exp_design:degla

Differences

This shows you the differences between two versions of the page.

Link to this comparison view

Both sides previous revision Previous revision
Next revision
Previous revision
exp_design:degla [2016/07/12 15:17]
jypeter [References cited] Added clickable links for the DOI cited
exp_design:degla [2019/02/25 15:36] (current)
jypeter Updated references
Line 19: Line 19:
 ==== Associated publications ==== ==== Associated publications ====
  
-**Last deglaciation experiment design, version 1:**\\ +**Transient climate simulations of the deglaciation 21–9 thousand years before present (version 1) – PMIP4 Core experiment design and boundary conditions**Ivanovic, R. F.Gregoire, L. J.Kageyama, M.Roche, D. M.Valdes, P. J.Burke, A.Drummond, R.Peltier, W. R.and Tarasov, L., Geosci. Model Dev., 92563-2587, [[https://doi.org/10.5194/gmd-9-2563-2016|doi:10.5194/gmd-9-2563-2016]], 2016.
-Ivanovic, R. F.Gregoire, L. J.Kageyama, M.Roche, D. M.Valdes, P. J.Burke, A.Drummond, R.Peltier, W. R. and Tarasov, L.: Transient climate simulations of the deglaciation 21–9 thousand years before present, version 1; PMIP4 Core experiment design and boundary conditions, Geosci. Model Dev. Discuss., 89045-9102doi:[[http://www.geosci-model-dev-discuss.net/gmd-2015-215/|10.5194/gmdd-8-9045-2015]], 2015\\  +
-\\+
  
 ===== Version 1 Specifications ===== ===== Version 1 Specifications =====
-For general advice on boundary condition implementation in palaeoclimate models, see [[#References_cited|Kageyama et al. (2016)]].+ 
 +For general advice on boundary condition implementation in palaeoclimate models, see [[#References_cited|Kageyama et al. (2018)]].
  
 ==== Last Glacial Maximum spinup (21 ka) ==== ==== Last Glacial Maximum spinup (21 ka) ====
 +
 This spinup simulation is compatible with the PMIP4-CMIP6 LGM experiment, which can also be used as the initialisation state for the fully transient run from 21 ka onwards, provided the ICE-6G_C or GLAC-1D ice sheet reconstructions and associated boundary conditions (orography, coastlines and bathymetry) were used. This spinup simulation is compatible with the PMIP4-CMIP6 LGM experiment, which can also be used as the initialisation state for the fully transient run from 21 ka onwards, provided the ICE-6G_C or GLAC-1D ice sheet reconstructions and associated boundary conditions (orography, coastlines and bathymetry) were used.
 +
 ^      ^PMIP4 specifications ^  ^      ^PMIP4 specifications ^ 
 | PMIP4 name | <wrap em>LDv1-LGMspin</wrap> | | PMIP4 name | <wrap em>LDv1-LGMspin</wrap> |
Line 33: Line 34:
 | Solar constant | 1361.0 ± 0.51365 W m<sup>-2</sup>  | Solar constant | 1361.0 ± 0.51365 W m<sup>-2</sup> 
 | Trace gases  | **CO<sub>2</sub>** = 190 ppm \\ **CH<sub>4</sub>** = 375 ppb \\ **N<sub>2</sub>O** = 200 ppb \\ **CFC** = 0 \\ **O<sub>3</sub>** = Preindustrial (e.g. 10 DU)  |  | Trace gases  | **CO<sub>2</sub>** = 190 ppm \\ **CH<sub>4</sub>** = 375 ppb \\ **N<sub>2</sub>O** = 200 ppb \\ **CFC** = 0 \\ **O<sub>3</sub>** = Preindustrial (e.g. 10 DU)  | 
-| Ice sheets, orography \\ and coastlines  | 21 ka data from either \\ - ICE-6G_C reconstruction [[:data:ice|[Access to data]]] \\ - GLAC-1D reconstruction [[:data:ice|[Access to data]]]| +| Ice sheets, orography \\ and coastlines  | 21 ka data from either \\ - ICE-6G_C reconstruction: [ [[:data:ice|Access to data]] ] \\ - GLAC-1D reconstruction: [ [[:data:ice|Access to data]] ]| 
 | Bathymetry  | Keep consistent with the coastlines, using either: \\ - Data associated with the ice sheet \\ - Preindustrial bathymetry |  | Bathymetry  | Keep consistent with the coastlines, using either: \\ - Data associated with the ice sheet \\ - Preindustrial bathymetry | 
 | Global ocean salinity | + 1 psu, relative to preindustrial  | | Global ocean salinity | + 1 psu, relative to preindustrial  |
Line 39: Line 40:
  
