Su Wenying, Charlock Thomas P, Rutledge Ken
Center for Atmospheric Sciences, Hampton University, Hampton, Virginia 23668, USA.
Appl Opt. 2002 Dec 10;41(35):7369-83. doi: 10.1364/ao.41.007369.
A scanning spectral photometer is deployed on a rigid coastal ocean platform to measure upwelling solar radiances from the sea surface at nine elevation angles spanning 150 degrees of azimuth. Measured radiance distributions at 500 nm wavelength have been compared with traditional model simulations employing the Cox and Munk distribution of wave slopes. The model captures the general features of the observed angular reflectance distributions, but: (a) the observed peak value of sunglint near the specular direction is larger than simulated, except for a very calm sea; the model-measurement differences increase with wind speed and are largest for low solar elevation; (b) the observed sunglint is wider than simulated. In contrast to some previous studies, our results do not show a clear dependence of the mean square sea-surface slope on stability (air-sea temperature difference).
一台扫描光谱光度计部署在一个坚固的沿海海洋平台上,用于测量在跨越150度方位角的九个仰角下从海面向上的太阳辐射亮度。已将在500纳米波长处测得的辐射亮度分布与采用Cox和Munk波斜率分布的传统模型模拟结果进行了比较。该模型捕捉到了观测到的角反射率分布的一般特征,但是:(a)除了海面非常平静的情况外,在镜面方向附近观测到的镜面反射峰值大于模拟值;模型与测量值的差异随风速增加,并且在太阳高度较低时最大;(b)观测到的镜面反射比模拟的更宽。与之前的一些研究不同,我们的结果并未显示出海面均方斜率对稳定性(海气温差)有明显的依赖性。