Local insolation changes enhance Antarctic interglacials: Insights from an 800,000-year ice sheet simulation with transient climate forcing
暂无分享,去创建一个
[1] Tobias Friedrich,et al. Nonlinear climate sensitivity and its implications for future greenhouse warming , 2016, Science Advances.
[2] A. Ganopolski,et al. Comparison of surface mass balance of ice sheets simulated by positive-degree-day method and energy balance approach , 2016 .
[3] A. Timmermann,et al. Late Pleistocene climate drivers of early human migration , 2016, Nature.
[4] R. DeConto,et al. Contribution of Antarctica to past and future sea-level rise , 2016, Nature.
[5] K. Grosfeld,et al. Ocean temperature thresholds for Last Interglacial West Antarctic Ice Sheet collapse , 2016 .
[6] K. Kusahara,et al. Modelling the Antarctic marine cryosphere at the Last Glacial Maximum , 2015, Annals of Glaciology.
[7] S. Rahmstorf,et al. Sea-level rise due to polar ice-sheet mass loss during past warm periods , 2015, Science.
[8] Matt A. King,et al. Low post-glacial rebound rates in the Weddell Sea due to Late Holocene ice-sheet readvance , 2014, Earth and Planetary Science Letters.
[9] L. Lisiecki,et al. A Late Pleistocene sea level stack , 2014 .
[10] T. L. Rasmussen,et al. Temporal and spatial structure of multi-millennial temperature changes at high latitudes during the Last Interglacial , 2014 .
[11] R. McKay,et al. Orbital forcing of the East Antarctic ice sheet during the Pliocene and Early Pleistocene , 2014 .
[12] M. England,et al. Antarctic contribution to meltwater pulse 1A from reduced Southern Ocean overturning , 2014, Nature Communications.
[13] John B. Anderson,et al. A community-based geological reconstruction of Antarctic Ice Sheet deglaciation since the Last Glacial Maximum , 2014 .
[14] M. Crucifix,et al. Modelling the evolution of the Antarctic ice sheet since the last interglacial , 2014 .
[15] A. Timmermann,et al. Modeling Obliquity and CO2Effects on Southern Hemisphere Climate during the Past 408 ka , 2014 .
[16] J. Jouzel,et al. Synchronous Change of Atmospheric CO2 and Antarctic Temperature During the Last Deglacial Warming , 2013, Science.
[17] J. Kutzbach,et al. Northern Hemisphere forcing of Southern Hemisphere climate during the last deglaciation , 2013, Nature.
[18] B. Boer,et al. A continuous simulation of global ice volume over the past 1 million years with 3-D ice-sheet models , 2013, Climate Dynamics.
[19] J. Gabrieli,et al. Iron fluxes to Talos Dome, Antarctica, over the past 200 kyr , 2012 .
[20] A. Rosell‐Melé,et al. Sea surface temperature variability in the Pacific sector of the Southern Ocean over the past 700 kyr , 2012 .
[21] M. Loutre,et al. An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120--800 ka , 2012 .
[22] David Pollard,et al. Description of a hybrid ice sheet-shelf model, and application to Antarctica , 2012 .
[23] R. McKay,et al. Pleistocene variability of Antarctic Ice Sheet extent in the Ross Embayment , 2012 .
[24] J. Jouzel,et al. Ranges of moisture-source temperature estimated from Antarctic ice cores stable isotope records over glacial–interglacial cycles , 2012 .
[25] S. Jacobs,et al. Stronger ocean circulation and increased melting under Pine Island Glacier ice shelf , 2011 .
[26] M. Werner,et al. Synchronicity of Antarctic temperatures and local solar insolation on orbital timescales , 2011, Nature.
[27] T. Stocker,et al. Expression of the bipolar see-saw in Antarctic climate records during the last deglaciation , 2011 .
[28] Benoît Tartinville,et al. Description of the Earth system model of intermediate complexity LOVECLIM version 1.2 , 2010 .
[29] P. Huybers. Antarctica's Orbital Beat , 2009, Science.
[30] A. Timmermann,et al. The Roles of CO2 and Orbital Forcing in Driving Southern Hemispheric Temperature Variations during the Last 21 000 Yr , 2009 .
[31] David Pollard,et al. Modelling West Antarctic ice sheet growth and collapse through the past five million years , 2009, Nature.
[32] A. Rosell‐Melé,et al. Links between iron supply, marine productivity, sea surface temperature, and CO2 over the last 1.1 Ma , 2009 .
[33] T. Stocker,et al. High-resolution carbon dioxide concentration record 650,000–800,000 years before present , 2008, Nature.
[34] R. Gersonde,et al. The last five glacial‐interglacial transitions: A high‐resolution 450,000‐year record from the subantarctic Atlantic , 2007 .
[35] C. Schoof. Ice sheet grounding line dynamics: Steady states, stability, and hysteresis , 2007 .
[36] A. Timmermann,et al. Simulation of the Last 21 000 Years Using Accelerated Transient Boundary Conditions , 2007 .
[37] Kenji Kawamura,et al. Northern Hemisphere forcing of climatic cycles in Antarctica over the past 360,000 years , 2007, Nature.
[38] A. Schilt,et al. Orbital and Millennial Antarctic Climate Variability over the Past 800,000 Years , 2007, Science.
[39] J. Tison,et al. One-to-one coupling of glacial climate variability in Greenland and Antarctica. , 2006 .
[40] Kerim H. Nisancioglu,et al. Plio-Pleistocene Ice Volume, Antarctic Climate, and the Global δ18O Record , 2006, Science.
[41] D. Nürnberg,et al. Pleistocene variability of the Subtropical Convergence at East Tasman Plateau: Evidence from planktonic foraminiferal Mg/Ca (ODP Site 1172A) , 2006 .
[42] Epica Community Members. One-to-one coupling of glacial climate variability in Greenland and Antarctica , 2006, Nature.
[43] Jacques Laskar,et al. A long-term numerical solution for the insolation quantities of the Earth , 2004 .
[44] J. Jouzel,et al. New modeling of the Vostok ice flow line and implication for the glaciological chronology of the Vostok ice core , 2004 .
[45] Philippe Huybrechts,et al. Sea-level changes at the LGM from ice-dynamic reconstructions of the Greenland and Antarctic ice sheets during the glacial cycles , 2002 .
[46] K. Lambeck,et al. Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records , 2002 .
[47] Catherine Ritz,et al. Modeling the evolution of Antarctic ice sheet over the last 420,000 years: Implications for altitude changes in the Vostok region , 2001 .
[48] N. Shackleton,et al. The 100,000-year ice-Age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity , 2000, Science.
[49] P. Mayewski,et al. Wisconsinan and holocene climate history from an ice core at taylor dome, western ross embayment, antarctica , 2000 .