An analysis of the surface production of sea-salt aerosols By C. W. FAIRALL, BDM Corporation, Naval Postgraduate School, Monterey, California 93940, U.S.A.
An analysis of the surface production of sea-salt aerosols By C. W. FAIRALL, BDM Corporation, Naval Postgraduate School, Monterey, California 93940, U.S.A.
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海盐气溶胶表面产生的分析作者：C. W. FAIRALL，BDM Corporation，海军研究生院，蒙特雷，加利福尼亚州 93940，美国
DOI：
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发表时间：
1983
期刊：
影响因子：
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通讯作者：
G. Schacher
中科院分区：
文献类型：
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作者：
K. Davidson;G. Schacher
在海洋表面，气泡破裂产生海水液滴的速度很难直接测量。实验室模拟也很困难。然而，表面通量可以从气溶胶密度变化率和海洋边界层高度变化的测量值中推断出来。本文分析了CEWCOM-78的资料，得到了9 m/s风速下0.8 ~ 15 pm半径范围内的气溶胶表面通量体积谱。使用JASIN的通量谱和平衡气溶胶谱。计算了风速从6到18 m s-1时的通量谱。
The rate of production of sea water droplets by bubble bursting at the ocean surface is very difficult to measure directly. Laboratory simulations are also difficult. However, the surface flux can be inferred from measuremerits of the rate of change of aerosol densities and changes in the height of the marine boundary layer. Data from CEWCOM-78 have been analyzed to produce the aerosol surface flux volume spectrum from 0.8 to 15 pm radius at a wind speed of 9 m s-’. Using this flux spectrum and equilibrium aerosol spectra from JASIN. flux spectra are calculated for wind speeds from 6 to 18 m s-’.