 ==== Transient orbit and trace gases spinup (26-21 ka) ==== ==== Transient orbit and trace gases spinup (26-21 ka) ====
 +
 This option for spinning-up the last deglaciation simulation uses transient orbital parameters and trace gases from 26-21 ka. This option for spinning-up the last deglaciation simulation uses transient orbital parameters and trace gases from 26-21 ka.
 ^      ^PMIP4 specifications ^  ^      ^PMIP4 specifications ^ 
 | PMIP4 name | <wrap em>LDv1-transpin</wrap> | | PMIP4 name | <wrap em>LDv1-transpin</wrap> |
-| Astronomical parameters  | All orbital parameters should be transient as per [[#References_cited|Berger (1978)]] 26-21 ka  [[ftp://ftp.ncdc.noaa.gov/pub/data/paleo/insolation/bein1.dat|[Access to data]]]|   +| Astronomical parameters  | All orbital parameters should be transient as per [[#References_cited|Berger (1978)]] 26-21 ka\\ [ [[ftp://ftp.ncdc.noaa.gov/pub/data/paleo/climate_forcing/orbital_variations/insolation/bein1.dat|Access to data]] **&** [[ftp://ftp.ncdc.noaa.gov/pub/data/paleo/climate_forcing/orbital_variations/insolation/readme_insolation.txt|README !]] ]|   
-| Trace gases  | All adjusted to the AICC2012 chronology [[#References_cited|Veres et al. (2013)]] 26-21 ka: \\ **CO<sub>2</sub>** = Transient, as per [[#References_cited|Bereiter et al. (2015)]] [[ftp://ftp.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/antarctica2015co2composite.txt|[Access to data]]] \\ **CH<sub>4</sub>** = Transient, as per [[#References_cited|Loulergue et al. (2008)]] \\ **N<sub>2</sub>O** = Transient, as per [[#References_cited|Schilt et al. (2010)]] \\  |  +| Trace gases  | All adjusted to the AICC2012 chronology [[#References_cited|Veres et al. (2013)]] 26-21 ka: \\ **CO<sub>2</sub>** = Transient, as per [[#References_cited|Bereiter et al. (2015)]]: [ [[ftp://ftp.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/antarctica2015co2composite.txt|Access to data]] (md5sum = ''c54a033d8cbf588bc2b95d3b92ff9b1c''] \\ **CH<sub>4</sub>** = Transient, as per [[#References_cited|Loulergue et al. (2008)]]: [ [[data:gases#loulergue_et_al_ch4_data|Access to data]] ] \\ **N<sub>2</sub>O** = Transient, as per [[#References_cited|Schilt et al. (2010)]]: [ [[data:gases#schilt_et_al_n20_data|Access to data]] ]  |  
-| All others  | As per the LGM (21 ka) spinup type; LDv1-LGMspin | +//All others// | As per the LGM (21 ka) spinup type; LDv1-LGMspin | 
  
