|Using the Panchromatic band for water column correction |
to derive water depth and spectral bottom signature:
Landsat 8 OLIP bandset used for this work
MULTI dada subsampled to 15 m ground sampling distance
|Collaboration with |
This has been presented at the ERIM Marine RS conference in 1998.
4SM only relies on the information contained in the bareland and marine parts of the spectral imagery in order to derive scene-dependent modeling parameters.
Seed value: then 4SM uses the table of diffuse attenuation coefficients for downwelling irradiance in marine/coastal Case I waters worldwide published in 1976 by Jerlov in his reference book "Marine Optics" (Elsevier), in order to derive a seed value for the operational attenuation coefficient for the water column under study which applies to the central(?) wavelength of each of the spectral waveband.
Spectral K: then, using that seed value, spectral operational K values are derived from Ki/Kj ratios observed for all possible pairs of visible bands i and j of the image itself.
Operational wavelength: this requires effective visible wavelengths to specified correctly, as it would seem that wavelength at mid-waveband are not suitable
Therefore, 4SM does not require, neither does it uses, any preliminary field data for the estimation of any of the modeling parameters.
As a consequence, the only thing that is needed is the imagery itself and the specifications of its band setting.
But all computed depths still need to be multiplied
by a final depth correction factor
to be derived from sea truth evidence when available:
Final_Z = CoefZ*Z - Htide_to_datum