A 4000*2305 SPOT_1 bi-HRV mosaic of Rangiroa atoll,
Tuamotu archipelago, French Polynesia
As this image does not have a blue band, 4SM modeling is only possible down to 4-6 m depth range.
For deeper areas, a depth is computed using XS1 alone
and assuming that the bottom is uniformly bright (coral sand/mud).
The "One Band Case", of course is the cause of much confusion,
as darker bottoms substrates (coral growths) are mapped to be deeper than their immediate surrounding.
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For deeper areas,
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![]() Lower: Image_Z in grey shades Today's Blue_Lagoon is just the heir of an older one: see how depths over the rim of the old_Blue_Lagoon is "inverted" by the One_Band case: this rim of course is expected to be shallower than inner lagoon bottom, whereas it is shown to be deeper!! WE LACK A BLUE BAND! | ![]() This location appears to have experienced a Blue_Lagoon_development_phase in the old days. No inversion of depths over the rim here, though. |
![]() | An easy calibration, for XS1 and XS2 at least Jerlov water type OII+0.36: not that clear, hey, although this very large lagoon has a complex hydrologic structure, with much less clear water masses at some locations far away from major inputs of crystal clear oceanic waters. Atmospheric adjacency effect is the cause of some problems along the densely vegetated areas. |
![]() | A SPOT 1 bi-HRV image of exceptional quality, taken on a "calm and clear day" It carries its own radiometric limitations though. The radiometric quality of SPOT 5 images is much better : see also sanaa.htm? |