PalMod2 MPI-M MPI-ESM1-2-CR-CH4 transient-deglaciation-prescribed-glac1d-methane

doi:10.26050/WDCC/PMMXMCHTD

Kleinen, Thomas et al.

Dataset GroupDOI
Summary
For transient-deglaciation-prescribed-glac1d-methane (r1i1p1f1):
The transient experiment was performed with the Max Planck Institute for Meteorology Earth System Model version 1.2 in coarse resolution (MPI-ESM-CR). The model includes the spectral atmospheric model ECHAM6.3 at T31 horizontal resolution (approx. 3.75°) and 31 vertical levels, the land surface vegetation model JSBACH3.2, and the primitive equation ocean model MPIOM1.6 with a nominal resolution of 3°. The model has been extended with a full methane cycle, including a simplified atmospheric chemistry, as described in Kleinen et al. (2020), Kleinen et al. (2021) and Kleinen et al. (2022).
For the experiment, the model was integrated from a glacial state at 23 ka to the year 1950 with prescribed atmospheric greenhouse gas concentrations (Köhler et al., 2017) and insolation (Berger & Loutre, 1991). Ice sheets and surface topographies were prescribed from GLAC-1D (Tarasov et al., 2012) reconstructions. All forcing fields are updated every 10 years of the simulations and initiate changes in the topography, glacier mask, river pathways, ocean bathymetry, and land-sea mask.
For transient-deglaciation-prescribed-glac1d-methane (r1i1p1f2):
This experiment is derived from the r1i1p1f1 experiment. It is branched off at 18 ka BP, and starting at 15.2 ka BP, meltwater from the Laurentide ice sheet was removed from the system and stored. The accumulated meltwater was released over a period of 1200 years starting at 12.8 ka BP. This induced a collapse of the AMOC, leading to climatic conditions very similar to the Younger Dryas cold period seen in climate reconstructions. After the end of the meltwater release, the circulation recovered quickly and climatic conditions converged with the r1i1p1f1 experiment.
Important:
Please be aware that due to CMORization constraints data set time values concerning to "Before Present(BP)" time got a year offset (+25001). Means for example year range 2001 to 25000 model time is equal to 23000 to 1 BP.
Project
PalMod2 (PalMod2)
Contact
Dr. Thomas Kleinen (
 thomas.kleinen@nullmpimet.mpg.de
0000-0001-9550-5164)

Dr. Victor Brovkin (
 victor.brovkin@nullmpimet.mpg.de
0000-0001-6420-3198)
Location(s)
global
Spatial Coverage
Longitude 0 to 356.25 Latitude -89.5 to 89.5
Temporal Coverage
2001-01-01 to 25000-12-31 (model time, 365 days per year)
Use constraints
Creative Commons Attribution 4.0 International (CC BY 4.0) (https://creativecommons.org/licenses/by/4.0/)
Data Catalog
World Data Center for Climate
Size
1.33 TiB (1459290827555 Byte)
Format
NetCDF
Status
completely archived
Creation Date
Future Review Date
2033-02-01
Cite as
Kleinen, Thomas; Gromov, Sergey; Steil, Benedikt; Brovkin, Victor (2023). PalMod2 MPI-M MPI-ESM1-2-CR-CH4 transient-deglaciation-prescribed-glac1d-methane. World Data Center for Climate (WDCC) at DKRZ. https://doi.org/10.26050/WDCC/PMMXMCHTD

BibTeX RIS
Funding
Description
as consistent as the model(s) MPI-ESM1-2-CR-CH4
Description
Summary:
Findable: 6 of 7 level;
Accessible: 2 of 3 level;
Interoperable: 3 of 4 level;
Reusable: 4 of 10 level
Method
F-UJI online v2.2.5 automated
Method Description
Checks performed by WDCC. Metrics documentation: https://doi.org/10.5281/zenodo.4081213 Metric Version: metrics_v0.5
Method Url
Result Date
2023-04-12
Result Date
2023-03-16
Description
1. Number of data sets is correct and > 0: passed;
2. Size of every data set is > 0: passed;
3. The data sets and corresponding metadata are accessible: passed;
4. The data sizes are controlled and correct: passed;
5. The spatial-temporal coverage description (metadata) is consistent to the data: passed;
6. The format is correct: passed;
7. Variable description and data are consistent: passed
Method
WDCC-TQA checklist
Method Description
Checks performed by WDCC. The list of TQA metrics are documented in the 'WDCC User Guide for Data Publication' Chapter 8.1.1
Method Url
Result Date
2023-03-16
Contact typePersonORCIDOrganization
-
-

