Articles | Volume 8, issue 7
https://doi.org/10.5194/gmd-8-2079-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/gmd-8-2079-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Methods for assessment of models
| Highlight paper
| 
16 Jul 2015
Methods for assessment of models | Highlight paper |
| 16 Jul 2015
14C-age tracers in global ocean circulation models
GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel, Kiel, Germany
H. Wagner
GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel, Kiel, Germany
P. Kähler
GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel, Kiel, Germany
A. Oschlies
GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel, Kiel, Germany
Viewed
Total article views: 7,729 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 24 Oct 2014)
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 5,420 | 2,064 | 245 | 7,729 | 250 | 255 |
- HTML: 5,420
- PDF: 2,064
- XML: 245
- Total: 7,729
- BibTeX: 250
- EndNote: 255
Total article views: 6,795 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 16 Jul 2015)
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 5,039 | 1,527 | 229 | 6,795 | 225 | 228 |
- HTML: 5,039
- PDF: 1,527
- XML: 229
- Total: 6,795
- BibTeX: 225
- EndNote: 228
Total article views: 934 (including HTML, PDF, and XML)
Cumulative views and downloads
(calculated since 24 Oct 2014)
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 381 | 537 | 16 | 934 | 25 | 27 |
- HTML: 381
- PDF: 537
- XML: 16
- Total: 934
- BibTeX: 25
- EndNote: 27
Cited
22 citations as recorded by crossref.
- On the Use of Dissolved Oxygen Isotopologues as Biogeochemical Tracers in the Northeast Pacific Ocean B. Li et al. 10.1029/2022JC018617
- Rejuvenating the ocean: mean ocean radiocarbon, CO2 release, and radiocarbon budget closure across the last deglaciation L. Skinner et al. 10.5194/cp-19-2177-2023
- Evaluation of the transport matrix method for simulation of ocean biogeochemical tracers K. Kvale et al. 10.5194/gmd-10-2425-2017
- Radium-226 in the global ocean as a tracer of thermohaline circulation: Synthesizing half a century of observations B. Xu et al. 10.1016/j.earscirev.2022.103956
- Flushing of the deep Pacific Ocean and the deglacial rise of atmospheric CO2 concentrations J. Du et al. 10.1038/s41561-018-0205-6
- Towards the construction of regional marine radiocarbon calibration curves: an unsupervised machine learning approach A. Mârza et al. 10.5194/gchron-6-503-2024
- Marine carbon sink dominated by biological pump after temperature overshoot W. Koeve et al. 10.1038/s41561-024-01541-y
- Marine Reservoir Age Variability Over the Last Deglaciation: Implications for Marine CarbonCycling and Prospects for Regional Radiocarbon Calibrations L. Skinner et al. 10.1029/2019PA003667
- Calcifying Phytoplankton Demonstrate an Enhanced Role in Greenhouse Atmospheric CO2 Regulation K. Kvale et al. 10.3389/fmars.2020.583989
- Disentangling magnetic and environmental signatures of sedimentary 10Be/9Be records T. Savranskaia et al. 10.1016/j.quascirev.2021.106809
- A year of transient tracers (chlorofluorocarbon 12 and sulfur hexafluoride), noble gases (helium and neon), and tritium in the Arctic Ocean from the MOSAiC expedition (2019–2020) C. Heuzé et al. 10.5194/essd-15-5517-2023
- Explicit silicate cycling in the Kiel Marine Biogeochemistry Model version 3 (KMBM3) embedded in the UVic ESCM version 2.9 K. Kvale et al. 10.5194/gmd-14-7255-2021
- Radiocarbon as a Dating Tool and Tracer in Paleoceanography L. Skinner & E. Bard 10.1029/2020RG000720
- Does Export Production Measure Transient Changes of the Biological Carbon Pump's Feedback to the Atmosphere Under Global Warming? W. Koeve et al. 10.1029/2020GL089928
- Decomposition of Deglacial Pacific Radiocarbon Age Controls Using an Isotope‐Enabled Ocean Model H. Zanowski et al. 10.1029/2021PA004363
- Holocene climate change and sea level oscillations in the pacific coast of Mexico D. Bocanegra-Ramírez et al. 10.1016/j.quaint.2019.01.003
- A Positive Cooling Feedback for the Neoproterozoic Snowball Earth Initiation Due To Weakening of Ocean Ventilation P. Liu et al. 10.1029/2022GL102020
- Young colonization history of a widespread sand dollar (Echinodermata; Clypeasteroida) in western Taiwan H. Lee et al. 10.1016/j.quaint.2018.12.003
- Recovery from microplastic-induced marine deoxygenation may take centuries K. Kvale & A. Oschlies 10.1038/s41561-022-01096-w
- Mechanisms of global ocean ventilation age change during the last deglaciation L. Li et al. 10.5194/cp-20-1161-2024
- Oxygen utilization rate (OUR) underestimates ocean respiration: A model study W. Koeve & P. Kähler 10.1002/2015GB005354
- Methods to evaluate CaCO<sub>3</sub> cycle modules in coupled global biogeochemical ocean models W. Koeve et al. 10.5194/gmd-7-2393-2014
21 citations as recorded by crossref.
