染料3气体和气溶胶取样计划期间影响南格陵兰冰盖的源区轨迹分析

Cliff I Davidson , Jean-Luc Jaffrezo , Mitchell J Small , Peter W Summers , Marvin P Olson , Randy D Borys
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引用次数: 54

摘要

格陵兰岛Dye 3(海拔2.5 km)的向后气团轨迹显示了不同季节的气源区域:最大输送距离的方向是秋季从西南方向,冬季从西方向,春季从西北方向;夏季的轨迹没有显示出强烈的偏好方向。基于5天的过境时间,秋季的轨迹表明北美作为潜在的来源区域的重要性,偶尔来自西欧的轨迹。春季,特别是4月份的轨迹表明欧亚大陆(极地上空的运输)、北美东部和西欧是潜在的来源区域。在夏季,当运输距离较短时,预计化学成分向染料3的运输较少。虽然一些到格陵兰岛的长途运输发生在冬季,但每年这个时候冰盖上大气的稳定性可能会限制化学成分向地表的输送。如果考虑到凌日时间超过5天,这些区域以外的来源也会影响染料3。这些结果与其他报告的海平面北极地区的轨迹相反,如阿拉斯加的巴罗和加拿大的莫德湾,在这些地区,来自欧亚大陆的极地运输是冬季和早春大部分时间化学物质浓度高的原因。总体而言,轨迹与几位研究人员报告的3号染区这段时间的气溶胶化学数据一致,显示春季和秋季浓度达到峰值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Trajectory analysis of source regions influencing the south Greenland Ice Sheet during the Dye 3 Gas and Aerosol Sampling Program

Backward air mass trajectories for Dye 3, Greenland (elevation 2.5 km) show source regions that vary with season: the direction of greatest transport distance is from the southwest in fall, west in winter, and northwest in spring; the trajectories in summer do not show a strong preferred direction. Based on 5 d transit times, the trajectories in fall suggest the importance of North America as a potential source region, with occasional trajectories from western Europe. The trajectories in spring, especially in April, suggest Eurasia (transport over the Pole), eastern North America, and Western Europe as potential source regions. Less transport of chemical constituents to Dye 3 is expected in summer when transport distances are shorter. Although some long-range transport to Greenland occurs in winter, the stability of the atmosphere over the ice sheet at this time of year is likely to limit the delivery of chemical constituents to the surface. Sources outside of these regions can also influence Dye 3 if transit times longer than 5 d are considered. These results are in contrast to trajectories reported by others for sea-level arctic locations such as Barrow, Alaska and Mould Bay, Canada, where transport over the Pole from Eurasia is responsible for high chemical species concentrations over much of the winter and early spring. Overall, the trajectories are consistent with aerosol chemical data for this time period at Dye 3 reported by several investigators, showing peak concentrations in spring and fall.

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