在洪加通加风云中,气溶形成的速度出乎意料
Elizabeth Asher1,2, Michael Todt1,2, Karen Rosenlof2
1Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO 80309.
概括
2022年洪加通加-洪加哈帕伊火山爆发将大量的二氧化硫 (SO2) 和水蒸气 (H2O) 注入平流层. 这导致了硫酸气溶的快速形成,并观察到大颗粒.
科学领域:
- 大气中的化学成分
- 火山学 火山学是一门学科.
- 石流层科学是一门科学.
背景情况:
- 2022年1月的Hunga Tonga-Hunga Ha'apai (HT-HH) 喷发产生了前所未有的平流层气溶光学深度的火山羽毛.
- 之前的火山事件,比如山. 皮纳图博,为评估平流层影响提供基准.
研究的目的:
- 描述HT-HH火山羽毛的组成和演变.
- 量化二氧化硫 (SO2) 和水蒸气 (H2O) 进入平流层的数量.
- 了解平流层气溶喷发后的形成路径和特征.
主要方法:
- 使用气球载载仪器从里昂尼翁岛发射,从喷发后7-10天取样HT-HH烟雾.
- 测量了气溶数量和尺寸分布,以及SO2和H2O度.
- 分析数据以确定羽毛的组成,注射高度和气溶形成率.
主要成果:
- 在火山羽毛中观察到意想不到的大量的大颗粒.
- 将总硫注入量限制在大约0.2 Tg.
- 确定硫酸气溶的形成在3周内完成.
- 确定了显著的H2O增强,为气溶表面积贡献了30%左右,并加速了SO2氧化.
结论:
- 在HT-HH喷发中,大量的SO2和H2O被注入了平流层.
- 高度的H2O显著影响了SO2氧化和气溶的形成,与平常的平流层条件相比,其速度翻了三倍.
- 气溶的快速形成和大颗粒的存在对平流层化学和动态有影响.
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