data:gases

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data:gases [2016/11/15 17:22]
jypeter Updated the gases values for 6ka and 127ka 		data:gases [2019/02/11 10:20] (current)
jypeter Updated the spinup gases
Line 11: Line 11:
 | LDv1-LGMspin | //Same as lgm// | | LDv1-LGMspin | //Same as lgm// |
 | LDv1-transpin\\ LDv1 | Transient, as per [[exp_design:degla#References_cited|Bereiter et al. (2015)]]\\ [ [[ftp://ftp.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/antarctica2015co2composite.txt|Bereiter et al data access]] ] (md5sum = ''c54a033d8cbf588bc2b95d3b92ff9b1c'') | | LDv1-transpin\\ LDv1 | Transient, as per [[exp_design:degla#References_cited|Bereiter et al. (2015)]]\\ [ [[ftp://ftp.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/antarctica2015co2composite.txt|Bereiter et al data access]] ] (md5sum = ''c54a033d8cbf588bc2b95d3b92ff9b1c'') |
 +| PDGv1-PGMspin | 191 |
 +| PDGv1 | **CO<sub>2</sub>** = Transient, as per [[exp_design:degla_t2#References_cited| the spline of Koehler et al. (2017)]]: [ [[https://doi.pangaea.de/10.1594/PANGAEA.871273|Access to data]] ] |
  
  
Line 23: Line 25:
 | LDv1-LGMspin | //Same as lgm// | | LDv1-LGMspin | //Same as lgm// |
 | LDv1-transpin\\ LDv1 | Transient, as per Loulergue et al. (2008)\\ **Get reference and data below!** | | LDv1-transpin\\ LDv1 | Transient, as per Loulergue et al. (2008)\\ **Get reference and data below!** |
 +| PDGv1-PGMspin | 385 |
 +| PDGv1 | Transient, as per [[exp_design:degla_t2#References_cited| the spline of Koehler et al. (2017)]]: [ [[https://doi.pangaea.de/10.1594/PANGAEA.871273|Access to data]] ] |
 +
  
 ==== Loulergue et al CH4 data ==== ==== Loulergue et al CH4 data ====
Line 40: Line 45:
 | LDv1-LGMspin | //Same as lgm// | | LDv1-LGMspin | //Same as lgm// |
 | LDv1-transpin\\ LDv1 | Transient, as per Schilt et al. (2010)\\ **Get reference and data below!** | | LDv1-transpin\\ LDv1 | Transient, as per Schilt et al. (2010)\\ **Get reference and data below!** |
 +| PDGv1-PGMspin | 201 |
 +| PDGv1 | Linear increase from 201 ppb at 140 ka to 218.74 ppb at 134.5 ka\\ then transient, as per [[exp_design:degla_t2#References_cited| the spline of Koehler et al. (2017)]]: [ [[https://doi.pangaea.de/10.1594/PANGAEA.871273|Access to data]] ] |
 +
  
 ==== Schilt et al N20 data ==== ==== Schilt et al N20 data ====
Line 56: Line 64:
 | midPliocene-eoi400 | //Same as in CMIP6 piControl// | | midPliocene-eoi400 | //Same as in CMIP6 piControl// |
 | LDv1-LGMspin\\ LDv1-transpin\\ LDv1 | \\ //Same as lgm// | | LDv1-LGMspin\\ LDv1-transpin\\ LDv1 | \\ //Same as lgm// |
 +| PDGv1-PGMspin\\ PDGv1 | 0 |
  
 ===== O3 ===== ===== O3 =====
  
 ^ Experiment ^ Value ^ ^ Experiment ^ Value ^
-| midHolocene\\ lgm\\ lig127k\\ midPliocene-eoi400 \\ LDv1-LGMspin\\ LDv1-transpin\\ LDv1 | \\ \\ \\ //Same as in CMIP6 piControl// |+| midHolocene\\ lgm\\ lig127k\\ midPliocene-eoi400 \\ LDv1-LGMspin\\ LDv1-transpin\\ LDv1\\ PDGv1-PGMspin\\ PDGv1 | \\ \\ \\ //Same as in CMIP6 piControl// |
 | past1000 | For models without interactive ozone chemistry, we suggest that O3 modulation is derived in a similar way from the modulation of the UV part of the solar spectrum as in the historical simulations (c.f. [[http://www.geosci-model-dev-discuss.net/gmd-2016-91/|Matthes et al., CMIP6 GMD special issue 2016]]) | | past1000 | For models without interactive ozone chemistry, we suggest that O3 modulation is derived in a similar way from the modulation of the UV part of the solar spectrum as in the historical simulations (c.f. [[http://www.geosci-model-dev-discuss.net/gmd-2016-91/|Matthes et al., CMIP6 GMD special issue 2016]]) |
  
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  • Last modified: 2016/11/15 17:22
  • by jypeter