An overview of mesoscales distribution of ocean color in the North Atlantic

The spatial changes in phytoplankton abundance is the result of regional differences in the amount of nutrient fluxed into the euphotic zone. The energy contributing to this flux is derived from ocean currents. A close coupling between physics and biology of the system accounts for mesoscale feature...

Full description

Bibliographic Details
Main Author: Yentsch, C. S.
Format: Other/Unknown Material
Language:unknown
Published: 1989
Subjects:
48
Online Access:http://ntrs.nasa.gov/search.jsp?R=19900023077
Description
Summary:The spatial changes in phytoplankton abundance is the result of regional differences in the amount of nutrient fluxed into the euphotic zone. The energy contributing to this flux is derived from ocean currents. A close coupling between physics and biology of the system accounts for mesoscale features associated with fluid dynamics being reflected by changes in ocean color.