Articles | Volume 2, issue 2
https://doi.org/10.5194/cp-2-221-2006
© Author(s) 2006. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
Special issue:
https://doi.org/10.5194/cp-2-221-2006
© Author(s) 2006. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
28 Nov 2006
Comparing transient, accelerated, and equilibrium simulations of the last 30 000 years with the GENIE-1 model
D. J. Lunt
Bristol Research Initiative for the Dynamic Global Environment (BRIDGE), School of Geographical Sciences, University of Bristol, Bristol, UK
M. S. Williamson
School of Environmental Sciences, University of East Anglia, UK
Tyndall Centre, UK
now at: Quantum Information Group, University of Leeds, Leeds, UK
P. J. Valdes
Bristol Research Initiative for the Dynamic Global Environment (BRIDGE), School of Geographical Sciences, University of Bristol, Bristol, UK
T. M. Lenton
School of Environmental Sciences, University of East Anglia, UK
Tyndall Centre, UK
R. Marsh
National Oceanography Centre, University of Southampton, Southhampton, UK
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Cited
23 citations as recorded by crossref.
- Simulation of the Last 21 000 Years Using Accelerated Transient Boundary Conditions* O. Timm & A. Timmermann 10.1175/JCLI4237.1
- Can we use ice sheet reconstructions to constrain meltwater for deglacial simulations? I. Bethke et al. 10.1029/2011PA002258
- Transient simulations of the present and the last interglacial climate using the Community Climate System Model version 3: effects of orbital acceleration V. Varma et al. 10.5194/gmd-9-3859-2016
- High-latitude climate sensitivity to ice-sheet forcing over the last 120kyr J. Singarayer & P. Valdes 10.1016/j.quascirev.2009.10.011
- Comparison of climate responses to orbital forcing at different latitudes during the Holocene Y. Jing et al. 10.1016/j.quaint.2022.02.004
- Assessing transient changes in the ocean carbon cycle during the last deglaciation through carbon isotope modeling H. Kobayashi et al. 10.5194/cp-20-769-2024
- Multi-centennial variability of the AMOC over the Holocene: A new reconstruction based on multiple proxy-derived SST records M. Ayache et al. 10.1016/j.gloplacha.2018.08.016
- A transient coupled general circulation model (CGCM) simulation of the past 3 million years K. Yun et al. 10.5194/cp-19-1951-2023
- Eurasian Holocene climate trends in transient coupled climate simulations and stable oxygen isotope records C. DANEK et al. 10.1002/jqs.3396
- Mechanisms for the Onset of the African Humid Period and Sahara Greening 14.5–11 ka BP* O. Timm et al. 10.1175/2010JCLI3217.1
- Diagnosing the causes of AMOC slowdown in a coupled model: a cautionary tale J. Gérard & M. Crucifix 10.5194/esd-15-293-2024
- Holocene North Atlantic Overturning in an atmosphere‐ocean‐sea ice model compared to proxy‐based reconstructions M. Blaschek et al. 10.1002/2015PA002828
- On the definition of seasons in paleoclimate simulations with orbital forcing O. Timm et al. 10.1029/2007PA001461
- A retrospective look at coupled ice sheet–climate modeling D. Pollard 10.1007/s10584-010-9830-9
- A probabilistic calibration of climate sensitivity and terrestrial carbon change in GENIE-1 P. Holden et al. 10.1007/s00382-009-0630-8
- Deciphering the spatio-temporal complexity of climate change of the last deglaciation: a model analysis D. Roche et al. 10.5194/cp-7-591-2011
- The relative contribution of orbital forcing and greenhouse gases to the North American deglaciation L. Gregoire et al. 10.1002/2015GL066005
- Multi-level emulation of complex climate model responses to boundary forcing data G. Tran et al. 10.1007/s00382-018-4205-4
- System Architecture and Planetary Obliquity: Implications for Long-term Habitability P. Vervoort et al. 10.3847/1538-3881/ac87fd
- Tropical Pacific response to continental ice sheet topography S. Lee et al. 10.1007/s00382-014-2162-0
- Interhemispheric coupling, the West Antarctic Ice Sheet and warm Antarctic interglacials P. Holden et al. 10.5194/cp-6-431-2010
- Deconstructing the Last Glacial termination: the role of millennial and orbital-scale forcings L. Menviel et al. 10.1016/j.quascirev.2011.02.005
- The Roles of CO2 and Orbital Forcing in Driving Southern Hemispheric Temperature Variations during the Last 21 000 Yr* A. Timmermann et al. 10.1175/2008JCLI2161.1
21 citations as recorded by crossref.
