Sea spray characteristics: equilibrium radius, evaporation time, and flight duration

A reference table for sea spray characteristics in NetCDF format according to a miscrophysical model of Andreas et al. (2008, Journal. of Physical Oceanography), which was coded by Kosuke Ito (Feb 14, 2017) working at University of the Ryukyus. It contains the following items:<br>(1) equilibrium droplet radius (rad_eq)(2) droplet radius at the end of flight duration (rad_f)(3) e-folding timescale toward the equilibrium radius (tau_r)(4) e-folding timescale toward the equilibrium volume (tau_v)(4) flight duration (tau_f)<br>These values are assumed to be a function of pressure, atmospheric pressure, relative humidity, ocean temperature, and 10-m height wind, supposed that the sea surface salinity is 34 psu and the initial droplet radius is 50.0 x 10^-6 m. Note that the values for the wind speed over 40 m s^-1 are highly uncertain.

本数据集为遵循Andreas等人（2008年发表于《物理海洋学杂志》）的微物理模型所构建的海表飞沫特性参考表，格式为NetCDF，由琉球大学的伊藤宏介（Kosuke Ito）于2017年2月14日编写。数据集包含以下内容：
(1) 平衡液滴半径（rad_eq）
(2) 飞行时长结束时的液滴半径（rad_f）
(3) 趋近平衡半径的e折叠时间尺度（tau_r）
(4) 趋近平衡体积的e折叠时间尺度（tau_v）
(5) 飞行时长（tau_f）
上述参数均以气压、大气压强、相对湿度、海洋温度以及10米高度风速为自变量，预设海表盐度为34 psu，初始液滴半径为50.0×10⁻⁶ 米。需注意，风速超过40 m·s⁻¹ 时的计算结果存在较高不确定性。