Fernando Gilbes1, Vilmaliz Rodriguez, Jose Martinez, and Eidalia ...

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SEPARATING THE REMOTE SIGNAL What we Measure • Water Optical Properties • Bottom Reflectance FromNEMO Overview Nemo.nrl.navy.gov
REFLECTANCE VS. SEDIMENTS • Reflectance • Previous findings • Increase in SS = Increase in reflectance • Red & Near IR wavelengths show lower slopes in high SS • Mayagüez Bay • Concentration too low to provide strong response From Witte et al. (1982)
Page 1 and 2: Fernando Gilbes 1 , Vilmaliz Rodrig
Page 3 and 4: TWO SEASONS IS EQUAL TO TWO OPTICAL
Page 5 and 6: MULTI‐SPECTRAL SATELLITE SENSORS
Page 7: REMOTE SIGNAL FROM THE OCEAN
Page 11 and 12: TECHNICAL APPROACH Field Work Testi
Page 13 and 14: GRID OF SAMPLING STATIONS
Page 15 and 16: MODIS SPATIAL RESOLUTION Bands 1-2
Page 17 and 18: SUSPENDED SEDIMENTS • Miller and
Page 19 and 20: RESULTS IN MAYAGUEZ BAY
Page 21 and 22: FIELD SS AND MODIS‐B1 %REFLECTANC
Page 23 and 24: FIELD SS AND MODIS‐B1 %REFLECTANC
Page 25 and 26: SS WITH NEW ALGORITHM October 7, 20
Page 27 and 28: AVIRIS MISSION OVER PUERTO RICO AUG
Page 29 and 30: Suspended Sediments measured during
Page 31 and 32: IMAGE PROCESSING Raw Image from NAS
Page 33: Testing different bands
Page 37 and 38: SUSPENDED SEDIMENTS AS DETERMINED W
Page 39: CONCLUSIONS • AVIRIS proved to be

Fernando Gilbes1, Vilmaliz Rodriguez, Jose Martinez, and Eidalia ...

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