松平原上的云凝结核激活的平坦变异:Swaami野战野外活动的结果

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Vertical distributions (altitude profiles) of condensation nuclei (CN) and cloud condensation nuclei (CCN) and their spatial variations across the Indo-Gangetic Plain (IGP) have been investigated based on airborne measurements carried out during the SWAAMI field campaign (June to July?2016) capturing the contrasting phases of the Indian monsoon activity in 2016 just prior to its onset and during its active phase. Prior to the monsoon onset, high concentrations of CN and CCN prevailed across the IGP, and the profiles revealed frequent occurrence of elevated layers (in the altitude range 1–3?km). Highest concentrations and elevated peaks with high values occurred over the central IGP. The scenario changed dramatically during the active phase of the monsoon, when the CN and CCN concentrations dropped (CN by 20?% to 30?% and CCN by 6?% to 25?%) throughout the IGP with more pronounced changes at altitudes higher than 3?km where decreases as high as? ?80?% were observed. These reductions have an east-to-west decreasing gradient, being most remarkable in the eastern IGP and very weak over the western IGP where the CN concentrations above 3?km increased during the monsoon. The activation ratios (ARs) showed contrasting features, increasing with increase in altitude, prior to the onset of monsoon, reversing the trend to decrease with increase in altitude during the active phase of the monsoon. The supersaturation spectrum became flatter during the active phase of the monsoon, indicating an increase in the hygroscopicity of aerosols following the mixing of surface-based emissions with the advected marine air mass.
机译:透明核(CN)和云凝结核(CCN)的垂直分布(高度曲线)以及跨甘曲平原(IGP)的空间变化是基于Swaami Field Campaign(6月至7月6月)的空中测量?2016年)在发病之前和在其活跃阶段之前,捕捉2016年印度季风活动的对比阶段。在季风发作之前,在IGP上占高浓度的CN和CCN,并且曲线透露出频繁发生升高的层(在高度范围内1-3 km)。在中央IGP上发生最高浓度和高值的升高峰。当在整个IGP中,当CN和CCN浓度在整个IGP中,当CN和CCN浓度下降时(CN和CCN浓度将20μl到30μl%和25μl%)下降(CN×20℃,CCN,CCN达到6μl25≤25μ%),这种情况发生了显着变化。超过3 km,在那里减少到何处&观察到80?%。这些减少有东部到西部的渐变,在东部IGP中是最显着的,在西部IGP方面非常弱,在季风期间CN浓度增加3 km。活化比(ARS)显示出对比度的特征,随着季风发作之前,随着高度的增加而增加,逆转季风活性阶段的高度增加趋势。在季风的活性相位期间,过饱和谱变得更加漂移,表明在具有完善的海洋空气质量的基于表面的排放之后,气溶胶的吸湿性增加。

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