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...
This article considers the evolutionary pressures that have brought us to our present state and how these forces will likely change, with a focus on U.S. institutional structures.
This report summarizes the research conducted during the first quarter of
the calendar year 1961 by the Department of Oceanography, Oregon State
University, under Contract Nonr 1286(02) Project NR 083-102 with the
Office of Naval Research.
This report summarizes the research conducted during the second quarter
of the calendar year 1961 by the Department of Oceanography, Oregon State
University, under Contract Nonr 1286(02) Project NR 083-102 with the
Office of Naval Research, and Grant No. G 15070 with the National Science
Foundation.
This report summarizes the research conducted during the fourth quarter
of the calendar year 1961 by the Department of Oceanography, Oregon
State University, under contract Nonr 1286(02) Project NR 083-102 with
the Office of Naval Research, and Grant No. G 19783 with the National
Science Foundation.
This report summarizes the research conducted during the third quarter of
the calendar year 1961 by the Department of Oceanography, Oregon State
University, under contract Nonr 1286(02) Project NR 083-102 with the Office
of Naval Research, and Grant No. G 15070 with the National Science Foundation.
The following report presents a summary of the work conducted between
1 March 1973 and 31 December 1973 as proposed in our research contract "The
Development of Methods for Studying Physical and Biological Processes in
the Nearshore Zone on the Pacific Coast of the United States," supported by
the Eugene...
The distribution of Antarctic Intermediate Water in the South
Pacific has been examined using a model of horizontal advection,
along the Sigma-t surface 27.10, with three point vertical mixing.
The core of the Antarctic Intermediate Water mass was traced
from the Antarctic Convergence northward. The charts used to
describe the...