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MARINGEOLOGI OG GLACIOLOGI

De Nationale Geologiske Undersøgelser for Danmark og Grønland (GEUS)
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CLIMATE CHANGE RESEARCH, OVERVIEW

Climate changes make up one the major challenges for humankind in the future. Recent climate modelling predicts that the average global temperature will rise more then previously thought.

Since the end of the 19th century the average temperature on earth has already risen by 0.3°C to 0.6°C . A possible link between this temperature rise and an anthropogenically-induced increase of greenhouse gases has been the topic of intensive and worldwide discussions. However, until few years ago it was doubtful whether global warming was (partly) caused by human use of fossil energy resources. Indeed, it could also be a purely natural phenomenon, since climate has changed through the Earth's history, also without interference of mankind. Progress has meanwhile been made, and recent research enables us to state with almost 100% certainty that mankind has started to play a role in changing the global climate. By the emission of greenhouse gases as carbon dioxide and methane, man is contributing actively to global warming.

Thus, the earth may warm u p more in one hundred years than it has done since the beginning of the present, "INTERGLACIAL" climate regime, which started c.10,000 years ago. One the consequences is that sea level is expected to rise several decimetres, maybe even more than 50 cm. Moreover, it is expected that extreme weather conditions will occur more frequently. This involves floods, storms and tropical cyclones which will be more severe and thus cause even more damage than they do already today. Also, climatic zones will tend to move pole wards. Even if this shift will not lead to spectacular changes like desertification or flooding everywhere, yet its influence on natural systems will probably be considerable.

Many existing natural ecosystems will no longer be able to adjust quickly enough to changing circumstances and will thus be thoroughly disturbed or may even disappear. An example may be the death of tropical coral reefs by 'coral bleaching' as we see it today. Data collected this year (2000) demonstrate that all over the world already 25% of the reef systems has died within the last few years. One thing further to consider is the chance that the natural environment (the habitat) of many plant and animal species will move faster than those species can adapt to, so that their chances of survival are seriously threatened. Consequently, there is a serious risk that climate change will lead to a reduction of biological diversity .

The department's climate change research

The research activities of the department dealing with climatical changes, i.e. climate history and development , are grouped in three specific focus areas

  • Marine geology
  • Glaciology
  • Palaeolimnology

The purpose is to contribute to public and scientific understanding of the importance of climate change and its environmental impact, in particular with regard to past natural changes . This may help to make a better assessment of present changes with the purpose to improve predictions of future development of our climate and environment.

In order to understand the impacts of natural and anthropogenic changes on climate systems, it is essential to have knowledge of environmental conditions and natural variability prior to human settlement, and if possible, of the mechanism forcing these changes. Geological records are often the only tool to reconstruct past environmental conditions and to establish a long-term record of natural variability . Research in the department has concentrated on understanding how (North Atlantic) ocean circulation and climate change are linked, and how these affect the distribution of biological communities. Moreover, studies are made how the sedimentary record can be used to distinguish between natural and human-induced environmental change on local and regional scales. Also the study of natural hazards, such as submarine slides, form part of the department's research activities

Current research includes:

  • West Greenland ice sheet dynamics linked to climate and ocean circulation change (past ca 10,000 years)
  • Little Ice Age, a period of cooling (AD 1350 -1850), and other distinct climate changes of the recent past (Greenland, North Atlantic, Caribbean)
  • Long-term North Atlantic Current variability and deep water formation during the past 200,000 years
  • Study of the relationship between climatic changes and dynamics of the Greenland ice cap as well as circulation variability in (adjacent) ocean waters. Study of bottom melting processes at major North Greenland outlet glaciers and investigations of past circulation changes in the Nordic Seas and North Atlantic form part of the present research activities. Results indicate that both melting processes and (deep) ocean current variations play a major role at global climate change.
  • High resolution study of natural aquatic variability in Denmark
  • Interpretation of the dinoflagellate cyst assemblages in sedimentary profiles to determine the past climatic and environmental conditions in North Atlantic regions on time-scales ranging from the last few centuries to thousands of years.

Publications

Nørgaard-Pedersen, N., Mikkelsen, N., Lassen, S.J., Kristoffersen, Y. and Sheldon, E. 2007: Reduced sea ice concentrations in the Arctic Ocean during the last interglacial period revealed by sediment cores off northern Greenland. Paleoceanography, 22 , PA1218, doi:10.1029/2006PA001283, 15 pp.
Download as pdf-file 939 Kb

Nørgaard-Pedersen, N., Mikkelsen N., Kristoffersen, Y., 2007: Arctic Ocean record of last two glacial-interglacial cycles off North Greenland/Ellesmere Island — Implications for glacial history. Marine Geology 244 , 93–108
Download as pdf-file 1779 Kb

Wadhams, Peter and Amanatidis, Georgios, (eds), 2006: EUR 22416 - Artic Sea Ice Thickness:Past, Present and Future. SCIENTIFIC REPORT. Luxembourg: Office for Official Publications of the European Communities, 2006. Climate Change and Natural Hazards series 10. 293 pp.
Download as pdf-file 4102 Kb





Aage Bertelsen Gletscher and Smalle Spærregletscher, NorthEast Greenland
Aage Bertelsen Gletscher and Smalle Spærregletscher, North-East
Greenland. Results of studies of glaciers illustrate the global climate development.

Other web sites


Atlantic Ocean Ocean Floor panorama with ocean-bottom currents

Research team

       Atlantic Ocean Ocean Floor panorama with ocean-bottom currents


Edited by:
Antoon Kuijpers, GEUS - aku@geus.dk
Niels E. Poulsen, GEUS - nep@geus.dk


[Til top]   Sidst ændret: 15. december 2008 © De Nationale Geologiske Undersøgelser for Danmark og Grønland - GEUS
Øster Voldgade 10, 1350 København K - Tlf.: 38142000 - Fax: 38142050 - E-post: geus@geus.dk
Siden vedligeholdes af: Niels E. Poulsen


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