Factors Influencing the Degree of Saturation of the Surface and Intermediate Waters of the North Pacific Ocean with Respect to Aragonite
New carbonate chemistry data obtained during a 1982 cruise have been combined with earlier GE‐OSECS and INDOPAC data to determine the degree of aragonite saturation of surface and intermediate waters of the North Pacific. Large gradients in saturation state occur in the region of the Subarctic Front...
Published in: | Journal of Geophysical Research |
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Digital Commons @ University of South Florida
1984
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ftusouthflorida:oai:digitalcommons.usf.edu:msc_facpub-1084 2023-07-30T04:07:09+02:00 Factors Influencing the Degree of Saturation of the Surface and Intermediate Waters of the North Pacific Ocean with Respect to Aragonite Feely, Richard A. Byrne, Robert H. Betzer, Peter R. Gendron, James F. Acker, James G. 1984-11-20T08:00:00Z application/pdf https://digitalcommons.usf.edu/msc_facpub/85 https://doi.org/10.1029/JC089iC06p10631 https://digitalcommons.usf.edu/context/msc_facpub/article/1084/viewcontent/Feely_et_al_1984_Journal_of_Geophysical_Research__Oceans.pdf unknown Digital Commons @ University of South Florida https://digitalcommons.usf.edu/msc_facpub/85 doi:10.1029/JC089iC06p10631 https://digitalcommons.usf.edu/context/msc_facpub/article/1084/viewcontent/Feely_et_al_1984_Journal_of_Geophysical_Research__Oceans.pdf default Marine Science Faculty Publications Life Sciences Marine Biology article 1984 ftusouthflorida https://doi.org/10.1029/JC089iC06p10631 2023-07-13T20:21:41Z New carbonate chemistry data obtained during a 1982 cruise have been combined with earlier GE‐OSECS and INDOPAC data to determine the degree of aragonite saturation of surface and intermediate waters of the North Pacific. Large gradients in saturation state occur in the region of the Subarctic Front in the north‐south direction and across the Subtropical Gyre in the east‐west direction. These gradients are primarily due to the extensive mixing that occurs in the intermediate waters of the western North Pacific. The major variations in saturation state were primarily related to the carbonate ion concentration, which, in turn, is primarily a function of mixing and biological processes. The present aragonite saturation depth at our northernmost station in the western North Pacific was calculated to be within 120 m of the surface. This result was directly corroborated by observations of aragonite dissolution under in vitro conditions. Our calculations show that one possible effect of fossil fuel‐derived CO2 on the surface of the North Pacific will be a steady progression of undersaturation from the northern to southern and western areas, with the first sign of undersaturation possibly occurring as early as the second half of the next century. Article in Journal/Newspaper Subarctic University of South Florida St. Petersburg: Digital USFSP Pacific Journal of Geophysical Research 89 C6 10631 |
institution |
Open Polar |
collection |
University of South Florida St. Petersburg: Digital USFSP |
op_collection_id |
ftusouthflorida |
language |
unknown |
topic |
Life Sciences Marine Biology |
spellingShingle |
Life Sciences Marine Biology Feely, Richard A. Byrne, Robert H. Betzer, Peter R. Gendron, James F. Acker, James G. Factors Influencing the Degree of Saturation of the Surface and Intermediate Waters of the North Pacific Ocean with Respect to Aragonite |
topic_facet |
Life Sciences Marine Biology |
description |
New carbonate chemistry data obtained during a 1982 cruise have been combined with earlier GE‐OSECS and INDOPAC data to determine the degree of aragonite saturation of surface and intermediate waters of the North Pacific. Large gradients in saturation state occur in the region of the Subarctic Front in the north‐south direction and across the Subtropical Gyre in the east‐west direction. These gradients are primarily due to the extensive mixing that occurs in the intermediate waters of the western North Pacific. The major variations in saturation state were primarily related to the carbonate ion concentration, which, in turn, is primarily a function of mixing and biological processes. The present aragonite saturation depth at our northernmost station in the western North Pacific was calculated to be within 120 m of the surface. This result was directly corroborated by observations of aragonite dissolution under in vitro conditions. Our calculations show that one possible effect of fossil fuel‐derived CO2 on the surface of the North Pacific will be a steady progression of undersaturation from the northern to southern and western areas, with the first sign of undersaturation possibly occurring as early as the second half of the next century. |
format |
Article in Journal/Newspaper |
author |
Feely, Richard A. Byrne, Robert H. Betzer, Peter R. Gendron, James F. Acker, James G. |
author_facet |
Feely, Richard A. Byrne, Robert H. Betzer, Peter R. Gendron, James F. Acker, James G. |
author_sort |
Feely, Richard A. |
title |
Factors Influencing the Degree of Saturation of the Surface and Intermediate Waters of the North Pacific Ocean with Respect to Aragonite |
title_short |
Factors Influencing the Degree of Saturation of the Surface and Intermediate Waters of the North Pacific Ocean with Respect to Aragonite |
title_full |
Factors Influencing the Degree of Saturation of the Surface and Intermediate Waters of the North Pacific Ocean with Respect to Aragonite |
title_fullStr |
Factors Influencing the Degree of Saturation of the Surface and Intermediate Waters of the North Pacific Ocean with Respect to Aragonite |
title_full_unstemmed |
Factors Influencing the Degree of Saturation of the Surface and Intermediate Waters of the North Pacific Ocean with Respect to Aragonite |
title_sort |
factors influencing the degree of saturation of the surface and intermediate waters of the north pacific ocean with respect to aragonite |
publisher |
Digital Commons @ University of South Florida |
publishDate |
1984 |
url |
https://digitalcommons.usf.edu/msc_facpub/85 https://doi.org/10.1029/JC089iC06p10631 https://digitalcommons.usf.edu/context/msc_facpub/article/1084/viewcontent/Feely_et_al_1984_Journal_of_Geophysical_Research__Oceans.pdf |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Subarctic |
genre_facet |
Subarctic |
op_source |
Marine Science Faculty Publications |
op_relation |
https://digitalcommons.usf.edu/msc_facpub/85 doi:10.1029/JC089iC06p10631 https://digitalcommons.usf.edu/context/msc_facpub/article/1084/viewcontent/Feely_et_al_1984_Journal_of_Geophysical_Research__Oceans.pdf |
op_rights |
default |
op_doi |
https://doi.org/10.1029/JC089iC06p10631 |
container_title |
Journal of Geophysical Research |
container_volume |
89 |
container_issue |
C6 |
container_start_page |
10631 |
_version_ |
1772820294474399744 |