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Using an optimization technique, we derived subsurface properties of coastal and oceanic waters from measured remote-sensing reflectance spectra. These data included both optically deep and shallow environments. The measured reflectance covered a spectral range from 400 to 800 nm. The inversions used data from each 5-, 10-, and 20-nm contiguous bands, including Sea-viewing Wide Field-of-view Sensor ͑SeaWiFS͒, moderate-resolution imaging spectrometer ͑MODIS͒, and a self-defined mediumresolutiondoi:10.1364/ao.41.002191 pmid:12003210 fatcat:dydfcp5n7rg3hjc36wos45odnm