- Simulation of the Last 21 000 Years Using Accelerated Transient Boundary Conditions* O. Timm & A. Timmermann 10.1175/JCLI4237.1
- Can we use ice sheet reconstructions to constrain meltwater for deglacial simulations? I. Bethke et al. 10.1029/2011PA002258
- Transient simulations of the present and the last interglacial climate using the Community Climate System Model version 3: effects of orbital acceleration V. Varma et al. 10.5194/gmd-9-3859-2016
- High-latitude climate sensitivity to ice-sheet forcing over the last 120kyr J. Singarayer & P. Valdes 10.1016/j.quascirev.2009.10.011
- Comparison of climate responses to orbital forcing at different latitudes during the Holocene Y. Jing et al. 10.1016/j.quaint.2022.02.004
- Assessing transient changes in the ocean carbon cycle during the last deglaciation through carbon isotope modeling H. Kobayashi et al. 10.5194/cp-20-769-2024
- Multi-centennial variability of the AMOC over the Holocene: A new reconstruction based on multiple proxy-derived SST records M. Ayache et al. 10.1016/j.gloplacha.2018.08.016
- A transient coupled general circulation model (CGCM) simulation of the past 3 million years K. Yun et al. 10.5194/cp-19-1951-2023
- Eurasian Holocene climate trends in transient coupled climate simulations and stable oxygen isotope records C. DANEK et al. 10.1002/jqs.3396
- Mechanisms for the Onset of the African Humid Period and Sahara Greening 14.5–11 ka BP* O. Timm et al. 10.1175/2010JCLI3217.1
- Diagnosing the causes of AMOC slowdown in a coupled model: a cautionary tale J. Gérard & M. Crucifix 10.5194/esd-15-293-2024
- Holocene North Atlantic Overturning in an atmosphere‐ocean‐sea ice model compared to proxy‐based reconstructions M. Blaschek et al. 10.1002/2015PA002828
- On the definition of seasons in paleoclimate simulations with orbital forcing O. Timm et al. 10.1029/2007PA001461
- A retrospective look at coupled ice sheet–climate modeling D. Pollard 10.1007/s10584-010-9830-9
- A probabilistic calibration of climate sensitivity and terrestrial carbon change in GENIE-1 P. Holden et al. 10.1007/s00382-009-0630-8
- Deciphering the spatio-temporal complexity of climate change of the last deglaciation: a model analysis D. Roche et al. 10.5194/cp-7-591-2011
- The relative contribution of orbital forcing and greenhouse gases to the North American deglaciation L. Gregoire et al. 10.1002/2015GL066005
- Multi-level emulation of complex climate model responses to boundary forcing data G. Tran et al. 10.1007/s00382-018-4205-4
- System Architecture and Planetary Obliquity: Implications for Long-term Habitability P. Vervoort et al. 10.3847/1538-3881/ac87fd
- Tropical Pacific response to continental ice sheet topography S. Lee et al. 10.1007/s00382-014-2162-0
- Interhemispheric coupling, the West Antarctic Ice Sheet and warm Antarctic interglacials P. Holden et al. 10.5194/cp-6-431-2010
2 citations as recorded by crossref.
- Deconstructing the Last Glacial termination: the role of millennial and orbital-scale forcings L. Menviel et al. 10.1016/j.quascirev.2011.02.005
- The Roles of CO2 and Orbital Forcing in Driving Southern Hemispheric Temperature Variations during the Last 21 000 Yr* A. Timmermann et al. 10.1175/2008JCLI2161.1
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