References

[1] DOI Mauritsen, Thorsten; Bader, Jürgen; Becker, Tobias; Behrens, Jörg; Bittner, Matthias; Brokopf, Renate; Brovkin, Victor; Claussen, Martin; Crueger, Traute; Esch, Monika; Fast, Irina; Fiedler, Stephanie; Fläschner, Dagmar; Gayler, Veronika; Giorgetta, Marco; Goll, Daniel S.; Haak, Helmuth; Hagemann, Stefan; Hedemann, Christopher; Hohenegger, Cathy; Ilyina, Tatiana; Jahns, Thomas; Jimenéz‐de‐la‐Cuesta, Diego; Jungclaus, Johann; Kleinen, Thomas; Kloster, Silvia; Kracher, Daniela; Kinne, Stefan; Kleberg, Deike; Lasslop, Gitta; Kornblueh, Luis; Marotzke, Jochem; Matei, Daniela; Meraner, Katharina; Mikolajewicz, Uwe; Modali, Kameswarrao; Möbis, Benjamin; Müller, Wolfgang A.; Nabel, Julia E. M. S.; Nam, Christine C. W.; Notz, Dirk; Nyawira, Sarah‐Sylvia; Paulsen, Hanna; Peters, Karsten; Pincus, Robert; Pohlmann, Holger; Pongratz, Julia; Popp, Max; Raddatz, Thomas Jürgen; Rast, Sebastian; Redler, Rene; Reick, Christian H.; Rohrschneider, Tim; Schemann, Vera; Schmidt, Hauke; Schnur, Reiner; Schulzweida, Uwe; Six, Katharina D.; Stein, Lukas; Stemmler, Irene; Stevens, Bjorn; Storch, Jin‐Song; Tian, Fangxing; Voigt, Aiko; Vrese, Philipp; Wieners, Karl‐Hermann; Wilkenskjeld, Stiig; Winkler, Alexander; Roeckner, Erich. (2019). Developments in the MPI-M Earth System Model version 1.2 (MPI-ESM1.2) and Its Response to Increasing CO2. doi:10.1029/2018ms001400
[2] DOI Müller, W. A.; Jungclaus, J. H.; Mauritsen, T.; Baehr, J.; Bittner, M.; Budich, R.; Bunzel, F.; Esch, M.; Ghosh, R.; Haak, H.; Ilyina, T.; Kleine, T.; Kornblueh, L.; Li, H.; Modali, K.; Notz, D.; Pohlmann, H.; Roeckner, E.; Stemmler, I.; Tian, F.; Marotzke, J. (2018). A Higher‐resolution Version of the Max Planck Institute Earth System Model (MPI‐ESM1.2‐HR). doi:10.1029/2017ms001217
[3] DOI Kleinen, T.; Gromov, S.; Steil, B.; Brovkin, V. (2022). Atmospheric methane since the LGM was driven by wetland sources. doi:10.5194/cp-2022-80
[4] DOI Kleinen, T.; Mikolajewicz, U.; Brovkin, V. (2020). Terrestrial methane emissions from the Last Glacial Maximum to the preindustrial period. doi:10.5194/cp-16-575-2020
[5] DOI Kleinen, T.; Gromov, S.; Steil, B.; Brovkin, V. (2021). Atmospheric methane underestimated in future climate projections. doi:10.1088/1748-9326/ac1814
[6] DOI Kapsch, Marie‐Luise; Mikolajewicz, Uwe; Ziemen, Florian; Schannwell, Clemens. (2022). Ocean Response in Transient Simulations of the Last Deglaciation Dominated by Underlying Ice‐Sheet Reconstruction and Method of Meltwater Distribution. doi:10.1029/2021gl096767
[7] DOI Meccia, Virna Loana; Mikolajewicz, Uwe. (2018). Interactive ocean bathymetry and coastlines for simulating the last deglaciation with the Max Planck Institute Earth System Model (MPI-ESM-v1.2). doi:10.5194/gmd-11-4677-2018
[8] DOI Riddick, Thomas; Brovkin, Victor; Hagemann, Stefan; Mikolajewicz, Uwe. (2018). Dynamic hydrological discharge modelling for coupled climate model simulations of the last glacial cycle: the MPI-DynamicHD model version 3.0. doi:10.5194/gmd-11-4291-2018

Is documented by

[1] DOI Köhler, Peter; Nehrbass-Ahles, Christoph; Schmitt, Jochen; Stocker, Thomas F.; Fischer, Hubertus. (2017). A 156 kyr smoothed history of the atmospheric greenhouse gases CO2, CH4 and N2O and their radiative forcing. doi:10.5194/essd-9-363-2017
[2] DOI Berger, A.; Loutre, M.F. (1991). Insolation values for the climate of the last 10 million years. doi:10.1016/0277-3791(91)90033-q
[3] DOI Tarasov, Lev; Dyke, Arthur S.; Neal, Radford M.; Peltier, W.R. (2012). A data-calibrated distribution of deglacial chronologies for the North American ice complex from glaciological modeling. doi:10.1016/j.epsl.2011.09.010

Parent

PalMod2 MPI-M MPI-ESM1-2-CR-CH4
Details

Attached Datasets ( 222 )

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Parent project(s)

PalMod2

[Entry acronym: PMMXMCHTD] [Entry id: 3967402]