The Relationship Between the Fine-scale Vertical Distributions of Macrozooplankton, Marine Snow, and Turbulences in the Upper Water Column

Abstract

Recent evidence indicates that large detrital aggregates, known as marine snow, are highly concentrated at pycnoclines and other density discontinuities in the water column due to turbulence, shear, and reduced sinking rates as the particles encounter denser fluid. The consequences of these thin layers of high particle abundance to the fine scale vertical distributions of zooplankton, many of which are voracious consumers of marine snow, is presently unknown, but likely to be significant. Our long term goal is to develop a predictive understanding of the relationship between the vertical distributions of zooplankton, marine snow, and turbulence in the ocean and the impacts of their patchy distribution in thin layers on optical and acoustical properties of the water column.

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Document Details

Document Type
Technical Report
Publication Date
Sep 30, 1997
Accession Number
ADA628487

Entities

People

  • Alice L. Alldredge
  • Sally Macintyre

Organizations

  • University of California, Santa Barbara

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Adriatic Sea
  • Boundary Layer
  • California
  • Cold Water
  • Layers
  • Marine Biology
  • Microstructure
  • Oceanography
  • Particle Flux
  • Particles
  • Remote Sensing
  • Temperature Gradients
  • Turbulence
  • Turbulent Mixing
  • Universities
  • Water
  • Zooplankton

Fields of Study

  • Environmental science

Readers

  • Economics
  • Marine Ecotoxicology
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers