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Whitecaps: spectral reflectance in the open ocean and their contribution to water-leaving radiance

机译:白帽:公海中的光谱反射率及其对离水辐射的贡献

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Abstract: The reflectance of white caps in the open ocean is obtained with a 6-channel spectral radiometer, extended from the bow of a ship, at wavelengths; 410, 440, 510, 670 and 860 nm. In addition to reflectance data, air/water temperature, wind speed and direction are obtained as well as GPS information in order to characterize ocean surface conditions. A visual reference for sea surface conditions measured by the radiometer is recorded using a video camera mounted beside the radiometer. By measuring a small area of the water surface over time, the presence and spectral influence of whitecaps can be quantified.Using this technique the spectral reflectance of individual whitecaps can be measured and tracked through their complete life cycle. Also, integration over a larger time series of ocean surface reflectance data provides a measurement of the augmented or extra contribution from white water reflectance to the water leaving radiance observed by ocean color satellites. Estimates of the augmented reflectance are subsequently correlated to sea surface state, and include the frequency of occurrence and spectral contribution from various levels of white water reflectance as whitecaps grow and decay. !18
机译:摘要:使用从船首延伸的六通道光谱辐射计在一定波长下获得的白帽在远洋中的反射率; 410、440、510、670和860 nm。除反射率数据外,还获得空气/水温,风速和风向以及GPS信息,以表征海洋表面状况。使用安装在辐射计旁边的摄像机记录由辐射计测得的海面状况的视觉参考。通过测量随时间变化的一小部分水面,可以量化白帽的存在和光谱影响。使用此技术,可以测量并跟踪整个白帽的整个生命周期中的光谱反射率。而且,在更大的时间序列的海洋表面反射率数据上的积分提供了白水反射率对海洋彩色卫星所观察到的离开水面辐射率的增加或额外贡献的度量。增强反射率的估计值随后与海表状态相关,并包括白帽生长和衰减时白水反射率不同级别的出现频率和光谱贡献。 !18

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