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 Please refer to Bora Bora and Sanaa for use of the PANchromatic band for water column correction |
![]() Seatruth regression Zcomputed vs Zseatruth RMSE=0.57 m Tide correction applied: 1.0 m | ![]() Difference ZDTM - Z4SM - 1.0m Tide correction applied: 1.0 m see legend |
![]() Profile GREEN regression It would appear that a CoefZ~=0.88 is needed? This would yield Zfinal=0.88*Z-0.5 in meters | ![]() Profile GREEN |
![]() Profile GREEN location Tide correction applied: 0.50 m see legend | ![]() Profile GREEN location DTM by Harris-Ellis see legend |
![]() Panchromatic band sum-aggregated to 30 m, exhibits excellent radiometric quality | ![]() TCC Landsat OLI exhibits excellent radiometric quality |
![]() Glint regression based on NIR band | ![]() Glint regression based on SWIR1 band |
Deglinting based on SWIR1 band is excellent! ![]() Deglinted BOA FCC Very shallow areas are well deglinted, thanks to near-null water penetration of the SWIR band | Deglinting based on SWIR1 band is excellent! ![]() Deglinted BOA TCC
|
![]() Deglinted Red band exhibits bottom detection in excess of 10 m Yellow is optically deep Following study of hyperspectral data, we shall see below that this requires manually decreasing 2K for the RED band | ![]() Deglinted Pan band exhibits bottom detection in excess of 30 m We shall see below how 2KPAN is established |
![]() Retrieved depth see legend | ![]() BOA TCC water column corrected pinkish areas denote an excess of RED radiance is it some "whiting"? or suspended particles? or pinkish oolith bottoms? |
![]() Average bottom brightness very bright in january 2014 | ![]() Spectral Angle mapping january 2014 this is a done using a spectral angle scheme (SAM) see legend for SAM |