Effect of glacial drainage water on the CO2 system and ocean acidification state in an Arctic tidewater-glacier fjord during two contrasting years

In order to investigate the effect of glacial water on the CO2 system in the fjord, we studied the variability of the total alkalinity (AT), total dissolved inorganic carbon (CT), dissolved inorganic nutrients, oxygen isotopic ratio (δ18O), and freshwater fractions from the glacier front to the oute...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Fransson, Agneta Ingrid, Chierici, Melissa, Nomura, Daiki, Granskog, Mats A., Kristiansen, Svein, Martma, Tõnu, Nehrke, Gernot
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
Online Access:https://hdl.handle.net/11250/2994899
https://doi.org/10.1002/2014JC010320
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spelling ftimr:oai:imr.brage.unit.no:11250/2994899 2023-05-15T15:09:34+02:00 Effect of glacial drainage water on the CO2 system and ocean acidification state in an Arctic tidewater-glacier fjord during two contrasting years Fransson, Agneta Ingrid Chierici, Melissa Nomura, Daiki Granskog, Mats A. Kristiansen, Svein Martma, Tõnu Nehrke, Gernot 2015 application/pdf https://hdl.handle.net/11250/2994899 https://doi.org/10.1002/2014JC010320 eng eng Journal of Geophysical Research (JGR): Oceans. 2015, 120 (4), 2413-2429. urn:issn:2169-9275 https://hdl.handle.net/11250/2994899 https://doi.org/10.1002/2014JC010320 cristin:1250146 2413-2429 120 Journal of Geophysical Research (JGR): Oceans 4 Peer reviewed Journal article 2015 ftimr https://doi.org/10.1002/2014JC010320 2022-05-11T22:40:30Z In order to investigate the effect of glacial water on the CO2 system in the fjord, we studied the variability of the total alkalinity (AT), total dissolved inorganic carbon (CT), dissolved inorganic nutrients, oxygen isotopic ratio (δ18O), and freshwater fractions from the glacier front to the outer Tempelfjorden on Spitsbergen in winter 2012 (January, March, and April) and 2013 (April) and summer/fall 2013 (September). The two contrasting years clearly showed that the influence of freshwater, mixing, and haline convection affected the chemical and physical characteristics of the fjord. The seasonal variability showed the lowest calcium carbonate saturation state (Ω) and pH values in March 2012 coinciding with the highest freshwater fractions. The highest Ω and pH were found in September 2013, mostly due to CO2 uptake during primary production. Overall, we found that increased freshwater supply decreased Ω, pH, and AT. On the other hand, we observed higher AT relative to salinity in the freshwater end-member in the mild and rainy winter of 2012 (1142 μmol kg−1) compared to AT in 2013 (526 μmol kg−1). Observations of calcite and dolomite crystals in the glacial ice suggested supply of carbonate-rich glacial drainage water to the fjord. This implies that winters with a large amount of glacial drainage water partly provide a lessening of further ocean acidification, which will also affect the air-sea CO2 exchange. publishedVersion Article in Journal/Newspaper Arctic Ocean acidification Tempelfjord* Tempelfjorden Tidewater Spitsbergen Institute for Marine Research: Brage IMR Arctic Tempelfjorden ENVELOPE(17.076,17.076,78.404,78.404) Journal of Geophysical Research: Oceans 120 4 2413 2429
institution Open Polar
collection Institute for Marine Research: Brage IMR
op_collection_id ftimr
language English
description In order to investigate the effect of glacial water on the CO2 system in the fjord, we studied the variability of the total alkalinity (AT), total dissolved inorganic carbon (CT), dissolved inorganic nutrients, oxygen isotopic ratio (δ18O), and freshwater fractions from the glacier front to the outer Tempelfjorden on Spitsbergen in winter 2012 (January, March, and April) and 2013 (April) and summer/fall 2013 (September). The two contrasting years clearly showed that the influence of freshwater, mixing, and haline convection affected the chemical and physical characteristics of the fjord. The seasonal variability showed the lowest calcium carbonate saturation state (Ω) and pH values in March 2012 coinciding with the highest freshwater fractions. The highest Ω and pH were found in September 2013, mostly due to CO2 uptake during primary production. Overall, we found that increased freshwater supply decreased Ω, pH, and AT. On the other hand, we observed higher AT relative to salinity in the freshwater end-member in the mild and rainy winter of 2012 (1142 μmol kg−1) compared to AT in 2013 (526 μmol kg−1). Observations of calcite and dolomite crystals in the glacial ice suggested supply of carbonate-rich glacial drainage water to the fjord. This implies that winters with a large amount of glacial drainage water partly provide a lessening of further ocean acidification, which will also affect the air-sea CO2 exchange. publishedVersion
format Article in Journal/Newspaper
author Fransson, Agneta Ingrid
Chierici, Melissa
Nomura, Daiki
Granskog, Mats A.
Kristiansen, Svein
Martma, Tõnu
Nehrke, Gernot
spellingShingle Fransson, Agneta Ingrid
Chierici, Melissa
Nomura, Daiki
Granskog, Mats A.
Kristiansen, Svein
Martma, Tõnu
Nehrke, Gernot
Effect of glacial drainage water on the CO2 system and ocean acidification state in an Arctic tidewater-glacier fjord during two contrasting years
author_facet Fransson, Agneta Ingrid
Chierici, Melissa
Nomura, Daiki
Granskog, Mats A.
Kristiansen, Svein
Martma, Tõnu
Nehrke, Gernot
author_sort Fransson, Agneta Ingrid
title Effect of glacial drainage water on the CO2 system and ocean acidification state in an Arctic tidewater-glacier fjord during two contrasting years
title_short Effect of glacial drainage water on the CO2 system and ocean acidification state in an Arctic tidewater-glacier fjord during two contrasting years
title_full Effect of glacial drainage water on the CO2 system and ocean acidification state in an Arctic tidewater-glacier fjord during two contrasting years
title_fullStr Effect of glacial drainage water on the CO2 system and ocean acidification state in an Arctic tidewater-glacier fjord during two contrasting years
title_full_unstemmed Effect of glacial drainage water on the CO2 system and ocean acidification state in an Arctic tidewater-glacier fjord during two contrasting years
title_sort effect of glacial drainage water on the co2 system and ocean acidification state in an arctic tidewater-glacier fjord during two contrasting years
publishDate 2015
url https://hdl.handle.net/11250/2994899
https://doi.org/10.1002/2014JC010320
long_lat ENVELOPE(17.076,17.076,78.404,78.404)
geographic Arctic
Tempelfjorden
geographic_facet Arctic
Tempelfjorden
genre Arctic
Ocean acidification
Tempelfjord*
Tempelfjorden
Tidewater
Spitsbergen
genre_facet Arctic
Ocean acidification
Tempelfjord*
Tempelfjorden
Tidewater
Spitsbergen
op_source 2413-2429
120
Journal of Geophysical Research (JGR): Oceans
4
op_relation Journal of Geophysical Research (JGR): Oceans. 2015, 120 (4), 2413-2429.
urn:issn:2169-9275
https://hdl.handle.net/11250/2994899
https://doi.org/10.1002/2014JC010320
cristin:1250146
op_doi https://doi.org/10.1002/2014JC010320
container_title Journal of Geophysical Research: Oceans
container_volume 120
container_issue 4
container_start_page 2413
op_container_end_page 2429
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