Using the Panchromatic band for water column correction to derive water depth and spectral bottom signature: Landsat 8 OLIP bandset used for this work Purple=1, Blue=2, Green=3, PAN=4, Red=5, NIR=6 and SWIR1=7 |
GREEN solution is used by most practioners after atmospheric correction and calibration using depth soundings | PAN solution is a breakthrough by 4SM requires neither atmospheric correction nor calibration using depth soundings |
|
I prefer PAN solution GREEN solution impractical in this water |
30 m GSD | 15 m GSD |
requires resampling the PAN band from 15m GSD to 30m GSD | requires resampling the MULTI bands from 30m GSD to 15m GSD |
![]() | ![]() |
![]() | ![]() |
I prefer 15 m GSD resampled |
15 m GSD resampled
| 15 m GSD pan-sharpened
|
I prefer 15 m GSD resampled | BUT: looks like your own two pan-sharpened images gave me quite some satisfaction: I need to go back, see why that! Maybe the R routine is much better than mine |
No smoothing applied
| Smoothing applied
|
see GSD 30 m Not smoothed Profile Black![]() | Profile Black see GSD 30 m Smoothed![]() |
![]() | ![]() |
![]() | ![]() |
![]() | ![]() |
NOTE: Pinkish hues in SAM signal are not an artifact They actually cover a wide range of bottom brightness, which includes very bright (saturated) bottoms What causes it? I am still looking for your rhodoliths! see legend for SAM | ![]() Some SAM bottom signatures SAM 10 is reference bright bottom SAM 12, 14 etc are a suite of greenish signatures SAM 31, 33, 35 etc are a suite of pinkish bottoms |