- On the Use of Dissolved Oxygen Isotopologues as Biogeochemical Tracers in the Northeast Pacific Ocean B. Li et al. 10.1029/2022JC018617
- Rejuvenating the ocean: mean ocean radiocarbon, CO2 release, and radiocarbon budget closure across the last deglaciation L. Skinner et al. 10.5194/cp-19-2177-2023
- Evaluation of the transport matrix method for simulation of ocean biogeochemical tracers K. Kvale et al. 10.5194/gmd-10-2425-2017
- Radium-226 in the global ocean as a tracer of thermohaline circulation: Synthesizing half a century of observations B. Xu et al. 10.1016/j.earscirev.2022.103956
- Flushing of the deep Pacific Ocean and the deglacial rise of atmospheric CO2 concentrations J. Du et al. 10.1038/s41561-018-0205-6
- Towards the construction of regional marine radiocarbon calibration curves: an unsupervised machine learning approach A. Mârza et al. 10.5194/gchron-6-503-2024
- Marine carbon sink dominated by biological pump after temperature overshoot W. Koeve et al. 10.1038/s41561-024-01541-y
- Marine Reservoir Age Variability Over the Last Deglaciation: Implications for Marine CarbonCycling and Prospects for Regional Radiocarbon Calibrations L. Skinner et al. 10.1029/2019PA003667
- Calcifying Phytoplankton Demonstrate an Enhanced Role in Greenhouse Atmospheric CO2 Regulation K. Kvale et al. 10.3389/fmars.2020.583989
- Disentangling magnetic and environmental signatures of sedimentary 10Be/9Be records T. Savranskaia et al. 10.1016/j.quascirev.2021.106809
- A year of transient tracers (chlorofluorocarbon 12 and sulfur hexafluoride), noble gases (helium and neon), and tritium in the Arctic Ocean from the MOSAiC expedition (2019–2020) C. Heuzé et al. 10.5194/essd-15-5517-2023
- Explicit silicate cycling in the Kiel Marine Biogeochemistry Model version 3 (KMBM3) embedded in the UVic ESCM version 2.9 K. Kvale et al. 10.5194/gmd-14-7255-2021
- Radiocarbon as a Dating Tool and Tracer in Paleoceanography L. Skinner & E. Bard 10.1029/2020RG000720
- Does Export Production Measure Transient Changes of the Biological Carbon Pump's Feedback to the Atmosphere Under Global Warming? W. Koeve et al. 10.1029/2020GL089928
- Decomposition of Deglacial Pacific Radiocarbon Age Controls Using an Isotope‐Enabled Ocean Model H. Zanowski et al. 10.1029/2021PA004363
- Holocene climate change and sea level oscillations in the pacific coast of Mexico D. Bocanegra-Ramírez et al. 10.1016/j.quaint.2019.01.003
- A Positive Cooling Feedback for the Neoproterozoic Snowball Earth Initiation Due To Weakening of Ocean Ventilation P. Liu et al. 10.1029/2022GL102020
- Young colonization history of a widespread sand dollar (Echinodermata; Clypeasteroida) in western Taiwan H. Lee et al. 10.1016/j.quaint.2018.12.003
- Recovery from microplastic-induced marine deoxygenation may take centuries K. Kvale & A. Oschlies 10.1038/s41561-022-01096-w
- Mechanisms of global ocean ventilation age change during the last deglaciation L. Li et al. 10.5194/cp-20-1161-2024
- Oxygen utilization rate (OUR) underestimates ocean respiration: A model study W. Koeve & P. Kähler 10.1002/2015GB005354
1 citations as recorded by crossref.
Saved (final revised paper)
Saved (preprint)
Latest update: 26 Dec 2024
Short summary
The natural abundance of 14C in CO2 dissolved in seawater is often used to evaluate circulation and age in the ocean and in ocean models. We study limitations of using natural 14C to determine the time elapsed since water had contact with the atmosphere. We find that, globally, bulk 14C age is dominated by two equally important components, (1) the time component of circulation and (2) the “preformed 14C-age”. Considering preformed 14C-age is critical for an assessment of circulation in models.
The natural abundance of 14C in CO2 dissolved in seawater is often used to evaluate circulation...