 ==== Transient deglaciation (21-0 ka) ==== ==== Transient deglaciation (21-0 ka) ====
 +
 These are the specifications for the full transient run 21-0 ka. \\ These are the specifications for the full transient run 21-0 ka. \\
 (Note, the period of focus for version 1 of the experiment is 21-9 ka, but all boundary conditions are provided until 0 ka so that groups can extend the run to present if they wish). (Note, the period of focus for version 1 of the experiment is 21-9 ka, but all boundary conditions are provided until 0 ka so that groups can extend the run to present if they wish).
 +
 ^      ^PMIP4 specifications ^  ^      ^PMIP4 specifications ^ 
 | PMIP4 name | <wrap em>LDv1</wrap> | | PMIP4 name | <wrap em>LDv1</wrap> |
 | Initial conditions (pre 21 ka) | Recommended (optional) to use either: \\ - LDv1-LGMspin \\ - LDv1-transpin \\ See above for details. The method must be documented, including information on the state of spinup  |   | Initial conditions (pre 21 ka) | Recommended (optional) to use either: \\ - LDv1-LGMspin \\ - LDv1-transpin \\ See above for details. The method must be documented, including information on the state of spinup  |  
-| Astronomical parameters  | Transient, as per [[#References_cited|Berger (1978)]] [[ftp://ftp.ncdc.noaa.gov/pub/data/paleo/insolation/bein1.dat|[Access to data]]]|  +| Astronomical parameters  | Transient, as per [[#References_cited|Berger (1978)]]\\ [ [[ftp://ftp.ncdc.noaa.gov/pub/data/paleo/climate_forcing/orbital_variations/insolation/bein1.dat|Access to data]] **&** [[ftp://ftp.ncdc.noaa.gov/pub/data/paleo/climate_forcing/orbital_variations/insolation/readme_insolation.txt|README !]] ]|  
 | Solar constant | 1361.0 ± 0.51365 W m<sup>-2</sup>  | Solar constant | 1361.0 ± 0.51365 W m<sup>-2</sup> 
-| Trace gases  | Adjusted to the AICC2012 chronology [[#References_cited|Veres et al. (2013)]] 21-0 ka: \\ **CO<sub>2</sub>** = Transient, as per [[#References_cited|Bereiter et al. (2015)]] [[ftp://ftp.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/antarctica2015co2composite.txt|[Access to data]]]\\ **CH<sub>4</sub>** = Transient, as per [[#References_cited|Loulergue et al. (2008)]] \\ **N<sub>2</sub>O** = Transient, as per [[#References_cited|Schilt et al. (2010)]] \\ **CFC** = 0 \\ **O<sub>3</sub>** = Preindustrial (e.g. 10 DU)  |  +| Trace gases  | Adjusted to the AICC2012 chronology [[#References_cited|Veres et al. (2013)]] 21-0 ka: \\ **CO<sub>2</sub>** = Transient, as per [[#References_cited|Bereiter et al. (2015)]]: [ [[ftp://ftp.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/antarctica2015co2composite.txt|Access to data]] (md5sum = ''c54a033d8cbf588bc2b95d3b92ff9b1c''] \\ **CH<sub>4</sub>** = Transient, as per [[#References_cited|Loulergue et al. (2008)]]: [ [[data:gases#loulergue_et_al_ch4_data|Access to data]] ] \\ **N<sub>2</sub>O** = Transient, as per [[#References_cited|Schilt et al. (2010)]]: [ [[data:gases#schilt_et_al_n20_data|Access to data]] ]\\ **CFC** = 0 \\ **O<sub>3</sub>** = Preindustrial (e.g. 10 DU)  |  
-| Ice sheet | Transient, with a choice of either : \\ - ICE-6G_C reconstruction [[:data:ice|[Access to data]]] \\ - GLAC-1D reconstruction [[:data:ice|[Access to data]]] \\ How often to update the ice sheet is optional |+| Ice sheet | Transient, with a choice of either : \\ - ICE-6G_C reconstruction: [ [[:data:ice|Access to data]] ] \\ - GLAC-1D reconstruction: [ [[:data:ice|Access to data]] ] \\ How often to update the ice sheet is optional |
