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中国喜马拉雅山和青藏高原三个偏远站点降水溶解有机碳(DOC)的沉降和光吸收特性。

Deposition and light absorption characteristics of precipitation dissolved organic carbon (DOC) at three remote stations in the Himalayas and Tibetan Plateau, China.

机构信息

Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China; Laboratory of Green Chemistry, Lappeenranta University of Technology, Sammonkatu 12, Mikkeli 50130, Finland; CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, China.

Laboratory of Green Chemistry, Lappeenranta University of Technology, Sammonkatu 12, Mikkeli 50130, Finland.

出版信息

Sci Total Environ. 2017 Dec 15;605-606:1039-1046. doi: 10.1016/j.scitotenv.2017.06.232. Epub 2017 Jul 10.

Abstract

The concentrations, depositions and optical properties of precipitation DOC at three remote stations (Nam Co, Lulang and Everest) were investigated in the Himalayas and Tibetan Plateau (HTP). The results showed that their volume-weighted mean DOC concentrations were 1.05±1.01mgCL, 0.83±0.85mgCL and 0.86±0.91mgCL, respectively, close to those of other remote areas in the world and lower than those of typical polluted urban cities. Combined with precipitation amounts, the DOC depositions at these three stations were calculated to be 0.34±0.32gCmyr, 0.84±0.86gCmyr and 0.16±0.17gCmyr, respectively. The annual DOC deposition in the HTP was approximately 0.94±0.87TgC, the highest and lowest values appeared in the southeastern and northwestern plateau, respectively. The sources of DOC in the precipitation at these three stations were remarkably different, indicating large spatial heterogeneity in the sources of precipitation DOC over the HTP. Nam Co presented combustion sources from South Asia and local residents, Lulang showed biomass combustion source from South Asia, and Everest was mainly influenced by local mineral dust. The values of the MAC at 365nm were 0.48±0.47mg, 0.25±0.15mg, and 0.64±0.49mg, respectively, for the precipitation at the three stations. All of these values were significantly lower than those of corresponding near-surface aerosol samples because precipitation DOC contains more secondary organic aerosol with low light absorption abilities. Additionally, this phenomenon was also observed in seriously polluted urban areas, implying it is universal in the atmosphere. Because precipitation DOC contains information for both particle-bound and gaseous components from the near surface up to the altitude of clouds where precipitation occurs, the MAC of precipitation is more representative than that of near-surface aerosols for a given region.

摘要

在喜马拉雅山和青藏高原(HTP)的三个偏远站点(纳木错、鲁朗和珠穆朗玛峰)研究了降水 DOC 的浓度、沉积和光学性质。结果表明,它们的体积加权平均 DOC 浓度分别为 1.05±1.01mgCL、0.83±0.85mgCL 和 0.86±0.91mgCL,接近世界其他偏远地区的浓度,低于典型污染城市的浓度。结合降水量,计算这三个站点的 DOC 沉积量分别为 0.34±0.32gCmyr、0.84±0.86gCmyr 和 0.16±0.17gCmyr。青藏高原的年 DOC 沉积量约为 0.94±0.87TgC,东南部和西北部高原的沉积量最高和最低。这三个站点降水 DOC 的来源明显不同,表明青藏高原降水 DOC 的来源具有很大的空间异质性。纳木错表现出南亚和当地居民的燃烧源,鲁朗表现出南亚生物质燃烧源,而珠穆朗玛峰主要受到当地矿物粉尘的影响。三个站点降水的 MAC 在 365nm 处的值分别为 0.48±0.47mg、0.25±0.15mg 和 0.64±0.49mg,均明显低于相应近地表气溶胶样品的值,因为降水 DOC 含有更多的具有低光吸收能力的二次有机气溶胶。此外,这种现象在污染严重的城市地区也有观察到,表明它在大气中是普遍存在的。由于降水 DOC 包含了从近地表到发生降水的云的高度的颗粒结合和气体成分的信息,因此对于给定区域,降水的 MAC 比近地表气溶胶更具代表性。

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