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Optical remote sensing of waters with vertical structure

机译:垂直结构水域的光学遥感

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摘要

Optical remote sensing of ocean color is a well-established technique that is used to produce maps of marine constituents on a routine basis. Retrieval algorithms used to infer pigment concentrations from measurements of ocean color are usually based on the assumption that the upper ocean column is vertically homogeneous. However, stable stratification of the water column is often encountered in coastal waters and in fjords. This stratification is decisive for the initiation, maintainance, and species composition of phytoplankton blooms. Here we present an optical remote-sensing algorithm with the ability to resolve such a vertical structure of oceanic waters. The vertical structure is assumed to consist of two homogeneous layers with different concentrations of chlorophyll a. The algorithm is designed to determine the chlorophyll-a concentrations of the two layers as well as the thickness of the upper layer. These three parameters influence the ocean color and are simultaneously retrieved through an inverse-modeling technique. This technique consists of using radiative-transfer computations for a coupled atmosphere-ocean system to simulate radiances received in various bands of the satellite sensor and to compare these simulated results with measured radiances. The sum of absolute values of differences between simulated and measured radiances is minimized by use of an optimization algorithm, and the retrieved parameters are those that yield the minimum sum of differences between measured and simulated data. The optimization algorithm that we used in our study is the simulated annealing method, which is an extension of the downhill simplex algorithm. In this study the algorithm was tested on synthetic data generated by the forward model. The results indicate that it should be possible to retrieve vertical variations in the pigment concentration. The synthetic data were generated for spectral bands that coincide with those of the Medium Resolution Imaging Spectrometer sensor, which will be a part of the mstrument package of the upcoming Environmental Satellite.
机译:海洋颜色的光学遥感技术是一项行之有效的技术,可用于常规生成海洋成分图。用于从海洋颜色的测量值推断颜料浓度的检索算法通常基于上洋柱垂直垂直的假设。但是,在沿海水域和峡湾中经常会遇到水柱的稳定分层现象。这种分层对于浮游植物绽放的启动,维持和物种组成起决定性作用。在这里,我们提出了一种光学遥感算法,能够解决这样的海洋垂直结构。假定垂直结构由具有不同叶绿素a浓度的两个均质层组成。该算法旨在确定两层叶绿素a的浓度以及上层的厚度。这三个参数影响海洋颜色,并通过逆建模技术同时进行检索。该技术包括对耦合的大气-海洋系统使用辐射传输计算,以模拟在卫星传感器各个波段中接收到的辐射,并将这些模拟结果与测得的辐射进行比较。通过使用优化算法,可以将模拟和测量的辐射之间的差的绝对值的总和最小化,并且所检索的参数是那些产生测量和模拟的数据之间的差的最小和的参数。我们在研究中使用的优化算法是模拟退火方法,它是下坡单纯形算法的扩展。在这项研究中,该算法在正向模型生成的综合数据上进行了测试。结果表明应该有可能恢复颜料浓度的垂直变化。生成的合成数据的光谱带与中分辨率成像光谱仪传感器的光谱带一致,该光谱带将成为即将到来的环境卫星的仪器套件的一部分。

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