基于海盐气溶胶通量观测的大液滴海雾生成函数

IF 3.8 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Xueling Cheng, Jiangbo Jin, Peng Fan, Run Guo, Yubin Ma, Jian Huang, Shouyin Zheng, Jiatian Chen, Hengchi Lei, Qingcun Zeng
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引用次数: 0

摘要

海洋微滴作为仅次于沙尘的最大天然气溶胶源,对气候变化、大气污染、台风等灾害天气产生重大影响。目前,由于观测资料的缺乏和对海气边界层湍流输运过程的认识不足,海雾雾滴的生成函数存在相当大的不确定性,特别是对于粒径大于20 μm的雾滴,大多数生成函数都低估了它们。利用自行研制的液滴光谱仪对海气边界层进行了多次液滴观测实验。得到了粒径为25μm ~ 1.6 mm的大液滴的浓度和上升速度。利用观测资料对海盐气溶胶(SSA)产生函数进行了分析,结果表明,大液滴的海盐气溶胶(SSA)通量远高于现有的海盐气溶胶产生函数,为海洋模式中计算SSA通量提供了一个新的大液滴生成函数。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Sea Spray Generation Function for Large Droplets Based on Sea Salt Aerosol Flux Observation

Marine droplets, as the largest natural aerosol source after sand and dust, can have a significant impact on climate change, air pollution, typhoons, and other disaster weather. At present, due to the lack of observational data and insufficient understanding of turbulent transport processes in the air-sea boundary layer, there is considerable uncertainty in the generation function of sea spray droplets, especially for droplets with a particle size greater than 20 μm, most of the generation functions underestimate them. The multiple experiments on observing droplets were conducted in the air-sea boundary layer using a self-developed droplet spectrometer. The concentration and upward velocity of large droplets with particle sizes ranging from 25μm to 1.6 mm were obtained. The sea spray generation function was analyzed using the observed data, and the results showed that the sea salt aerosol (SSA) flux of large droplets was much higher than that given by existing sea spray generation functions, providing a new generation function for large droplets in calculating SSA flux in ocean models.

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来源期刊
Journal of Geophysical Research: Atmospheres
Journal of Geophysical Research: Atmospheres Earth and Planetary Sciences-Geophysics
CiteScore
7.30
自引率
11.40%
发文量
684
期刊介绍: JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.
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