 | Orography and coastlines  | Transient. To be consistent with the choice of ice sheet. \\ Orography is updated on the same timestep as the ice sheet. It is optional how often the land-sea mask is updated, but ensure consistency with the ice sheet reconstruction is maintained |  | Orography and coastlines  | Transient. To be consistent with the choice of ice sheet. \\ Orography is updated on the same timestep as the ice sheet. It is optional how often the land-sea mask is updated, but ensure consistency with the ice sheet reconstruction is maintained | 
 | Bathymetry  | Keep consistent with the coastlines, and otherwise use either: \\ - Data associated with the ice sheet; it is optional how often the bathymetry is updated \\ - Preindustrial bathymetry |  | Bathymetry  | Keep consistent with the coastlines, and otherwise use either: \\ - Data associated with the ice sheet; it is optional how often the bathymetry is updated \\ - Preindustrial bathymetry | 
 | River routing | Ensure that rivers reach the coastline \\ It is recommended (optional) to use one of the following: \\ - Preindustrial configuration for the model \\ - Transient routing provided with the ice sheet reconstruction (if available) \\ - Manual/model calculation of river network to match topography  | | River routing | Ensure that rivers reach the coastline \\ It is recommended (optional) to use one of the following: \\ - Preindustrial configuration for the model \\ - Transient routing provided with the ice sheet reconstruction (if available) \\ - Manual/model calculation of river network to match topography  |
-| Freshwater fluxes | At participant discretion. Three options are: //melt-uniform//, //melt-routed// and //no-melt//: \\ - //Melt-uniform// : use a globally uniform ice meltwater flux, e.g. as associated with one of the ice sheet reconstructions [[:data:freshwater|[Access to data]]] \\ - //Melt-routed// : use a routed ice meltwater flux, e.g. as associated with one of the ice sheet reconstructions [[:data:freshwater|[Access to data]]] \\ - //No-melt// : have no ice sheet meltwater in the simulation \\ It is recommended (optional) to run at least one Core simulation with a scenario consistent with the chosen ice sheet reconstruction to conserve salinity. |+| Freshwater fluxes | At participant discretion. Three options are: //melt-uniform//, //melt-routed// and //no-melt//: \\ - //Melt-uniform// : use a globally uniform ice meltwater flux, e.g. as associated with one of the ice sheet reconstructions\\ [ [[data:ice_ice6g_c#freshwater_fluxes|ICE-6G_C]] ] - [ [[data:ice_glac_1d#freshwater_fluxes|GLAC-1D]] ] \\ - //Melt-routed// : use a routed ice meltwater flux, e.g. as associated with one of the ice sheet reconstructions\\ [ [[data:ice_ice6g_c#freshwater_fluxes|ICE-6G_C]] ] - [ [[data:ice_glac_1d#freshwater_fluxes|GLAC-1D]] ] \\ - //No-melt// : have no ice sheet meltwater in the simulation \\ It is recommended (optional) to run at least one Core simulation with a scenario consistent with the chosen ice sheet reconstruction to conserve salinity. |
 | Vegetation & land cover \\ Aerosols (dust) | Prescribed preindustrial cover or dynamic vegetation model \\ Prescribed preindustrial distribution or prognostic aerosols | | Vegetation & land cover \\ Aerosols (dust) | Prescribed preindustrial cover or dynamic vegetation model \\ Prescribed preindustrial distribution or prognostic aerosols |
  
