A time series of Landsat 8 images
at San Lorenzo Channel, Baja California


LANDSAT 8 OLIP 
 
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=1Blue=2Green=3PAN=4Red=5NIR=6 and SWIR1=7
Collaboration with 
Fabio Favoretto, Ph.D Student, Coralline Algae Ecology
Grupo Interdisciplinario de Ciencia Ambiental, Universidad Autonoma de Baja California Sur
Carretera al sur km 5.5  | La Paz
favorettofabio@gmail.com
Using pan sharpened images in this study
Pan sharpening  using Rstudio with Brovey method

work done october-november 2016
Procedure/flowchart for operating  4SM.7.00

home
 
 

go to Combined Depth vs Fabio's DTM
go to Combined Depth vs Fabio's Sonar seatruth
 
 
Enforcing Combined Depth
  • Now that I have a new DTM derived for the whole study area by combining retrieved depths from nine scenes, 
    • I can enforce ZDTM while inverting the simplified radiative transfer equation.
  • So much for the Soil Line assumption, it is not needed anymore at this stage.
  • This allows for more contrasted water column corrected bottom reflectance signatures:
    • this is a bonus for bottom typing.
    • RMSE on retrieved depths now are really representative of the 4SM method, as this new DTM is near-perfect.
everything below is limited to this image subset
 
CC
BOA WCC
normalized CoefNorm=5 
SAM
Spectral
Angle
Mapper
Retrieved depth
vs
Combined Depth
Depth
Histograms
Red is Combined Depth
Grey is Retrieved Depth

October 19th 2013

October 19th 2013

October 19th 2013
tide correction -0.6 m
RMSE=0.78 m

 

October 19th 2013
tide correction -0.6 m

November 4th 2013 

November 4th 2013

November 4th 2013
tide correction -0.5 m

November 4th 2013

tide correction -0.5 m
   January 07th 2014   January 07th 2014   January 07th 2014
tide correction -0.2 m

 
   January 07th 2014
tide correction -0.2 m
   February 08th 2014  February 08th 2014   February 08th 2014
tide correction: -0.5 m
 
 February 08th 2014
tide correction: -0.5 m
  October 22th 2014   October 22th 2014    October 22th 2014
tide correction: 0.3 m
  October 22th 2014
tide correction: 0.3 m
 January 29th 2016  January 29th 2016  
January 29th 2016
tide correction: 0.3 m
 
January 29th 2016
tide correction: 0.3 m
 March 1rst 2016  March 1rst 2016  March 1rst 2016
tide correction: -0.3 m
  March 1rst 2016
tide correction: -0.3 m

October 11th 2016
 

October 11th 2016

 

October 11th 2016 
tide correction: -0.20 m

October 11th 2016  
tide correction: -0.20 m
  
puzzling! 

October 27th 2016

October 27th 2016

October 27th 2016
tide correction: 0.00 m 

 

October 27th 2016
tide correction: 0.00 m 

 

Work finished
Andy

Champagne!
Fabio
 
  • Uncertainties: here you can appreciate that each of the 9 instances of this time series carries its own lot of unwanted/weird variations
    • which need to be sorted out to produce a DTM
    • Profile_black: see that combining depths removes most of the noise at depth: Goooooooooooooooood!
  • Existing nautical-chart/DTM?
    • OK, 4SM does not require access to an existing map or depth dataset
      • But, in view of such adverse variations, it certainly helps the practioner to keep his cool
      • And chances are that some info may be gathered from the NET anyway
    • Or a blind test has to be dead-blind: then make sure your scene is of exceptional/improbable quality, and be prepared to face the uggly consequences of a bad choice!
  
  • Breaking new ground here!
    • You are the one to make sense of it all
    • Please do not hesitate to let me know your thoughts:
      • what is usefull and needs to be investigated further
      • what is futile and should go to the back burner
  • Bay of La Paz
    • I am surprised how good the combined depth results appear to be
    • although I had gathered that this was a lost case, in view of so adverse (anthropogenic?) turbidity in the bay

go to Combined Depth vs Fabio's DTM
 

 



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