Kattawar G W, Humphreys T J
Appl Opt. 1976 Jan 1;15(1):273-82. doi: 10.1364/AO.15.000273.
A Monte Carlo program was written to compute the effect of chlorophyll on the ratio of upwelling to down-welling radiance and irradiance as a function of wavelength, height above the ocean, and depth within the ocean. This program simulates the actual physical situation, since a real atmospheric model was used, i.e., one that contained both aerosol and Rayleigh scattering as well as ozone absorption. The complete interaction of the radiation field with the ocean was also taken into account. The chlorophyll was assumed to be uniformly mixed in the ocean and was also assumed to act only as an absorbing agent. For the ocean model both scattering and absorption by hydrosols was included. Results have been obtained for both a very clear ocean and a medium turbid ocean. Recommendations are made for optimum techniques for remotely sensing chlorophyll both in situ and in vitro.
编写了一个蒙特卡罗程序，用于计算叶绿素对向上和向下辐射率及辐照度之比的影响，该影响是波长、海洋上方高度和海洋深度的函数。该程序模拟了实际物理情况，因为使用了真实的大气模型，即一个包含气溶胶、瑞利散射以及臭氧吸收的模型。还考虑了辐射场与海洋的完整相互作用。假设叶绿素在海洋中均匀混合，并且仅作为吸收剂起作用。对于海洋模型，包括了水溶胶的散射和吸收。已经获得了非常清澈海洋和中等浑浊海洋的结果。针对原位和体外遥感叶绿素的最佳技术提出了建议。
