Articles | Volume 11, issue 10
https://doi.org/10.5194/gmd-11-4291-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-11-4291-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Development and technical paper
| 
19 Oct 2018
Development and technical paper |
| 19 Oct 2018
| 19 Oct 2018
Dynamic hydrological discharge modelling for coupled climate model simulations of the last glacial cycle: the MPI-DynamicHD model version 3.0
Thomas Riddick
CORRESPONDING AUTHOR
Max Planck Institute for Meteorology, Bundesstraße 53, 20146 Hamburg, Germany
Victor Brovkin
Max Planck Institute for Meteorology, Bundesstraße 53, 20146 Hamburg, Germany
Stefan Hagemann
Max Planck Institute for Meteorology, Bundesstraße 53, 20146 Hamburg, Germany
now at: Institute of Coastal Research, Helmholtz-Zentrum Geesthacht, Max-Planck-Straße 1, 21502 Geesthacht, Germany
Uwe Mikolajewicz
Max Planck Institute for Meteorology, Bundesstraße 53, 20146 Hamburg, Germany
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Cited
16 citations as recorded by crossref.
- Sensitivity of Heinrich-type ice-sheet surge characteristics to boundary forcing perturbations C. Schannwell et al. 10.5194/cp-19-179-2023
- Dynamic interaction between lakes, climate, and vegetation across northern Africa during the mid-Holocene N. Specht et al. 10.5194/cp-20-1595-2024
- How the climate shapes stalagmites—A comparative study of model and speleothem at the Sofular Cave, Northern Turkey N. Merz et al. 10.3389/feart.2022.969211
- Glacial inception through rapid ice area increase driven by albedo and vegetation feedbacks M. Willeit et al. 10.5194/cp-20-597-2024
- The deglacial forest conundrum A. Dallmeyer et al. 10.1038/s41467-022-33646-6
- Computing water flow through complex landscapes – Part 3: Fill–Spill–Merge: flow routing in depression hierarchies R. Barnes et al. 10.5194/esurf-9-105-2021
- Interactive ocean bathymetry and coastlines for simulating the last deglaciation with the Max Planck Institute Earth System Model (MPI-ESM-v1.2) V. Meccia & U. Mikolajewicz 10.5194/gmd-11-4677-2018
- Analysis of the surface mass balance for deglacial climate simulations M. Kapsch et al. 10.5194/tc-15-1131-2021
- Modelling Mediterranean ocean biogeochemistry of the Last Glacial Maximum K. Six et al. 10.5194/cp-20-1785-2024
- A multi-model assessment of the early last deglaciation (PMIP4 LDv1): a meltwater perspective B. Snoll et al. 10.5194/cp-20-789-2024
- Towards spatio-temporal comparison of simulated and reconstructed sea surface temperatures for the last deglaciation N. Weitzel et al. 10.5194/cp-20-865-2024
- Computing water flow through complex landscapes – Part 1: Incorporating depressions in flow routing using FlowFill K. Callaghan & A. Wickert 10.5194/esurf-7-737-2019
- Terrestrial methane emissions from the Last Glacial Maximum to the preindustrial period T. Kleinen et al. 10.5194/cp-16-575-2020
- Ocean Response in Transient Simulations of the Last Deglaciation Dominated by Underlying Ice‐Sheet Reconstruction and Method of Meltwater Distribution M. Kapsch et al. 10.1029/2021GL096767
- Local oceanic CO<sub>2</sub> outgassing triggered by terrestrial carbon fluxes during deglacial flooding T. Extier et al. 10.5194/cp-18-273-2022
- Atmospheric methane since the last glacial maximum was driven by wetland sources T. Kleinen et al. 10.5194/cp-19-1081-2023
16 citations as recorded by crossref.
- Sensitivity of Heinrich-type ice-sheet surge characteristics to boundary forcing perturbations C. Schannwell et al. 10.5194/cp-19-179-2023
- Dynamic interaction between lakes, climate, and vegetation across northern Africa during the mid-Holocene N. Specht et al. 10.5194/cp-20-1595-2024
- How the climate shapes stalagmites—A comparative study of model and speleothem at the Sofular Cave, Northern Turkey N. Merz et al. 10.3389/feart.2022.969211
- Glacial inception through rapid ice area increase driven by albedo and vegetation feedbacks M. Willeit et al. 10.5194/cp-20-597-2024
- The deglacial forest conundrum A. Dallmeyer et al. 10.1038/s41467-022-33646-6
- Computing water flow through complex landscapes – Part 3: Fill–Spill–Merge: flow routing in depression hierarchies R. Barnes et al. 10.5194/esurf-9-105-2021
- Interactive ocean bathymetry and coastlines for simulating the last deglaciation with the Max Planck Institute Earth System Model (MPI-ESM-v1.2) V. Meccia & U. Mikolajewicz 10.5194/gmd-11-4677-2018
- Analysis of the surface mass balance for deglacial climate simulations M. Kapsch et al. 10.5194/tc-15-1131-2021
- Modelling Mediterranean ocean biogeochemistry of the Last Glacial Maximum K. Six et al. 10.5194/cp-20-1785-2024
- A multi-model assessment of the early last deglaciation (PMIP4 LDv1): a meltwater perspective B. Snoll et al. 10.5194/cp-20-789-2024
- Towards spatio-temporal comparison of simulated and reconstructed sea surface temperatures for the last deglaciation N. Weitzel et al. 10.5194/cp-20-865-2024
- Computing water flow through complex landscapes – Part 1: Incorporating depressions in flow routing using FlowFill K. Callaghan & A. Wickert 10.5194/esurf-7-737-2019
- Terrestrial methane emissions from the Last Glacial Maximum to the preindustrial period T. Kleinen et al. 10.5194/cp-16-575-2020
- Ocean Response in Transient Simulations of the Last Deglaciation Dominated by Underlying Ice‐Sheet Reconstruction and Method of Meltwater Distribution M. Kapsch et al. 10.1029/2021GL096767
- Local oceanic CO<sub>2</sub> outgassing triggered by terrestrial carbon fluxes during deglacial flooding T. Extier et al. 10.5194/cp-18-273-2022
- Atmospheric methane since the last glacial maximum was driven by wetland sources T. Kleinen et al. 10.5194/cp-19-1081-2023
Latest update: 23 Nov 2024
Short summary
During the Last Glacial Maximum, many rivers were blocked by the presence of large ice sheets and thus found new routes to the sea. This resulted in changes in the pattern of freshwater discharge into the oceans and thus would have significantly affected ocean circulation. Also, rivers found routes across the vast exposed continental shelves to the lower coastlines of that time. We propose a model for such changes in river routing suitable for use in wider models of the last glacial cycle.
During the Last Glacial Maximum, many rivers were blocked by the presence of large ice sheets...
