Articles | Volume 15, issue 1
https://doi.org/10.5194/bg-15-51-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-15-51-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
03 Jan 2018
Research article |
| 03 Jan 2018
Inorganic carbon and water masses in the Irminger Sea since 1991
Geophysical Institute, University of Bergen, 5007 Bergen, Norway
Bjerknes Centre for Climate Research, 5007 Bergen, Norway
Geophysical Institute, University of Bergen, 5007 Bergen, Norway
Bjerknes Centre for Climate Research, 5007 Bergen, Norway
Fiz F. Pérez
Instituto de Investigaciones Marinas (IIM-CSIC), 36208 Vigo, Spain
Maribel I. García-Ibáñez
Uni Research Climate, Bjerknes Centre for Climate Research, 5008 Bergen, Norway
Emil Jeansson
Uni Research Climate, Bjerknes Centre for Climate Research, 5008 Bergen, Norway
Abdirahman Omar
Uni Research Climate, Bjerknes Centre for Climate Research, 5008 Bergen, Norway
Siv K. Lauvset
Uni Research Climate, Bjerknes Centre for Climate Research, 5008 Bergen, Norway
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Cited
15 citations as recorded by crossref.
- Arrival of New Great Salinity Anomaly Weakens Convection in the Irminger Sea T. Biló et al. 10.1029/2022GL098857
- Impact of physical and biological processes on temporal variations of the ocean carbon sink in the mid-latitude North Atlantic (2002–2016) V. Macovei et al. 10.1016/j.pocean.2019.102223
- Introduction to the French GEOTRACES North Atlantic Transect (GA01): GEOVIDE cruise G. Sarthou et al. 10.5194/bg-15-7097-2018
- ECOSMO II(CHL): a marine biogeochemical model for the North Atlantic and the Arctic V. Yumruktepe et al. 10.5194/gmd-15-3901-2022
- Cold-water corals in the Subpolar North Atlantic Ocean exposed to aragonite undersaturation if the 2 °C global warming target is not met M. García-Ibáñez et al. 10.1016/j.gloplacha.2021.103480
- Decadal Trends in the Oceanic Storage of Anthropogenic Carbon From 1994 to 2014 J. Müller et al. 10.1029/2023AV000875
- GLODAPv2.2019 – an update of GLODAPv2 A. Olsen et al. 10.5194/essd-11-1437-2019
- SURATLANT: a 1993–2017 surface sampling in the central part of the North Atlantic subpolar gyre G. Reverdin et al. 10.5194/essd-10-1901-2018
- Trends of Anthropogenic Dissolved Inorganic Carbon in the Northwest Atlantic Ocean Estimated Using a State Space Model C. Boteler et al. 10.1029/2022JC019483
- Anthropogenic CO2 and ocean acidification in Argentine Basin Water Masses over almost five decades of observations M. Fontela et al. 10.1016/j.scitotenv.2021.146570
- Ocean carbonate system variability in the North Atlantic Subpolar surface water (1993–2017) C. Leseurre et al. 10.5194/bg-17-2553-2020
- Overflow waters in the western Irminger Sea modify deep sound speed structure and convergence zone propagation E. Bhatt et al. 10.1121/10.0024350
- Environmental Change at Deep-Sea Sponge Habitats Over the Last Half Century: A Model Hindcast Study for the Age of Anthropogenic Climate Change A. Samuelsen et al. 10.3389/fmars.2022.737164
- Anthropogenic carbon pathways towards the North Atlantic interior revealed by Argo-O2, neural networks and back-calculations R. Asselot et al. 10.1038/s41467-024-46074-5
- Can Empirical Algorithms Successfully Estimate Aragonite Saturation State in the Subpolar North Atlantic? D. Turk et al. 10.3389/fmars.2017.00385
14 citations as recorded by crossref.
- Arrival of New Great Salinity Anomaly Weakens Convection in the Irminger Sea T. Biló et al. 10.1029/2022GL098857
- Impact of physical and biological processes on temporal variations of the ocean carbon sink in the mid-latitude North Atlantic (2002–2016) V. Macovei et al. 10.1016/j.pocean.2019.102223
- Introduction to the French GEOTRACES North Atlantic Transect (GA01): GEOVIDE cruise G. Sarthou et al. 10.5194/bg-15-7097-2018
- ECOSMO II(CHL): a marine biogeochemical model for the North Atlantic and the Arctic V. Yumruktepe et al. 10.5194/gmd-15-3901-2022
- Cold-water corals in the Subpolar North Atlantic Ocean exposed to aragonite undersaturation if the 2 °C global warming target is not met M. García-Ibáñez et al. 10.1016/j.gloplacha.2021.103480
- Decadal Trends in the Oceanic Storage of Anthropogenic Carbon From 1994 to 2014 J. Müller et al. 10.1029/2023AV000875
- GLODAPv2.2019 – an update of GLODAPv2 A. Olsen et al. 10.5194/essd-11-1437-2019
- SURATLANT: a 1993–2017 surface sampling in the central part of the North Atlantic subpolar gyre G. Reverdin et al. 10.5194/essd-10-1901-2018
- Trends of Anthropogenic Dissolved Inorganic Carbon in the Northwest Atlantic Ocean Estimated Using a State Space Model C. Boteler et al. 10.1029/2022JC019483
- Anthropogenic CO2 and ocean acidification in Argentine Basin Water Masses over almost five decades of observations M. Fontela et al. 10.1016/j.scitotenv.2021.146570
- Ocean carbonate system variability in the North Atlantic Subpolar surface water (1993–2017) C. Leseurre et al. 10.5194/bg-17-2553-2020
- Overflow waters in the western Irminger Sea modify deep sound speed structure and convergence zone propagation E. Bhatt et al. 10.1121/10.0024350
- Environmental Change at Deep-Sea Sponge Habitats Over the Last Half Century: A Model Hindcast Study for the Age of Anthropogenic Climate Change A. Samuelsen et al. 10.3389/fmars.2022.737164
- Anthropogenic carbon pathways towards the North Atlantic interior revealed by Argo-O2, neural networks and back-calculations R. Asselot et al. 10.1038/s41467-024-46074-5
1 citations as recorded by crossref.
Latest update: 23 Nov 2024
Short summary
On long timescales, the inventory of total dissolved inorganic carbon in the ocean is mainly driven by the increase in anthropogenic CO2 emitted to the atmosphere due to human activities. On short timescales, however, the anthropogenic signal can be masked by the variability in natural inorganic carbon, shown in this study based on Irminger Sea cruise data from 1991 to 2015. In order to estimate oceanic carbon budgets, we suggest jointly assessing natural, anthropogenic and total carbon.
On long timescales, the inventory of total dissolved inorganic carbon in the ocean is mainly...
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