生物冰核子在降雪中的普遍存在
Brent C Christner1, Cindy E Morris, Christine M Foreman
1Department of Biological Sciences, Louisiana State University, Baton Rouge, LA 70803, USA. xner@lsu.edu
概括
包括细菌在内的生物颗粒是降雪中发现的高度活跃的冰核子 (IN) 的主要来源. 这些发现表明,生物圈显著影响大气过程和降水.
科学领域:
- 大气科学 大气科学
- 微生物学 微生物学
- 环境科学 环境科学
背景情况:
- 冰核子 (IN) 对于降水形成至关重要.
- IN的起源和分布在很大程度上是未知的.
- 了解IN来源对于大气和气候研究至关重要.
研究的目的:
- 为了确定在降雪中高度活跃的冰核子 (IN) 的来源.
- 为了确定在更高温度下活跃的IN的特性.
- 评估生物颗粒作为IN的作用.
主要方法:
- 收集了来自中高度地区的降雪样本.
- 分析了IN属性,包括大小和温度依赖的活动.
- 利用显微镜和其他技术来识别粒子组成.
主要成果:
- 在降雪中最活跃的IN主要是生物的.
- 69-100%的IN大于0.2微米,在-7°C以上活跃,是生物的.
- 细菌构成了这些生物IN的很大一部分.
结论:
- 生物圈是高活性IN的主要来源.
- 生物IN,特别是细菌,在大气过程中起着重要作用.
- 这些发现表明,生物颗粒可以影响降雨模式和自身的运输.
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