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Reply to comment on 'Size distribution of sea-salt emissions as a function of relative humidity'

机译:关于“海盐排放量的大小分布与相对湿度的函数”的评论答复

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We appreciate the insightful comments provided by Lewis and Schwartz (2005). We became aware of their parameterization of sea-salt's size dependence on relative humidity (Lewis and Schwartz, 2004) only after our original manuscript was in press and agree that Eq. (4) of Lewis and Schwartz (2005) is an improvement over the expression for the size-correction factor (C_0, defined as the ratio of sea-salt particle diameter at formation to that at ambient relative humidity, RH) in Zhang et al. (2005) due to its physical basis rather than derivation from a polynomial fit to laboratory data. Although both parameterizations are useful for general atmospheric modeling applications, the Lewis and Schwartz parameterization can be applied not only to typical ocean environments, but also to the few locations where salinity departs significantly from 35 per thousand, and is more accurate at times and locations where the ambient RH exceeds 98%.
机译:我们感谢Lewis和Schwartz(2005)提供的有见地的评论。只有在我们的原始手稿付印后,我们才意识到他们对海盐大小依赖于相对湿度的参数化(Lewis和Schwartz,2004)。 Lewis et al。(4)(2005)是Zhang等人对尺寸校正因子(C_0,定义为地层中海盐粒径与环境相对湿度RH之比)的表达的改进。 。 (2005年)由于其物理基础,而不是从多项式拟合得出实验室数据。尽管这两种参数化都可用于一般的大气建模应用,但Lewis和Schwartz的参数化不仅可以应用于典型的海洋环境,而且还可以应用于盐度明显偏离千分之35的少数位置,并且在某些时间和位置更准确环境相对湿度超过98%。

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