云碎片对夜间过程驱动的气溶的反应
Geoffrey Pugsley1, Edward Gryspeerdt1, Vishnu Nair1
1Department of Physics, Imperial College London, London, SW7 2BX, United Kingdom.
概括
夜间的过程对层积云部分的气溶影响很大,而白天的过程的影响较小. 气溶白天使云层变薄,但夜间的过程部分抵消了这一点,影响了气候强迫评估.
科学领域:
- 大气科学 大气科学
- 气候科学 气候科学
- 云物理 云物理
背景情况:
- 气溶与云的相互作用是气候强迫的主要不确定性来源.
- 对于气候至关重要的石云受到白天周期的影响,但研究往往忽略了夜间的行为.
- 了解气溶对云碎片和液态水路的影响对于气候建模至关重要.
研究的目的:
- 为了研究云层云中对气溶的云敏感度的日间变化.
- 区分夜间和白天过程在气溶云相互作用中的作用.
- 通过纳入对气溶对云的影响更准确的表示来改进气候模型.
主要方法:
- 利用拉格朗的框架来分析云特性的昼夜变化.
- 描述了云碎片和液态水路对气溶的敏感性.
- 与模型观察数据进行比较,重点关注白天周期表示.
主要成果:
- 云碎片对气溶的反应主要是由夜间过程驱动的.
- 气溶减少白天云的分数,这一效应被夜间过程部分抵消.
- 气溶诱导的降水抑制在夜间是最有效的,与最强的平流体积降水相吻合.
结论:
- 夜间的过程对于确定平流体云的白天演变及其辐射影响至关重要.
- 准确的日间周期表现和夜间观测对于气候强迫评估至关重要.
- 通过突出夜间云动态的重要性,研究结果揭示了海洋云亮化策略的可行性.
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