Analysis of Central Equatorial Pacific Water Masses by Method of Principal Components ...
The distribution of Antarctic Intermediate Water at the extent of dispersion in the equatorial Pacific Ocean was investigated by means of multivariate analysis. Interrelationships among the upper intermediate water masses at this location are proposed. Oceanographic data contained in seven cruise le...
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Old Dominion University
1984
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ftdatacite:10.25777/jrbc-6k22 2024-04-28T07:59:20+00:00 Analysis of Central Equatorial Pacific Water Masses by Method of Principal Components ... Tuxhorn, Ross 1984 https://dx.doi.org/10.25777/jrbc-6k22 https://digitalcommons.odu.edu/oeas_etds/298/ unknown Old Dominion University article-journal Text ScholarlyArticle Thesis 1984 ftdatacite https://doi.org/10.25777/jrbc-6k22 2024-04-02T11:34:00Z The distribution of Antarctic Intermediate Water at the extent of dispersion in the equatorial Pacific Ocean was investigated by means of multivariate analysis. Interrelationships among the upper intermediate water masses at this location are proposed. Oceanographic data contained in seven cruise legs measured during the 1979-80 Hawaii to Tahiti Shuttle Experiment formed the basis of this study. Six parameters -- temperature, salinity, dissolved oxygen, phosphate, silicate and nitrate -- were used in the method of principal component analysis to classify water masses between the sea surface and 1000m. The derived water masses were compatible with previously described oceanographic features of the region. Validity of the classification was measured by Discriminant Analysis and was found to be significant. Two salinity minimum layers were determined. A deep layer (800-1000m) corresponded to core and upper AAIW, while the shallow layer was low salinity water from both the North and South Pacific. AAIW and ... Text Antarc* Antarctic DataCite Metadata Store (German National Library of Science and Technology) |
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DataCite Metadata Store (German National Library of Science and Technology) |
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The distribution of Antarctic Intermediate Water at the extent of dispersion in the equatorial Pacific Ocean was investigated by means of multivariate analysis. Interrelationships among the upper intermediate water masses at this location are proposed. Oceanographic data contained in seven cruise legs measured during the 1979-80 Hawaii to Tahiti Shuttle Experiment formed the basis of this study. Six parameters -- temperature, salinity, dissolved oxygen, phosphate, silicate and nitrate -- were used in the method of principal component analysis to classify water masses between the sea surface and 1000m. The derived water masses were compatible with previously described oceanographic features of the region. Validity of the classification was measured by Discriminant Analysis and was found to be significant. Two salinity minimum layers were determined. A deep layer (800-1000m) corresponded to core and upper AAIW, while the shallow layer was low salinity water from both the North and South Pacific. AAIW and ... |
format |
Text |
author |
Tuxhorn, Ross |
spellingShingle |
Tuxhorn, Ross Analysis of Central Equatorial Pacific Water Masses by Method of Principal Components ... |
author_facet |
Tuxhorn, Ross |
author_sort |
Tuxhorn, Ross |
title |
Analysis of Central Equatorial Pacific Water Masses by Method of Principal Components ... |
title_short |
Analysis of Central Equatorial Pacific Water Masses by Method of Principal Components ... |
title_full |
Analysis of Central Equatorial Pacific Water Masses by Method of Principal Components ... |
title_fullStr |
Analysis of Central Equatorial Pacific Water Masses by Method of Principal Components ... |
title_full_unstemmed |
Analysis of Central Equatorial Pacific Water Masses by Method of Principal Components ... |
title_sort |
analysis of central equatorial pacific water masses by method of principal components ... |
publisher |
Old Dominion University |
publishDate |
1984 |
url |
https://dx.doi.org/10.25777/jrbc-6k22 https://digitalcommons.odu.edu/oeas_etds/298/ |
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Antarc* Antarctic |
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Antarc* Antarctic |
op_doi |
https://doi.org/10.25777/jrbc-6k22 |
_version_ |
1797572142768848896 |