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FLEXPART?v10.1 simulation of source contributions to Arctic black carbon

机译:Flexpart?v10.1源对北极黑碳的源贡献模拟

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The Arctic environment is undergoing rapid changes such as faster warming than the global average and exceptional melting of glaciers in Greenland. Black carbon?(BC) particles, which are a short-lived climate pollutant, are one cause of Arctic warming and glacier melting. However, the sources of BC?particles are still uncertain. We simulated the potential emission sensitivity of atmospheric?BC present over the Arctic (north of 66°N) using the FLEXPART (FLEXible PARTicle) Lagrangian transport model (version?10.1). This version includes a new aerosol wet removal scheme, which better represents particle-scavenging processes than older versions did. Arctic BC at the surface (0–500m) and high altitudes (4750–5250m) is sensitive to emissions in high latitude (north of 60°N) and mid-latitude (30–60°N) regions, respectively. Geospatial sources of Arctic?BC were quantified, with a focus on emissions from anthropogenic activities (including domestic biofuel burning) and open biomass burning (including agricultural burning in the open field) in?2010. We found that anthropogenic sources contributed 82% and 83% of annual Arctic?BC at the surface and high altitudes, respectively. Arctic surface?BC comes predominantly from anthropogenic emissions in Russia (56%), with gas flaring from the Yamalo-Nenets Autonomous Okrug and Komi Republic being the main source (31% of Arctic surface?BC). These results highlight the need for regulations to control BC?emissions from gas flaring to mitigate the rapid changes in the Arctic environment. In summer, combined open biomass burning in Siberia, Alaska, and Canada contributes 56%–85% (75% on average) and 40%–72% (57%) of Arctic BC at the surface and high altitudes, respectively. A large fraction (40%) of?BC in the Arctic at high altitudes comes from anthropogenic emissions in East Asia, which suggests that the rapidly growing economies of developing countries could have a non-negligible effect on the Arctic. To our knowledge, this is the first year-round evaluation of Arctic?BC sources that has been performed using the new wet deposition scheme in FLEXPART. The study provides a scientific basis for actions to mitigate the rapidly changing Arctic environment.
机译:北极环境正在进行快速变化,例如更快的变暖,比格陵兰岛冰川的全球平均水平和特殊融化更快。黑碳?(BC)颗粒是一种短暂的气候污染物,是北极变暖和冰川熔化的一个原因。然而,BC的来源仍然不确定。我们使用Flexpart(柔性粒子)拉格朗日传输模型(版本?10.1)模拟了大气(北距离66°N的北部)的潜在发射敏感性。该版本包括一种新的气溶胶湿式拆除方案,它更好地代表粒子清除的过程,而不是旧版本。表面(0-500M)和高海拔(4750-5250M)的北极BC对高纬度(60°N北部)和中纬度(30-60°N)区域的排放敏感。北极地理空间来源?BC量化,重点关注人为活动(包括国内生物燃烧)和开放生物量燃烧(包括开放领域的农业燃烧)的排放。我们发现人为的来源分别在表面和高海拔地区占年度北极的82%和83%。北极表面?BC来自主要来自人为排放,在俄罗斯(56%),与气体从亚马尔 - 涅涅茨自治区和科米共和国扩口是主要源(北极表面的31%?BC)。这些结果突出了对BC控制BC的规则的需要,来自燃气燃烧的排放,以减轻北极环境的快速变化。在夏季,组合的开生物质燃烧在西伯利亚,阿拉斯加,和分别加拿大有助于北极BC的56%-85%(平均75%)和40%-72%(57%)在表面处和高海拔。高海拔地区北极的大部分(40%)的BC来自东亚的人为排放,这表明发展中国家的快速增长经济体可能对北极产生不可忽略的影响。据我们所知,这是北极的第一期评估,这是使用Flexpart中的新湿沉积方案进行的。该研究为减轻了快速变化的北极环境的行动提供了科学依据。

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