The edge effect in the Northeast North Pacific Ocean

During April 1989, an intensive, short-term study of oceanic zooplankton tested the hypothesis that multidimensional distribution (patchiness, diffusion, layering) reflects the water mass interaction in the Northeast North Pacific Ocean (NENPO) during the spring season. The mixing water masses crea...

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Main Author: JW Foerster
Format: Article
Language:English
Published: Universidad Autónoma de Baja California 1996-03-01
Series:Ciencias Marinas
Subjects:
Online Access:http://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/855
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author JW Foerster
author_facet JW Foerster
author_sort JW Foerster
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description During April 1989, an intensive, short-term study of oceanic zooplankton tested the hypothesis that multidimensional distribution (patchiness, diffusion, layering) reflects the water mass interaction in the Northeast North Pacific Ocean (NENPO) during the spring season. The mixing water masses created an edge effect to which the biota responded. A dual frequency sonar array (38 kHz, 200 kHz), towing in tandem with an oceanographic sensor system, recorded zooplankton and environmental changes across various water masses. The tandem sensor system was a method to synoptically map the NENPO at the beginning of the productive period of early spring over an area of 3.3 × 105 km, 125 m in depth. Results from the plankton data showed patchiness and layers conforming to oceanographic physical features. These patterns appeared to define the interactions of the water masses and confirm the hypothesis.
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spelling doaj.art-ae26c8badb304a419f9449c2f6556f732024-03-04T16:43:20ZengUniversidad Autónoma de Baja CaliforniaCiencias Marinas0185-38802395-90531996-03-0122210.7773/cm.v22i2.855The edge effect in the Northeast North Pacific OceanJW Foerster0US Naval Academy During April 1989, an intensive, short-term study of oceanic zooplankton tested the hypothesis that multidimensional distribution (patchiness, diffusion, layering) reflects the water mass interaction in the Northeast North Pacific Ocean (NENPO) during the spring season. The mixing water masses created an edge effect to which the biota responded. A dual frequency sonar array (38 kHz, 200 kHz), towing in tandem with an oceanographic sensor system, recorded zooplankton and environmental changes across various water masses. The tandem sensor system was a method to synoptically map the NENPO at the beginning of the productive period of early spring over an area of 3.3 × 105 km, 125 m in depth. Results from the plankton data showed patchiness and layers conforming to oceanographic physical features. These patterns appeared to define the interactions of the water masses and confirm the hypothesis. http://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/855dual frequencysonarplanktonfrontal zoneNorth Pacific CurrentDavidson Current
spellingShingle JW Foerster
The edge effect in the Northeast North Pacific Ocean
Ciencias Marinas
dual frequency
sonar
plankton
frontal zone
North Pacific Current
Davidson Current
title The edge effect in the Northeast North Pacific Ocean
title_full The edge effect in the Northeast North Pacific Ocean
title_fullStr The edge effect in the Northeast North Pacific Ocean
title_full_unstemmed The edge effect in the Northeast North Pacific Ocean
title_short The edge effect in the Northeast North Pacific Ocean
title_sort edge effect in the northeast north pacific ocean
topic dual frequency
sonar
plankton
frontal zone
North Pacific Current
Davidson Current
url http://www.cienciasmarinas.com.mx/index.php/cmarinas/article/view/855
work_keys_str_mv AT jwfoerster theedgeeffectinthenortheastnorthpacificocean
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