User Tools

Site Tools


pmip3:wg:p2f:methods

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
Next revision Both sides next revision
pmip3:wg:p2f:methods [2013/09/11 03:44]
jules [Overview of papers]
pmip3:wg:p2f:methods [2013/09/11 07:00]
jules [Overview of papers]
Line 155: Line 155:
 J. C. Hargreaves, J. D. Annan1, R. Ohgaito, A. Paul, and A. Abe-Ouchi, Clim. Past, 9, 811–823, [[http://​www.clim-past.net/​9/​811/​2013/​|open access]] doi:​10.5194/​cp-9-811-20132013. and **Are paleoclimate model ensembles consistent with the MARGO data synthesis?​** J. C. Hargreaves, A. Paul, R. Ohgaito, A. Abe-Ouchi, and J. D. Annan Clim. Past, 7, 917–933, [[http://​www.clim-past.net/​7/​917/​2011/​|open access]] doi:​10.5194/​cp-7-917-2011,​ 2011 J. C. Hargreaves, J. D. Annan1, R. Ohgaito, A. Paul, and A. Abe-Ouchi, Clim. Past, 9, 811–823, [[http://​www.clim-past.net/​9/​811/​2013/​|open access]] doi:​10.5194/​cp-9-811-20132013. and **Are paleoclimate model ensembles consistent with the MARGO data synthesis?​** J. C. Hargreaves, A. Paul, R. Ohgaito, A. Abe-Ouchi, and J. D. Annan Clim. Past, 7, 917–933, [[http://​www.clim-past.net/​7/​917/​2011/​|open access]] doi:​10.5194/​cp-7-917-2011,​ 2011
  
-//keywords: PMIP, LGM, evaluation, ​ocean (SST)// ​+//keywords: PMIP, LGM, evaluation, ​temperature ​(SAT over land, SST for ocean)// 
  
 ''​Show that PMIP2 and available PMIP3 models are reliable and have skill for air and surface ocean temperatures on broad scales, for the LGM. On the other hand, the MIROC single model ensemble is under-dispersive (a result common for single model ensembles - see Yokohata et al 2010). Additionally the models have no skill and are not reliable for the mid-Holocene interval. ''​ ''​Show that PMIP2 and available PMIP3 models are reliable and have skill for air and surface ocean temperatures on broad scales, for the LGM. On the other hand, the MIROC single model ensemble is under-dispersive (a result common for single model ensembles - see Yokohata et al 2010). Additionally the models have no skill and are not reliable for the mid-Holocene interval. ''​
Line 168: Line 168:
  
 ==September sea-ice cover in the Arctic Ocean projected to vanish by 2100== ​ ==September sea-ice cover in the Arctic Ocean projected to vanish by 2100== ​
-Julien Boé, Alex Hall and Xin Qu, Nature Geoscience 2, 341, [[http://​www.atmos.ucla.edu/​csrl/​publications/​Hall/​boe_et_al_2009a.pdf|free PDF at author'​s homepage]] or [[http://​www.nature.com/​ngeo/​journal/​v2/​n5/​abs/​ngeo467.html|paywall]], ​]doi:​10.1038/​ngeo467,​ 2009.+Julien Boé, Alex Hall and Xin Qu, Nature Geoscience 2, 341, [[http://​www.atmos.ucla.edu/​csrl/​publications/​Hall/​boe_et_al_2009a.pdf|free PDF at author'​s homepage]] or [[http://​www.nature.com/​ngeo/​journal/​v2/​n5/​abs/​ngeo467.html|paywall]],​ doi:​10.1038/​ngeo467,​ 2009.
  
 //keywords : model ensemble, past century, sea-ice, Arctic// //keywords : model ensemble, past century, sea-ice, Arctic//
Line 211: Line 211:
  
 ==Using the current seasonal cycle to constrain snow albedo feedback in future climate change== ​ ==Using the current seasonal cycle to constrain snow albedo feedback in future climate change== ​
-Hall, A., & Qu, X.  Geophysical Research Letters, 33(3), L03502, [[http://​www.atmos.ucla.edu/​csrl/​publications/​Hall/​Hall_Qu_2006.pdf|PDF at author'​s website]] or [[http://​onlinelibrary.wiley.com/​doi/​10.1029/​2005GL025127/​abstract|paywall]],​ doi:​10.1029/​2005GL025127,​ 2006+Hall, A., & Qu, X.  Geophysical Research Letters, 33(3), L03502, [[http://​www.atmos.ucla.edu/​csrl/​publications/​Hall/​Hall_Qu_2006.pdf|free PDF at author'​s website]] or [[http://​onlinelibrary.wiley.com/​doi/​10.1029/​2005GL025127/​abstract|paywall]],​ doi:​10.1029/​2005GL025127,​ 2006
  
 //keywords: Northern hemisphere, PMIP, modern, model ensemble// //keywords: Northern hemisphere, PMIP, modern, model ensemble//
Line 219: Line 219:
  
 ==Climate sensitivity estimated from ensemble simulations of glacial climate== ​ ==Climate sensitivity estimated from ensemble simulations of glacial climate== ​
-Thomas Schneider von Deimling, Hermann Held, Andrey Ganopolski & Stefan Rahmstorf, Climate Dynamics, [[http://​www.pik-potsdam.de/​~stefan/​Publications/​Journals/​Schneider_etal_ClimDyn_2006.pdf|PDF at author'​s website]] or [[http://​link.springer.com/​article/​10.1007%2Fs00382-006-0126-8|paywall]],​ DOI 10.1007/​s00382-006-0126-8,​ 2006+Thomas Schneider von Deimling, Hermann Held, Andrey Ganopolski & Stefan Rahmstorf, Climate Dynamics, [[http://​www.pik-potsdam.de/​~stefan/​Publications/​Journals/​Schneider_etal_ClimDyn_2006.pdf|free PDF at author'​s website]] or [[http://​link.springer.com/​article/​10.1007%2Fs00382-006-0126-8|paywall]],​ DOI 10.1007/​s00382-006-0126-8,​ 2006
  
 //keywords: parameter ensemble, climate sensitivity,​ LGM, dust// //keywords: parameter ensemble, climate sensitivity,​ LGM, dust//
Line 232: Line 232:
  
 ''​In this case, estimates of tropical SST taken from the literature were used to constrain a since model ensemble with varied parameters of the MIROC GCM. This MIROC ensemble has now been shown to be of much lower dispersion than the multi-model ensemble (Hargreaves et al above, and Yokohata et al 2010). Indeed it was found impossible to produce a run with this model climate sensitivity less than 4C, while the data constraint for the LGM data suggested a lower value was entirely plausible.''​ ''​In this case, estimates of tropical SST taken from the literature were used to constrain a since model ensemble with varied parameters of the MIROC GCM. This MIROC ensemble has now been shown to be of much lower dispersion than the multi-model ensemble (Hargreaves et al above, and Yokohata et al 2010). Indeed it was found impossible to produce a run with this model climate sensitivity less than 4C, while the data constraint for the LGM data suggested a lower value was entirely plausible.''​
 +
 +====Authors====
 +Contributors to this page:
 +
 +James Annan,
 +Michel Crucifix,
 +Julia Hargreaves.
 +
  
 /* standard page footer */ /* standard page footer */
pmip3/wg/p2f/methods.txt · Last modified: 2017/02/10 15:47 by jules