| Oceanography > Issues > Archive > Volume 17 > Issue 2 |
2004, Oceanography 17(2):16–23, http://dx.doi.org/10.5670/oceanog.2004.43
Authors | First Paragraph | Full Article | Citation
Grace Chang | Ocean Physics Laboratory, University of California, Santa Barbara, Goleta, CA, USA
Kevin Mahoney | Monterey Bay Aquarium Research Institute, Moss Landing, CA, USA
Amanda Briggs-Whitmire | College of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, OR, USA
David D.R. Kohler | Florida Environmental Research Institute, Tampa, FL, USA
Curtis D. Mobley | Sequoia Scientific, Inc., Bellevue, WA, USA
Marlon Lewis | Department of Oceanography, Dalhousie University, Halifax, Nova Scotia, Canada
Mark A. Moline | Biological Sciences Department, California Polytechnic State University, San Luis Obispo, CA, USA
Emmanuel Boss | School of Marine Sciences, University of Maine, Orono, ME, USA
Minsu Kim | School of Civil & Environmental Engineering, Cornell University, Ithaca, NY, USA
William Philpot | School of Civil & Environmental Engineering, Cornell University, Ithaca, NY, USA
Tommy D. Dickey | Ocean Physics Laboratory, University of California, Santa Barbara, Goleta, CA, USA
A multispectral optical sensor collects data at select wavebands or channels. An example is the Sea-viewing Wide-Field-of-view Sensor (SeaWiFS) ocean color satellite, which measures eight wavebands between 402 and 885 nm (20-40 nm bandwidth with peaks centered around 412, 443, 490, 510, 555, 670, 765, and 865 nm). Optical oceanographers have been using multispectral sensors since the 1980s with great success.
Chang, G., K. Mahoney, A. Briggs-Whitmire, D.D.R. Kohler, C.D. Mobley, M. Lewis, M.A. Moline, E. Boss, M. Kim, W. Philpot, and T.D. Dickey. 2004. The new age of hyperspectral oceanography. Oceanography 17(2):16–23, http://dx.doi.org/10.5670/oceanog.2004.43.