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Explore the significance of studying past climate change, including glacial-interglacial cycles, natural variability, and climate feedbacks, with a focus on findings from Greenland and Antarctica. Discover the impact of Greenland melt on global climate projections and the connections between Northern and Southern Hemispheres. Gain insights from ice core data and climate simulations to understand the Earth's response to climatic forcings.
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A bipolar perspective on pastclimatechange (and expectations for information from the Third Pole) Valérie Masson-Delmotte Laboratoire des Sciences du Climat et de l’Environnement (CEA-CNRS-UVSQ/IPSL) Gif-sur-Yvette, France 3rd TPE Workshop, Reykjavik, Iceland – August 2011
Whystudypastclimate change? Glacial-interglacial cycles Seasonal cycle • Expand the short instrumental records • Naturalclimatevariability • « Slow » components: ocean, carbon cycle, icesheets • Understand the response of climate to forcings Detection / attribution Climatefeedbacks Thresholds • Natural case studies to benchmark Earth System models Huybers and Curry, Nature, 2006
AIR Global atmospheric composition Firnificationprocesses Icecores ICE Local climate AEROSOLS Regionalatmosphericaerosol content: Seasalt, dust, volcanism, solaractivity, pollutants…
NEEM ? Deeppolar icecores NorthGRIP ~ 125 000 yrs EDML : 140 000 yrs EDC : 800 000 yrs European Project for IceCoring in Antarctica (EPICA)
The greening of Greenland Greenlandicesheet mass balance Masson-Delmotte et al, submitted; updates from Bhatt et al, 2010 and van den Broeke et al, 2009
Past, present and projected changes Orbital forcing Icecore perspective : the last 125 000 years Icecore perspective : the last 10 000 years Greenland cultures Instrumental data Projections (A1B) Masson-Delmotte et al, submitted; data from NGRIP, Nature 2004 and Vinther et al, Nature, 2009
Limited analogies betweenpast and future climate change 126 ka (orbital forcing) 2xCO2 IPSL climate model DJF JJA ann • Comparable magnitude of summerwarming and feedbacks atmid to high latitudes north • Major differences in low-high latitude temperature gradients and seasonality Masson-Delmotte et al, Clim Past, in press
Global impacts of Greenlandmelt in climate projections • global sealevel • Atlantic meridionaloverturning circulation • negativefeedback on Arcticwarming • ITCZ shifts with major impacts on monsoon • precipitation Masson-Delmotte et al, submitted; simulations fromSwingedouw et al, J. Climate, 2009 Masson-Delmotte et al, submitted; data from NGRIP, Nature 2004 and Vinther et al, Nature, 2009
The Greenland-Antarcticbipolarseesaw Precursors: dustfromChinesedeserts, Greenlandmoistureorigin shifts Full glacial conditions Glacial inception EPICA, Nature, 2006; Steffenson et al, Science, 2008; Capron et al, Clim. Past, 2010; Masson-Delmotte et al, PNAS, 2010
Bipolarseesawunderinterglacial conditions? Bipolarseesaw CO2 Antarctica T Antarcticmoisture source Asianmonsoon Methane N. Atlantic SST Greenland T Links between abrupt shifts in Antarcticmoistureorigin and monsoon Masson-Delmotte et al, PNAS, 2010 An Zhisheng et al, Science, 2011
New tools for new challenges Searching for the oldestice in Antarctica • Cause for the shift between 40 ky to 100 kyclimatic cycles ? • Oldestice challenge Interglacials +5°C Present-day -9°C Glacials Jouzel et al Science 2007, Loulergue et al Nature 2008, Lisiecki & RaymoPaleoceano2005 Masson-Delmotte et al, QSR, 2010; Jouzel and Masson-Delmotte, QSR, 2011
Towards a tri-polar perspective on climate change • Links between « northern pull », « southern push » and monsoon • Sequence of eventsbetweentropical,mid latitude and polar atmospheric circulation • Response of climate to major volcaniceruptions (importance for the decadalpredictability of climate) ChunmingShi et al, Clim. Past, submitted
Towards a tri-polar perspective on climate change • Exceptionalmonitoring effort for process-basedunderstanding of the climatic drivers of precipitationisotopiccomposition • Unique opportunity for a multi-archive TPE approach for reconstructingpastprecipitationd18O (icecores, tree rings, lakesediments, speleothems…) • Need of data synthesesfor benchmarkingclimatemodels • (CMIP5 includespaleoclimate simulations) Yao Tandong et al, in preparation