日本EANET站点高浓度降水样本频率的时间和季节变化:20年的日湿沉降数据

IF 1.8 Q4 METEOROLOGY & ATMOSPHERIC SCIENCES
Yuhei Kato, Tsuyoshi Ohizumi, Makoto Nakata, Hiroyuki Sase
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引用次数: 0

摘要

近几十年来,东北亚地区的大气环境发生了动态变化。东亚酸沉降监测网(EANET)通过在许多站点的日常采样,积累了湿沉降监测数据。每日降水样本比每隔较长时间(如每隔一周或每隔两周)收集的样本更能动态地反映空气污染物浓度。在日本10个EANET站点2000 - 2019年20年间积累的日降水数据中,我们选择了非海盐成分在前2%范围内的高浓度数据,分别是H⁺、NH₄⁺、nss-Ca2⁺、NO₃⁻和nss-SO₄2⁻。约67%的高浓度数据发生在2005 - 2014年。此后,近年来高度集中的数据点数量有限。大部分高浓度数据集中在春季(3 - 5月,约占50%)和冬季(12 - 2月,约占31%)。这些结果与中国大陆的空气污染状况部分一致,高浓度现象被认为是受跨境空气污染的影响。对冬春季节浓度数据最高的样品进行的轨迹分析证实,在大多数情况下,来自大陆的气团被输送到每个站点。样品中共存的高浓度成分的季节差异表明,由于大陆春季沙尘暴的输送,从冬季到春季,SO₄2⁻和NO3⁻的反离子从H+变成了Ca2+。因此,日高浓度数据动态地反映了该地区的气团流动情况。图形抽象
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Temporal and seasonal variations in the frequency of high-concentration precipitation samples at EANET sites in Japan: 20 years of daily wet deposition data

Over the past decades, the atmospheric environment in Northeast Asia has changed dynamically. The Acid Deposition Monitoring Network in East Asia (EANET) has accumulated wet deposition monitoring data through daily sampling at many sites. Daily precipitation samples may reflect air pollutant concentrations more dynamically than samples collected at longer intervals, such as weekly or biweekly. Among daily precipitation data accumulated over the 20 years from 2000 to 2019 at the 10 EANET sites in Japan, we selected high-concentration data within the top 2% range for non-sea salt components, namely H⁺, NH₄⁺, nss-Ca2⁺, NO₃⁻, and nss-SO₄2⁻, respectively. Approximately 67% of the high-concentration data were from 2005 to 2014. Thereafter, the number of high-concentration data points was limited in recent years. Most of the high-concentration data were obtained in spring (March–May; approximately 50%) and winter (December–February; approximately 31%). These results are partially consistent with the air pollution conditions in mainland China, and the high concentration phenomenon is thought to be influenced by transboundary air pollution. Trajectory analysis performed on the samples with the highest concentration data in the winter-spring season confirmed that, in most cases, air masses from the continent were transported to each site. The seasonal differences in the coexisting high-concentration components in the samples suggested that counterions of SO₄2⁻ and NO3⁻ were changed from H+ to Ca2+ from winter to spring due to the transport of spring dust storm from the continent. Thus, the daily high-concentration data dynamically reflected the air mass flow in the region.

Graphical Abstract

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来源期刊
Asian Journal of Atmospheric Environment
Asian Journal of Atmospheric Environment METEOROLOGY & ATMOSPHERIC SCIENCES-
CiteScore
2.80
自引率
6.70%
发文量
22
审稿时长
21 weeks
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