Modelling the end of an interglacial (MIS 1, 5, 7, 9, 11)

[1]  M. Claussen,et al.  Climate Dynamics (2006) DOI 10.1007/s00382-006-0136-6 , 2005 .

[2]  M. Claussen,et al.  Transient simulation of the last glacial inception. Part I: glacial inception as a bifurcation in the climate system , 2005 .

[3]  V. Brovkin,et al.  Transient simulation of the last glacial inception. Part II: sensitivity and feedback analysis , 2005 .

[4]  G. Kukla,et al.  North Atlantic Current and European environments during the declining stage of the last interglacial , 2004 .

[5]  C. Ritz,et al.  Quantifying ice‐sheet feedbacks during the last glacial inception , 2004 .

[6]  J Schwander,et al.  High-resolution record of Northern Hemisphere climate extending into the last interglacial period , 2004, Nature.

[7]  W. Peltier,et al.  Sensitivity of glacial inception to orbital and greenhouse gas climate forcing. , 2004 .

[8]  Katrin J. Meissner,et al.  The role of land surface dynamics in glacial inception: a study with the UVic Earth System Model , 2003 .

[9]  M. Siddall,et al.  Sea-level fluctuations during the last glacial cycle , 2003, Nature.

[10]  Victor Brovkin,et al.  Carbon cycle, vegetation, and climate dynamics in the Holocene: Experiments with the CLIMBER‐2 model , 2002 .

[11]  L. Mysak,et al.  Simulation of the last glacial inception and rapid ice sheet growth in the McGill Paleoclimate Model , 2002 .

[12]  André Berger,et al.  An Exceptionally Long Interglacial Ahead? , 2002, Science.

[13]  M. Loutre,et al.  Transient simulations over the last interglacial period (126–115 kyr BP): feedback and forcing analysis , 2002 .

[14]  K. Lambeck,et al.  Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records , 2002 .

[15]  A. Weaver,et al.  On the causes of glacial inception at 116 kaBP , 2002 .

[16]  G. Ramstein,et al.  Simulating the amplification of orbital forcing by ocean feedbacks in the last glaciation , 2001, Nature.

[17]  Stefan Rahmstorf,et al.  Rapid changes of glacial climate simulated in a coupled climate model , 2001, Nature.

[18]  S. Marshall,et al.  Substantial contribution to sea-level rise during the last interglacial from the Greenland ice sheet , 2000, Nature.

[19]  H. Storch,et al.  Climate Simulation for 125 kyr BP with a Coupled Ocean-Atmosphere General Circulation Model , 2000 .

[20]  Victor Brovkin,et al.  CLIMBER-2: a climate system model of intermediate complexity. Part I: model description and performance for present climate , 2000 .

[21]  Victor Brovkin,et al.  CLIMBER-2: a climate system model of intermediate complexity. Part II: model sensitivity , 2001 .

[22]  J. Jouzel,et al.  Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica , 1999, Nature.

[23]  M. Loutre,et al.  Sensitivity of the LLN climate model to the astronomical and CO2 forcings over the last 200 ky , 1998 .

[24]  W. Peltier,et al.  Terminating the 100 kyr ice age cycle , 1997 .

[25]  R. Greve.  A continuum–mechanical formulation for shallow polythermal ice sheets , 1997, Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences.

[26]  Pascale Braconnot,et al.  Sensitivity of paleoclimate simulation results to season definitions , 1997 .

[27]  Aurélie Botta,et al.  Possible role of atmosphere-biosphere interactions in triggering the last glaciation , 1996 .

[28]  B. Grieger,et al.  Investigating the sensitivity of the Atmospheric General Circulation Model ECHAM 3 to paleoclimatic boundary conditions , 1996 .

[29]  N. Noblet,et al.  Sensitivity of simulated Asian and African summer monsoons to orbitally induced variations in insolation 126, 115 and 6 kBP , 1996 .

[30]  J. Kutzbach,et al.  Role of orbitally induced changes in tundra area in the onset of glaciation , 1996, Nature.

[31]  J. Pandolfi,et al.  Reconciliation of late Quaternary sea levels derived from coral terraces at Huon Peninsula with deep sea oxygen isotope records , 1996 .

[32]  P. Valdes,et al.  Sensitivity Studies of Northern Hemisphere Glaciation Using an Atmospheric General Circulation Model , 1995 .

[33]  J. Clague,et al.  Initiation and development of the Laurentide and Cordilleran Ice Sheets following the last interglaciation , 1993 .

[34]  André Berger,et al.  Simulation of the Last Glacial Cycle By a Coupled, Sectorially Averaged Climate-ice Sheet Model .2. Response To Insolation and Co2 Variations , 1992 .

[35]  W. Peltier,et al.  A One-Dimensional Model of Continental Ice Volume Fluctuations through the Pleistocene: Implications for the Origin of the Mid-Pleistocene Climate Transition , 1991 .

[36]  C. Lorius,et al.  Vostok ice core provides 160,000-year record of atmospheric CO2 , 1987, Nature.

[37]  J. Kutzbach,et al.  The Sensitivity of the African-Asian Monsoonal Climate to Orbital Parameter Changes for 9000 Years B.P. in a Low-Resolution General Circulation Model. , 1982 .

[38]  André Berger,et al.  Long-term variations of daily insolation and Quaternary climatic changes , 1978 .