-==== Focused simulations ==== +==== Focused simulations ==== 
   * Empty   * Empty
   * Empty   * Empty
  
 ===== References cited ===== ===== References cited =====
-  * Bereiter, B., Eggleston, S., Schmitt, J., Nehrbass-Ahles, C., Stocker, T. F., Fischer, H., Kipfstuhl, S. and Chappellaz, J.: Revision of the EPICA Dome C CO2 record from 800 to 600 kyr before present, Geophys. Res. Lett., 42(2), 2014GL061957, [[http://onlinelibrary.wiley.com/doi/10.1002/2014GL061957/abstract|doi:10.1002/2014GL061957]], 2015. + 
-  * Berger, A.: Long-Term Variations of Daily Insolation and Quaternary Climatic Changes, J. Atmospheric Sci., 35(12), 2362–2367, [[http://journals.ametsoc.org/doi/abs/10.1175/1520-0469(1978)035%3C2362:LTVODI%3E2.0.CO%3B2|doi:10.1175/1520-0469(1978)035<2362:LTVODI>2.0.CO;2]], 1978. +  * Bereiter, B., Eggleston, S., Schmitt, J., Nehrbass-Ahles, C., Stocker, T. F., Fischer, H., Kipfstuhl, S. and Chappellaz, J.: **Revision of the EPICA Dome C CO2 record from 800 to 600 kyr before present**, Geophys. Res. Lett., 42(2), 2014GL061957, [[http://onlinelibrary.wiley.com/doi/10.1002/2014GL061957/abstract|doi:10.1002/2014GL061957]], 2015. 
-  * Kageyama, M., Braconnot, P., Harrison, S. P., Haywood, A. M., Jungclaus, J., Otto-Bliesner, B. L., Peterschmitt, J.-Y., Abe-Ouchi, A., Albani, S., Bartlein, P. J., Brierley, C., Crucifix, M., Dolan, A., Fernandez-Donado, L., Fischer, H., Hopcroft, P. O., Ivanovic, R. F., Lambert, F., Lunt, D. J., Mahowald, N. M., Peltier, W. R., Phipps, S. J., Roche, D. M., Schmidt, G. A., Tarasov, L., Valdes, P. J., Zhang, Q. and Zhou, T.: PMIP4-CMIP6: the contribution of the Paleoclimate Modelling Intercomparison Project to CMIP6, Geosci. Model Dev. Discuss., 1–46, [[http://www.geosci-model-dev-discuss.net/gmd-2016-106/|doi:10.5194/gmd-2016-106]], 2016\\ +  * Berger, A.: **Long-Term Variations of Daily Insolation and Quaternary Climatic Changes**, J. Atmospheric Sci., 35(12), 2362–2367, [[http://journals.ametsoc.org/doi/abs/10.1175/1520-0469(1978)035%3C2362:LTVODI%3E2.0.CO%3B2|doi:10.1175/1520-0469(1978)035<2362:LTVODI>2.0.CO;2]], 1978. 
-  * Loulergue, L., Schilt, A., Spahni, R., Masson-Delmotte, V., Blunier, T., Lemieux, B., Barnola, J.-M., Raynaud, D., Stocker, T. F. and Chappellaz, J.: Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years, Nature, 453(7193), 383–386, [[http://www.nature.com/nature/journal/v453/n7193/full/nature06950.html|doi:10.1038/nature06950]], 2008. +  * **The PMIP4 contribution to CMIP6 – Part 1: Overview and over-arching analysis plan**, Kageyama, M., Braconnot, P., Harrison, S. P., Haywood, A. M., Jungclaus, J. H., Otto-Bliesner, B. L., Peterschmitt, J.-Y., Abe-Ouchi, A., Albani, S., Bartlein, P. J., Brierley, C., Crucifix, M., Dolan, A., Fernandez-Donado, L., Fischer, H., Hopcroft, P. O., Ivanovic, R. F., Lambert, F., Lunt, D. J., Mahowald, N. M., Peltier, W. R., Phipps, S. J., Roche, D. M., Schmidt, G. A., Tarasov, L., Valdes, P. J., Zhang, Q.and Zhou, T., Geosci. Model Dev., 11, 1033-1057, [[https://doi.org/10.5194/gmd-11-1033-2018|doi:10.5194/gmd-11-1033-2018]], 2018
-  * Schilt, A., Baumgartner, M., Schwander, J., Buiron, D., Capron, E., Chappellaz, J., Loulergue, L., Schüpbach, S., Spahni, R., Fischer, H. and Stocker, T. F.: Atmospheric nitrous oxide during the last 140,000 years, Earth Planet. Sci. Lett., 300(1–2), 33–43, [[http://www.sciencedirect.com/science/article/pii/S0012821X10006023|doi:10.1016/j.epsl.2010.09.027]], 2010. +  * Loulergue, L., Schilt, A., Spahni, R., Masson-Delmotte, V., Blunier, T., Lemieux, B., Barnola, J.-M., Raynaud, D., Stocker, T. F. and Chappellaz, J.: **Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years**, Nature, 453(7193), 383–386, [[http://www.nature.com/nature/journal/v453/n7193/full/nature06950.html|doi:10.1038/nature06950]], 2008. 
-  * Veres, D., Bazin, L., Landais, A., Toyé Mahamadou Kele, H., Lemieux-Dudon, B., Parrenin, F., Martinerie, P., Blayo, E., Blunier, T., Capron, E., Chappellaz, J., Rasmussen, S. O., Severi, M., Svensson, A., Vinther, B. and Wolff, E. W.: The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years, Clim Past, 9(4), 1733–1748, [[http://www.clim-past.net/9/1733/2013/|doi:10.5194/cp-9-1733-2013]], 2013.+  * Schilt, A., Baumgartner, M., Schwander, J., Buiron, D., Capron, E., Chappellaz, J., Loulergue, L., Schüpbach, S., Spahni, R., Fischer, H. and Stocker, T. F.: **Atmospheric nitrous oxide during the last 140,000 years**, Earth Planet. Sci. Lett., 300(1–2), 33–43, [[http://www.sciencedirect.com/science/article/pii/S0012821X10006023|doi:10.1016/j.epsl.2010.09.027]], 2010. 
 +  * Veres, D., Bazin, L., Landais, A., Toyé Mahamadou Kele, H., Lemieux-Dudon, B., Parrenin, F., Martinerie, P., Blayo, E., Blunier, T., Capron, E., Chappellaz, J., Rasmussen, S. O., Severi, M., Svensson, A., Vinther, B. and Wolff, E. W.: **The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years**, Clim Past, 9(4), 1733–1748, [[http://www.clim-past.net/9/1733/2013/|doi:10.5194/cp-9-1733-2013]], 2013.
  
  • exp_design/degla.1468336646.txt.gz
  • Last modified: 2016/07/12 15:17
  • by jypeter