Satellite oceanography

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Surface Temperature: 1 kmIR SST: 26 Sept. 1998Bathymetry
Passive measurementSpecific ExamplesOcean color (chlorophyll)Measures light scattered and transmitted upward through theocean surface - its „color‟ (careful to distinguish between„transmission‟ and „reflection‟)PROBLEM: Most of the signal (>90%) at the satellite is NOTocean color – It is atmospheric interference: sunlight that hasbeen scattered or reflected by molecules or aerosols in theatmosphere back into the satellite‟s field-of-view.
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: Why Use Microwave?Clouds!Two-days o
Page 31 and 32: Surface Temperature and Chlorophyll
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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