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A parameterization of sea-salt aerosol source function for sub- and super-micron particles

机译:亚微米和超微米颗粒的海盐气溶胶源函数参数化

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摘要

[1] A parameterization of a sea-salt source function for both sub- and super-micron particles was developed based on the semi-empirical formulation of Monahan et al. [1986]. This new parameterization extends the range of Monahan's equation to below 0.2 μm in diameter where it has been found to overestimate submicron sea-salt aerosols, especially the sea-salt number concentrations. The new parameterization was used in a one-dimensional (1-D) column model to predict the number size distributions and compared with reasonable agreement to the observed distributions at various wind speeds reported by O'Dowd et al. [1997]. A global 3-D sea-salt simulation with this parameterization was also made and a much better dependence of sea-salt on surface wind speed was predicted than other schemes compared to observations. For an indirect impact assessment of sea-salt aerosols on climate where submicron particles may have a dominant contribution to aerosol-cloud interactions, this scheme provides the most realistic number flux of sea-salt particles between ocean and atmosphere.
机译:[1]基于Monahan等人的半经验公式,开发了针对亚微米和超微米颗粒的海盐源函数的参数化方法。 [1986]。这种新的参数化将Monahan方程的范围扩展到了直径小于0.2μm的直径,从而发现它高估了亚微米海盐气溶胶,特别是海盐数量浓度。新的参数化用于一维(1-D)列模型中,以预测数值大小分布,并与O'Dowd等人报道的在各种风速下观察到的分布进行合理的比较。 [1997]。还进行了具有此参数化的全局3-D海盐模拟,与其他方案相比,与观测值相比,海盐对地表风速的依赖性要好得多。对于海盐气溶胶对气候的间接影响评估(亚微米颗粒可能对气溶胶-云相互作用起主要作用),该方案提供了最现实的海盐颗粒在海洋和大气之间的通量。

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