Satellite oceanography

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Components of a passive “ocean color” remote sensing systemUsing Visible wavelengthssourcesensorsignalraw datacalibration/validationAbsorption and scatteringof visible light – dependson pigments in the waterThe “color” is thewavelength that isnot absorbed!processing /dissemination
Surface Temperature and Chlorophyll: 1 kmSST: 26 Sept. 1998BathymetryChl-a Pigment:26-27 Sept. 1998
Page 1 and 2: Ocean Remote Sensing from Satellite
Page 3 and 4: Remote Sensing PioneersEarly Days 1
Page 6 and 7: Ships take time to “map out” an
Page 9 and 10: Components of a passive “SST” r
Page 11 and 12: Orbits Determine SamplingGeostation
Page 13 and 14: A Global System of Geosynchronous S
Page 15 and 16: What SeaWiFS (visible) sees in one
Page 17 and 18: Space Debris
Page 24 and 25: Specific ExamplesSea Surface Temper
Page 27 and 28: Why Use Microwave?Clouds!Two-days o
Page 29: Passive measurementSpecific Example
Page 33 and 34: Components of an active radar “al
Page 35 and 36: Surface Height, Temperature and Chl
Page 37: Components of an active radar “sc
Page 43 and 44: Altimeter and Scatterometer
Page 45 and 46: Altimeter Estimates ofGlobal Sea Le
Page 47 and 48: Computer Models of 3-D Currents and
Page 49 and 50: Future Technologies“Next generati
Page 51 and 52: Web SitesOSU/COAS: Cooperative Inst

Satellite oceanography

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