Concentrations and size-distributions of water-soluble inorganic and organic species on aerosols over the Arctic Ocean observed during the US GEOTRACES Western Arctic Cruise GN01

被引:2
|
作者
Mukherjee, Pami [1 ,5 ]
Marsay, Christopher M. [2 ]
Yu, Shun [3 ]
Buck, Clifton S. [2 ]
Landing, William M. [4 ]
Gao, Yuan [1 ]
机构
[1] Rutgers State Univ, Dept Earth & Environm Sci, Newark, NJ 07102 USA
[2] Univ Georgia, Skidaway Inst Oceanog, Savannah, GA USA
[3] Rutgers State Univ, Dept Marine & Coastal Sci, New Brunswick, NJ USA
[4] Florida State Univ, Dept Earth Ocean & Atmospher Sci, Tallahassee, FL 32306 USA
[5] South Coast Air Qual Management Dist, Diamond Bar, CA USA
基金
美国国家科学基金会;
关键词
Arctic summer aerosols; Water-soluble organic aerosols; Fine mode MSA and Non-sea-salt-sulfate; CLOUD-CONDENSATION-NUCLEI; MARINE BOUNDARY-LAYER; SEA-SALT AEROSOL; BIOGENIC SULFUR AEROSOL; CHEMICAL-COMPOSITION; DIMETHYL SULFIDE; ATMOSPHERIC AEROSOL; DICARBOXYLIC-ACIDS; PARTICLE FORMATION; METHANESULFONIC-ACID;
D O I
10.1016/j.atmosenv.2021.118569
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Marine aerosols affect the climate directly and indirectly as well as serving as tracers of biogenic processes. Here we present the results from size-segregated and bulk aerosol samples collected from 2nd August to 10th October 2015 during the US GEOTRACES Arctic Ocean (GN01) expedition. Samples were analyzed for concentrations of major water-soluble organic and inorganic species, including acetate, formate, methanesulfonate (MSA), oxalate, propionate, chloride, nitrate, sulfate and major cations (Na+, K+, Mg2+, Ca2+, NH4+). Back-trajectory analysis was performed to categorize the wind patterns into three types; type 1, originating from the North Pacific and the Bering Sea, type-2, consisting entirely of marine Arctic air, and type 3, consisting of marine Arctic air mixed with air masses from the surrounding continents. Sea-salt was the major aerosol component, dominating in the coarse mode, 1.8-5.6 mu m. Non-sea-salt sulfate and MSA were predominantly present in the fine mode, 0.18-0.32 mu m, and MSA was associated with type 1 and type 2 air masses. The results from this study provide useful information on the origins and chemical processes involving these aerosol species over the Arctic in summer and help elucidate the significance of natural sources as contributors for the formation of cloud condensation nuclei.
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页数:15
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