Optical remote sensing of waters with vertical structure

Citation
O. Frette et al., Optical remote sensing of waters with vertical structure, APPL OPTICS, 40(9), 2001, pp. 1478-1487
Citations number
34
Categorie Soggetti
Apllied Physucs/Condensed Matter/Materiales Science","Optics & Acoustics
Journal title
APPLIED OPTICS
ISSN journal
00036935 → ACNP
Volume
40
Issue
9
Year of publication
2001
Pages
1478 - 1487
Database
ISI
SICI code
0003-6935(20010320)40:9<1478:ORSOWW>2.0.ZU;2-0
Abstract
Optical remote sensing of ocean color is a well-established technique that is used to produce maps of marine constituents on a routine basis. Retrieva l algorithms used to infer pigment concentrations from measurements of ocea n 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 i s decisive for the initiation, maintainance, and species composition of phy toplankton blooms. Here we present an optical remote-sensing algorithm with the ability to resolve such a vertical structure of oceanic waters. The ve rtical structure is assumed to consist of two homogeneous layers with diffe rent concentrations of chlorophyll a. The algorithm is designed to determin e the chlorophyll-alpha concentrations of the two layers as well as the thi ckness of the upper layer. These three parameters influence the ocean color and are simultaneously retrieved through an inverse-modeling technique. Th is technique consists of using radiative-transfer computations for a couple d atmosphere-ocean system to simulate radiances received in various bands o f 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 t he retrieved parameters are those that yield the minimum sum of differences between measured and simulated data. The optimization algorithm that we us ed 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 concentr ation. The synthetic data were generated for spectral bands that coincide w ith those of the Medium Resolution Imaging Spectrometer sensor, which will be a part of the instrument package of the upcoming Environmental Satellite . (C) 2001 Optical Society of America.