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交流风暴通过冷池和降水改变生物气溶群体
Teresa K Feldman1, Chamari B A Mampage1, Nicholas M Falk2
1Department of Chemistry, University of Iowa Iowa City IA 52242 USA betsy-stone@uiowa.edu.
概括
交流风暴显著增加空气中的真菌子和冰核颗粒 (INPs),对公众健康构成风险,并影响云层形成. 较强的冷池与较高的生物气溶度相关.
科学领域:
- 大气科学 大气科学
- 环境科学 环境科学
- 微生物学 微生物学
背景情况:
- 气象事件,如对流风暴,可以改变生物气溶的特性.
- 生物气溶影响公共卫生和云微物理.
- 生物气溶和对流风暴 (BACS) 研究调查了这些影响.
研究的目的:
- 检查对流风暴过程 (降水,冷池) 如何影响生物气溶的度和性质.
- 描述生物气溶,包括花粉,真菌子和细菌内毒素.
- 评估对冰核粒子 (INP) 度的影响.
主要方法:
- 在2022年5月至6月和2023年期间在北科罗拉多州进行了BACS研究.
- 利用在线 (光) 和离线 (化学标记物) 测量用于生物气溶的表征.
- 进行冰核化颗粒 (INP) 的同位测量.
主要成果:
- 降水事件增加了超微米光粒子度,主要是真菌子.
- 风暴产生的冷池产生了不同的影响,更强的池与更高的生物气溶度相关 (r = 0.79).
- 生物INP度 (1-10μm,> -15 °C) 在风暴期间增加一个数量级,与真菌子有关 (r = 0.91).
结论:
- 交流风暴显著增加了真菌子和温暖温度生物INP的边界层度.
- 增加的生物气溶对敏感人群构成高暴露风险.
- 这些生物气溶有可能影响云层过程.
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