The effect of island generated flow disturbances on chlorophyll distribution: a study in the vicinity of Palmyra Atoll

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Abstract/Contents

Abstract
Palmyra Atoll is located at 5.9° N, 162.1° W in the Line Island chain. It is in the southern region of the North-East Trade winds, and in the midst of the North Equatorial Countercurrent (NECC) year round. ADCP, fluorometer, and CTD data was used to sample the water column to depths of 300 meters during a cruise aboard the Robert C. Seamans in May and June 2003. A southeasterly incident current generated significant shear and mixing as it passed the island. The wake of the island showed enhanced primary production as indicated by a raise in chlorophyll a concentration. The greatest enhancement seen was near a cold-core cyclonic eddy to the south. Areas of elevation in the thermocline showed corresponding enhancements in productivity, suggesting that upwelling deep water is an important source of nutrients to Palmyra’s ecosystem.

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Type of resource text
Date created June 12, 2003

Creators/Contributors

Author Clowes, Alec
Author Reineman, Ben

Subjects

Subject Stanford@SEA
Subject S-187
Subject Hopkins Marine Station
Subject Department of Biology
Subject Department of Earth System Science
Subject BIOHOPK 182H
Subject BIOHOPK 323H
Subject EARTHSYS 323
Subject ESS 323
Subject Palmyra Atoll
Subject chlorophyll distribution
Subject flow disturbances
Subject ADCP
Subject shear
Subject mixing
Genre Student project report

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This work is licensed under a Creative Commons Attribution 3.0 Unported license (CC BY).

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Preferred Citation
Alec Clowes and Ben Reineman, 2003. The effect of island generated flow disturbances on chlorophyll distribution: a study in the vicinity of Palmyra Atoll. Unpublished student research paper, S-187, Stanford@SEA, Stanford Digital Repository. https://purl.stanford.edu/qy007ht7512.

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