Studying the Greenland ice sheet: Implications for climate past and present.
durch
Dorthe Dahl-Jensen(University of Copenhagen)
→
Europe/Berlin
SB1 1.120 (GSI Main Lecture Hall)
SB1 1.120
GSI Main Lecture Hall
Beschreibung
The Greenland ice sheet is reacting to the recent climate change and is losing more and more mass for every year. One of our challenges in the future is to adapt to rising sea levels [1]. Looking into the past gains us knowledge on how the ice sheets react to changing climate of the past and this knowledge can be used to improve predictions of sea level rise in the future. The deep ice cores from Greenland contain information on the past climate more than 130.000 years back in time.
Results from the Greenland ice cores are presented and are used to extract information on the climate during the glacial period where 25 abrupt climate changes named Dansgaard-Oeschger events are discussed [2,3].
All the ice cores drilled though the Greenland ice sheets show that they all contain ice from the previous warm Eemian climate period, 130.000 to 155000 years before present. Is it thus clear that the Greenland Ice Sheet did exist for 120.000 years ago in this warm climate period where it was 5 C warmer over Greenland [4] and the sea level has been estimated to have been 6-9 m [5] higher than the present sea level?
1 Shepherd, A. et al. A Reconciled Estimate of Ice-Sheet Mass Balance. Science 338, 1183-1189, doi:10.1126/science.1228102 (2012).
2 Johnsen, S. J. et al. Oxygen isotope and palaeotemperature records from six Greenland ice-core stations: Camp Century, Dye-3, GRIP, GISP2, Renland and NorthGRIP. Journal of Quaternary Science 16, 299-307 (2001).
3 Buizert, C. et al. Greenland temperature response to climate forcing during the last deglaciation. Science 345, 1177-1180, doi:10.1126/science.1254961 (2014).
4 Dahl-Jensen, D. et al. Eemian interglacial reconstructed from a Greenland folded ice core. Nature 493, 489-494, doi:10.1038/nature11789 (2013).
5 Kopp, R. E., Simons, F. J., Mitrovica, J. X., Maloof, A. C. & Oppenheimer, M. Probabilistic assessment of sea level during the last interglacial stage. Nature 462, 863-U851, doi:10.1038/nature08686 (2009).
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