A Model of the Spatial Structure and Productivity of Phytoplankton Populations during Variable Upwelling Off the Coast of Oregon

Abstract

During the season favorable for coastal upwelling off the western boundary of continents, the local circulation is strongly influenced by occasional wind events of several days' duration. Variability in the wind stress affects the rate of upwelling and ultimately the local biological productivity. To investigate the relationship between wind events and primary production off the coast of Oregon in August 1973, a time-dependent, numerical model of the upwelling circulation was coupled to a complex model of primary and secondary productivity. Primary productivity is a function of nutrient concentration, light intensity and temperature. Advection by a two-cell, upwelling circulation is the major physical mechanism leading to mesoscale patchiness in the phytoplankton, zooplankton, detritus and nutrient fields. The numerical model predicts a phytoplankton and detritus plume for which considerable observational evidence exists. Model predictions of daily primary production during intermittent upwelling are paradoxically comparable to production during strong upwelling. A new formulation for herbivore egestion as a function of food availability is proposed.

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Document Details

Document Type
Technical Report
Publication Date
Sep 01, 1976
Accession Number
ADA030900

Entities

People

  • J. S. Wroblewski

Organizations

  • Florida State University

Tags

Communities of Interest

  • Ground and Sea Platforms

DTIC Thesaurus Topics

  • Biological Processes
  • Chemical Kinetics
  • Dynamics
  • Equations
  • Grids
  • Kinetics
  • New York
  • Oceanography
  • Oceans
  • Particles
  • Phytoplankton
  • Plankton
  • Sea Surface Temperature
  • Sea Water
  • Spatial Distribution
  • Surface Temperature
  • Topography

Fields of Study

  • Environmental science

Readers

  • Aquatic Ecology
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers