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Research Notes
Beneath the Earth's Surface Biology Climate Change Coastal Zones Human health Ocean physics Polar Science Satellite Remote Sensing Solar System Research
Students in the Field
Crab Pots and Ocean Observing Microbes in Hydrates Movement of Arctic Water Masses Silicon Cycle Variability Zooplankton Discoveries
Inside COAS
Clare Reimers, 2009 AGU Fellow Charlie Miller, A Selective Biography COAS 50th Anniversary

Satellites and Remote Sensing


It is difficult to observe the vast ocean that controls much of our climate and other Earth-system processes. However, satellite instruments can quickly make a variety of measurements over a wide swath of ocean. 

Because of its excellence in satellite-based research, modeling and observations, COAS was selected to develop and maintain a center of excellence in satellite remote-sensing research and modeling of the ocean, the Cooperative Institute for Oceanographic Satellite Studies (CIOSS).

Snapshots of COAS research:

Satellite instruments return a variety of information:

  • Infared sensors measure surface temperatures which show upwelling areas where cooler, nutrient-rich water is pulled up.
  • Visual sensors measure ocean color at several wavelengths and allow estimating phytoplankton growth.
  • Microwave instruments (scatterometers, altimeters and radiometers) see through clouds, allowing all-weather measurements of the ocean surface.
  • Scatterometers measure winds and show the mixing power and driving force for currents in the top 40 meters, as well as the strength of the transfer of heat and carbon dioxide through the ocean’s surface.
  • Altimeters measure sea-surface height, which shows geostrophic currents beneath a wind layer and significant wave heights.
  • Microwave radiometers measure surface temperatures on a coarser grid than the infrared sensors, but look through clouds (which the infrared sensors cannot do).
  • Many of the above instruments are also used to look at cloud properties and to estimate the amount of radiation that reaches the surface of the ocean.
By collecting measurements over time, oceanographers can see patterns that indicate circulation and variability on time scales ranging from days to decades, for instance, from storms to global climate change.

More information:

   

Eddies in the Gulf of California
Eddies on the order of five kilometers in diameter, made visible by phytoplankton in the Gulf of California.



Canary Island wakes
Canary Island wakes, shown by SeaWiFS satellite, April 24, 1999.



Louisiana coast
Louisiana coast and the dynamic coastal region showing the suspended sediments, organic matter and phytoplankton.

 

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College of Oceanic and Atmospheric Sciences
Oregon State University
104 COAS Administration Building
Corvallis, OR 97331-5503
Telephone: (541) 737-3504
Fax: (541) 737-2064
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