Ocean biogeochemical signatures of the North Pacific Blob

The Blob was the early manifestation of the Northeast Pacific marine heat wave from 2013 to 2016. While the upper ocean temperature in the Blob has been well described, the impacts on marine biogeochemistry have not been fully studied. Here, we characterize and develop understanding of Eastern North...

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Published in:Geophysical Research Letters
Other Authors: Mogen, Samuel C. (author), Lovenduski, Nicole S. (author), Dallmann, Allysa R. (author), Gregor, Luke (author), Sutton, Adrienne J. (author), Bograd, Steven J. (author), Quiros, Nathali Cordero (author), Di Lorenzo, Emanuele (author), Hazen, Elliott L. (author), Jacox, Michael G. (author), Buil, Mercedes Pozo (author), Yeager, Stephen (author)
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.1029/2021GL096938
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spelling ftncar:oai:drupal-site.org:articles_25419 2024-04-14T08:17:43+00:00 Ocean biogeochemical signatures of the North Pacific Blob Mogen, Samuel C. (author) Lovenduski, Nicole S. (author) Dallmann, Allysa R. (author) Gregor, Luke (author) Sutton, Adrienne J. (author) Bograd, Steven J. (author) Quiros, Nathali Cordero (author) Di Lorenzo, Emanuele (author) Hazen, Elliott L. (author) Jacox, Michael G. (author) Buil, Mercedes Pozo (author) Yeager, Stephen (author) 2022-05-16 https://doi.org/10.1029/2021GL096938 en eng Geophysical Research Letters--Geophysical Research Letters--0094-8276--1944-8007 Salinity and other variables collected from time series observations using Bubble type equilibrator for autonomous carbon dioxide (CO2) measurement, Carbon dioxide (CO2) gas analyzer and other instruments from MOORINGS_PAPA_145W_50N in the North Pacific Ocean from 2007-06-08 to 2014-11-06 (NCEI Accession 0160486)--10.3334/cdiac/otg.tsm_papa_145w_50n_o2_n2 PyCO2SYS: marine carbonate system calculations in Python--10.5281/zenodo.5176106 articles:25419 doi:10.1029/2021GL096938 ark:/85065/d75142zx Copyright 2022 American Geophysical Union. article Text 2022 ftncar https://doi.org/10.1029/2021GL096938 2024-03-21T18:00:26Z The Blob was the early manifestation of the Northeast Pacific marine heat wave from 2013 to 2016. While the upper ocean temperature in the Blob has been well described, the impacts on marine biogeochemistry have not been fully studied. Here, we characterize and develop understanding of Eastern North Pacific upper ocean biogeochemical properties during the Winter of 2013-2014 using in situ observations, an observation-based product, and reconstructions from a collection of ocean models. We find that the Blob is associated with significant upper ocean biogeochemical anomalies: A 5% increase in aragonite saturation state (temporary reprieve of ocean acidification) and a 3% decrease in oxygen concentration (enhanced deoxygenation). Anomalous advection and mixing drive the aragonite saturation anomaly, while anomalous heating and air-sea gas exchange drive the oxygen anomaly. Marine heatwaves do not necessarily serve as an analog for future change as they may enhance or mitigate long-term trends. Article in Journal/Newspaper Ocean acidification OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Pacific The Blob ENVELOPE(-124.933,-124.933,-73.400,-73.400) Geophysical Research Letters 49 9
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
description The Blob was the early manifestation of the Northeast Pacific marine heat wave from 2013 to 2016. While the upper ocean temperature in the Blob has been well described, the impacts on marine biogeochemistry have not been fully studied. Here, we characterize and develop understanding of Eastern North Pacific upper ocean biogeochemical properties during the Winter of 2013-2014 using in situ observations, an observation-based product, and reconstructions from a collection of ocean models. We find that the Blob is associated with significant upper ocean biogeochemical anomalies: A 5% increase in aragonite saturation state (temporary reprieve of ocean acidification) and a 3% decrease in oxygen concentration (enhanced deoxygenation). Anomalous advection and mixing drive the aragonite saturation anomaly, while anomalous heating and air-sea gas exchange drive the oxygen anomaly. Marine heatwaves do not necessarily serve as an analog for future change as they may enhance or mitigate long-term trends.
author2 Mogen, Samuel C. (author)
Lovenduski, Nicole S. (author)
Dallmann, Allysa R. (author)
Gregor, Luke (author)
Sutton, Adrienne J. (author)
Bograd, Steven J. (author)
Quiros, Nathali Cordero (author)
Di Lorenzo, Emanuele (author)
Hazen, Elliott L. (author)
Jacox, Michael G. (author)
Buil, Mercedes Pozo (author)
Yeager, Stephen (author)
format Article in Journal/Newspaper
title Ocean biogeochemical signatures of the North Pacific Blob
spellingShingle Ocean biogeochemical signatures of the North Pacific Blob
title_short Ocean biogeochemical signatures of the North Pacific Blob
title_full Ocean biogeochemical signatures of the North Pacific Blob
title_fullStr Ocean biogeochemical signatures of the North Pacific Blob
title_full_unstemmed Ocean biogeochemical signatures of the North Pacific Blob
title_sort ocean biogeochemical signatures of the north pacific blob
publishDate 2022
url https://doi.org/10.1029/2021GL096938
long_lat ENVELOPE(-124.933,-124.933,-73.400,-73.400)
geographic Pacific
The Blob
geographic_facet Pacific
The Blob
genre Ocean acidification
genre_facet Ocean acidification
op_relation Geophysical Research Letters--Geophysical Research Letters--0094-8276--1944-8007
Salinity and other variables collected from time series observations using Bubble type equilibrator for autonomous carbon dioxide (CO2) measurement, Carbon dioxide (CO2) gas analyzer and other instruments from MOORINGS_PAPA_145W_50N in the North Pacific Ocean from 2007-06-08 to 2014-11-06 (NCEI Accession 0160486)--10.3334/cdiac/otg.tsm_papa_145w_50n_o2_n2
PyCO2SYS: marine carbonate system calculations in Python--10.5281/zenodo.5176106
articles:25419
doi:10.1029/2021GL096938
ark:/85065/d75142zx
op_rights Copyright 2022 American Geophysical Union.
op_doi https://doi.org/10.1029/2021GL096938
container_title Geophysical Research Letters
container_volume 49
container_issue 9
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