Articles | Volume 6, issue 2
https://doi.org/10.5194/gmd-6-477-2013
© Author(s) 2013. 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-6-477-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Model description paper
| 
12 Apr 2013
Model description paper |
| 12 Apr 2013
MESMO 2: a mechanistic marine silica cycle and coupling to a simple terrestrial scheme
K. Matsumoto
Department of Earth Sciences, University of Minnesota, Minneapolis, Minnesota, USA
K. Tokos
University of California, Santa Cruz, California, USA
A. Huston
University of California, Santa Cruz, California, USA
H. Joy-Warren
University of Chicago, Chicago, Illinois, USA
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Cited
20 citations as recorded by crossref.
- Simulating the modern δ30Si distribution in the oceans and in marine sediments S. Gao et al. 10.1002/2015GB005189
- Buffering of Ocean Export Production by Flexible Elemental Stoichiometry of Particulate Organic Matter T. Tanioka & K. Matsumoto 10.1002/2017GB005670
- The influence of water mass mixing on the dissolved Si isotope composition in the Eastern Equatorial Pacific P. Grasse et al. 10.1016/j.epsl.2013.07.033
- Controls on biogenic silica burial in the Southern Ocean Z. Chase et al. 10.1002/2015GB005186
- Shifts in regional production as a driver of future global ocean production stoichiometry K. Matsumoto & T. Tanioka 10.1088/1748-9326/abc4b0
- Controls on the silicon isotope distribution in the ocean: New diagnostics from a data‐constrained model M. Holzer & M. Brzezinski 10.1002/2014GB004967
- MESMO 3: Flexible phytoplankton stoichiometry and refractory dissolved organic matter K. Matsumoto et al. 10.5194/gmd-14-2265-2021
- Southern-ocean and glaciogenic nutrients control diatom export production on the Chile margin Z. Chase et al. 10.1016/j.quascirev.2014.06.015
- Sensitivity of Steady State, Deep Ocean Dissolved Organic Carbon to Surface Boundary Conditions K. Matsumoto et al. 10.1029/2021GB007102
- Diatom Physiology Controls Silicic Acid Leakage in Response to Iron Fertilization M. Holzer et al. 10.1029/2019GB006460
- Dynamics of the Marine Dissolved Organic Carbon Reservoir in Glacial Climate Simulations: The Importance of Biological Production M. Gilchrist & K. Matsumoto 10.1029/2022PA004522
- Atmospheric 14 C/ 12 C changes during the last glacial period from Hulu Cave H. Cheng et al. 10.1126/science.aau0747
- Reviews and syntheses: The biogeochemical cycle of silicon in the modern ocean P. Tréguer et al. 10.5194/bg-18-1269-2021
- How well do global ocean biogeochemistry models simulate dissolved iron distributions? A. Tagliabue et al. 10.1002/2015GB005289
- Linkages Between Dynamic Phytoplankton C:N:P and the Ocean Carbon Cycle Under Climate Change K. Matsumoto et al. 10.5670/oceanog.2020.203
- Different mechanisms of silicic acid leakage and their biogeochemical consequences K. Matsumoto et al. 10.1002/2013PA002588
- Carbon Export Buffering and CO2 Drawdown by Flexible Phytoplankton C:N:P Under Glacial Conditions K. Matsumoto et al. 10.1029/2019PA003823
- Inverse-model estimates of the ocean's coupled phosphorus, silicon, and iron cycles B. Pasquier & M. Holzer 10.5194/bg-14-4125-2017
- Coupled climate–carbon cycle simulation of the Last Glacial Maximum atmospheric CO<sub>2</sub> decrease using a large ensemble of modern plausible parameter sets K. Kemppinen et al. 10.5194/cp-15-1039-2019
- Coupling of the distribution of silicon isotopes to the meridional overturning circulation of the North Atlantic Ocean M. Brzezinski & J. Jones 10.1016/j.dsr2.2014.11.015
19 citations as recorded by crossref.
- Simulating the modern δ30Si distribution in the oceans and in marine sediments S. Gao et al. 10.1002/2015GB005189
- Buffering of Ocean Export Production by Flexible Elemental Stoichiometry of Particulate Organic Matter T. Tanioka & K. Matsumoto 10.1002/2017GB005670
- The influence of water mass mixing on the dissolved Si isotope composition in the Eastern Equatorial Pacific P. Grasse et al. 10.1016/j.epsl.2013.07.033
- Controls on biogenic silica burial in the Southern Ocean Z. Chase et al. 10.1002/2015GB005186
- Shifts in regional production as a driver of future global ocean production stoichiometry K. Matsumoto & T. Tanioka 10.1088/1748-9326/abc4b0
- Controls on the silicon isotope distribution in the ocean: New diagnostics from a data‐constrained model M. Holzer & M. Brzezinski 10.1002/2014GB004967
- MESMO 3: Flexible phytoplankton stoichiometry and refractory dissolved organic matter K. Matsumoto et al. 10.5194/gmd-14-2265-2021
- Southern-ocean and glaciogenic nutrients control diatom export production on the Chile margin Z. Chase et al. 10.1016/j.quascirev.2014.06.015
- Sensitivity of Steady State, Deep Ocean Dissolved Organic Carbon to Surface Boundary Conditions K. Matsumoto et al. 10.1029/2021GB007102
- Diatom Physiology Controls Silicic Acid Leakage in Response to Iron Fertilization M. Holzer et al. 10.1029/2019GB006460
- Dynamics of the Marine Dissolved Organic Carbon Reservoir in Glacial Climate Simulations: The Importance of Biological Production M. Gilchrist & K. Matsumoto 10.1029/2022PA004522
- Atmospheric 14 C/ 12 C changes during the last glacial period from Hulu Cave H. Cheng et al. 10.1126/science.aau0747
- Reviews and syntheses: The biogeochemical cycle of silicon in the modern ocean P. Tréguer et al. 10.5194/bg-18-1269-2021
- How well do global ocean biogeochemistry models simulate dissolved iron distributions? A. Tagliabue et al. 10.1002/2015GB005289
- Linkages Between Dynamic Phytoplankton C:N:P and the Ocean Carbon Cycle Under Climate Change K. Matsumoto et al. 10.5670/oceanog.2020.203
- Different mechanisms of silicic acid leakage and their biogeochemical consequences K. Matsumoto et al. 10.1002/2013PA002588
- Carbon Export Buffering and CO2 Drawdown by Flexible Phytoplankton C:N:P Under Glacial Conditions K. Matsumoto et al. 10.1029/2019PA003823
- Inverse-model estimates of the ocean's coupled phosphorus, silicon, and iron cycles B. Pasquier & M. Holzer 10.5194/bg-14-4125-2017
- Coupled climate–carbon cycle simulation of the Last Glacial Maximum atmospheric CO<sub>2</sub> decrease using a large ensemble of modern plausible parameter sets K. Kemppinen et al. 10.5194/cp-15-1039-2019
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