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Characterization of particulate matter and black carbon over Bay of Bengal during summer monsoon: results from the OMM cruise experiment

机译:夏季孟加拉湾常春藤常见物质和黑碳的表征:OMM巡航实验的结果

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Total and size-segregated particulate matter (PM) and black carbon (BC) concentrations over the Bay of Bengal (BoB) have been measured in the summer monsoon (August–September 2014) onboard a scientific cruise conducted as a part of the Ocean Monsoon and Mixing (OMM) experiment. Role of long-range transport and prevailing meteorology in producing the observed spatio-temporal features is inferred by synthesizing the results of in situ observations in conjunction with the wind components from Modern Era Retrospective Analysis for Research and Applications (MERRA), rainfall data from Tropical Rainfall Measuring Mission (TRMM), surface BC concentration and BC Aerosol Optical Thickness (AOT~(BC)) from MERRA2 and HYSPLIT back trajectory and dispersion model analysis. Mean values of total PM and BC mass concentrations are observed to be ~?21.4?μgm_(?3)and ~?393ngm_(?3)respectively. The study has revealed significant influence of monsoon rainfall (over the measurement locations and regions through which transport occurred) on the concentration of both PM and BC over northern BoB. Results also indicate transport of aerosols with significant anthropogenic fraction, from the land regions at west to the BoB. A comprehensive analysis showed that while an eastward wind (westerly) from the Indian mainland produced an increase in PM~(2.5)over northern BoB, a southerly wind, mostly from the Indian Ocean, caused a decrease in concentration of PM~(2.5). Spectral variation of absorption coefficients of aerosols reveals that most of the BC over BoB is associated with fossil fuel combustion. Prevailing strong surface-level convergence (associated with a low-level anticyclone) resulted in accumulation and consequent enhancement of aerosol concentration over central and northern BoB during the study period. In addition, horizontal flow rates estimated across western boundary of BoB using AOT~(BC)from MERRA2 for 10?years revealed an increasing trend in BC transport from the mainland leading to a gradual buildup in BC concentration over the regions of BoB.
机译:道达尔和尺寸分离颗粒物(PM)和黑碳(BC)在孟加拉湾(BOB)的浓度在夏季风(8月2014年9月)进行了测量船上的海洋季风的一部分进行了科学巡航和混合(OMM)实验。生产所观察到的时空特征长距离运输的作用及现行气象学通过与来自现代时代回顾性分析风力组件研究与应用(MERRA),从热带降雨量数据合成的实地观测结果一起推断降雨测量使命(TRMM),表面BC的浓度和从MERRA2 BC气溶胶光学厚度(AOT〜(BC))和背HYSPLIT轨迹和扩散模型分析。总PM和BC质量浓度的平均值被观察到〜?21.4?μgm_(?3)和〜?393ngm _分别(θ3)。该研究揭示了季风降水(在测量位置和地区通过发生运输)在PM和BC两个在BOB的北部浓度显著的影响。结果还表明有显著人为气溶胶部分运输,从土地的区域在西鲍勃。综合分析表明,尽管向东风(西风)从印度大陆产于下午〜(2.5)在BOB的北部,一个偏南风,其中大部分来自印度洋的增加,导致下午〜浓度的降低(2.5) 。气溶胶吸收系数的光谱变化表明,大多数BC超过鲍勃与化石燃料燃烧有关。盛行强的表面级收敛(具有低级别反气旋相关联)导致的积累和在中部和北部BOB的气溶胶浓度随之增强在研究期间。此外,水平流率的全面使用AOT〜(BC)从MERRA2 10鲍勃西界估计?年发现于公元前运输增加的趋势从大陆导致BC浓度超过鲍勃区域逐渐积聚。

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