水同位素比率D/H,18O/16O,17O/16O在云层内外映射脱水路径
Christopher R Webster1, Andrew J Heymsfield
1Earth and Space Sciences Division, Jet Propulsion Laboratory (JPL), California Institute of Technology, Pasadena, CA 91109, USA. chris.r.webster@jpl.nasa.gov
概括
对状云的同位素分析显示,在上层热带层有显著的水蒸气枯竭. 这表明各种脱水过程,冰颗粒在水运输中发挥着关键作用.
科学领域:
- 大气科学 大气科学
- 云物理 云物理
- 同位素地球化学 同位素地球化学
背景情况:
- 圆柱状云对地球的辐射平衡和水循环至关重要.
- 了解高层热带层的水蒸气同位素组成对于气候建模至关重要.
- 之前的研究对亚热带云中同位素比率的数据有限.
研究的目的:
- 为了测量水同位素的比率进出亚热带云.
- 为了研究上层热层水蒸气的起源和脱水机制.
- 为了区分现场形成的冰颗粒和从较低海拔上升的冰颗粒.
主要方法:
- 激光吸收光谱法用于测量水同位素比率.
- 现场测量是在状云中进行的.
- 分析的重点是水蒸气和冰颗粒同位素特征.
主要成果:
- 在热带和亚热带上层热带层水蒸气中观察到广泛的,以前未记录的同位素耗尽范围.
- 确定了对流和逐渐脱水的机制,导致这种枯竭.
- 确定25%的上层热带层水样本是冰颗粒,具有明显的同位素特征,表明形成过程.
结论:
- 亚热带上层热带层的水蒸气通过多个途径经历了显著的脱水.
- 雪花云中的冰颗粒是大气水运输和处理的重要标记物.
- 同位素分析提供了对云形成和水循环在上层热带层的关键见解.
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