Open AccessCharacteristics of Aerosol WSI With High‐Time‐Resolution Observation Over Arctic Ocean
Author(s) -
Yu Congcong,
Yan Jinpei,
Zhang Honghai,
Lin Qi,
Zheng Hongguo,
Zhong Xinlin,
Zhao Suli,
Zhang Miming,
Zhao Shuhui,
Li Xiaojun
Publication year - 2020
Publication title -
earth and space science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.843
H-Index - 23
ISSN - 2333-5084
DOI - 10.1029/2020ea001227
Subject(s) - aerosol , methanesulfonic acid , arctic , environmental science , sea salt , the arctic , atmospheric sciences , oceanography , climatology , environmental chemistry , meteorology , chemistry , geology , geography , organic chemistry
Abstract In the current study, the characteristics of aerosol water‐soluble ions (WSI) were investigated via high‐time‐resolution observations as part of the nineth Chinese National Arctic Research Expedition (CHINARE) in 2018. WSI, including Cl − , SO 4 2− , NO 3 − , NO 2 − , F − , Br − , Na + , NH 4 + , K + , Ca 2+ , Mg 2+ , and Methanesulfonic acid (MSA − ), were measured using an online ion chromatography system deployed on the Xuelong research vessel. Moreover, aerosol particle sources were analyzed in order to clarify the impacts of marine emissions and anthropogenic sources on atmospheric aerosols in the Arctic Ocean. Sea salt ions (Na + and Cl − ) were observed to be the most dominant compounds, accounting for 53.5% of the total WSI, followed by the secondary ions (SO 4 2− , NH 4 + , and NO 3 − ), which accounted for 36.0%. Furthermore, similar spatial distributions of MSA − and SO 4 2− were observed during the measurement period. High levels of Na + were observed in the areas close to the land and Central Arctic Ocean, attributed to wind speed. In the open ocean, NH 4 + and NO 3 − concentrations were extremely low, however, high levels of NH 4 + and NO 3 − were observed in the coastal area close to Alaska and Russia. This indicates that these aerosol particles were influenced by the anthropogenic sources in these regions. In addition, mean fluxes of NO 3 − and NH 4 + were determined as 42 ± 41 and 347 ± 166 μg m −2 day −1 in the Arctic Ocean, respectively.