Articles & Interviews
Sciencepoles articles look at key findings from a range of polar science and research fields. Our articles RSS feed will inform you when new articles are published on this website.
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Martin Jakobsson: Arctic Sea Ice Extent, Its History and How It Affects the Carbon Cycle
27.12.2011
Professor Martin Jakobsson is a professor at Stockholm University who has conducted extensive research on Arctic paleoclimates, with a focus on the oceanographic and environmental history of the planet’s polar oceans and their sea ice cover. Using geophysical mapping methods, he has also been involved in studying the morphology of…
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Martin Jakobsson: Investigating Arctic Paleoclimates
29.11.2011
A professor at Stockholm University who has conducted extensive research on Arctic paleoclimates, Professor Martin Jakobsson’s main research interests include the oceanographic and environmental history of the planet’s polar oceans and their sea ice cover. Using geophysical mapping methods, he has also been involved in studying the morphology of the seafloor.
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Bruno Delille: A Closer Look at Carbon Cycling in Antarctica
27.06.2011
Dr. Bruno Delille is a sea ice researcher and oceanographer from the University of Liège in Belgium. He has been involved in past research projects such as BELCANTO (BELgian research on Carbon uptake in the ANTarctic Ocean), which was studying carbon cycling (how carbon is cycled between atmosphere, marine life…
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The Measured and the Catastrophic: David Vaughan on Glacial and Ice Sheet Melt
03.05.2011
In a follow-up to an interview published last month on SciencePoles, Professor David Vaughan of the British Antarctic Survey (BAS) discusses his ongoing research, as well as current findings, estimates, questions, and discussions on the subject of glacial and ice sheet contribution to sea level rise. Professor Vaughan is a…
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David Vaughan on Ice2sea: Providing the IPCC with Sea Level Rise Projections
18.04.2011
Professor David Vaughan is a glaciologist who works for the British Antarctic Survey (BAS). His research focuses on glaciers and ice sheets, their response to climate change, and their contribution to sea level rise. He was a coordinating Lead Author for the 4th Assessment Report released by the Intergovernmental Panel…
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David Barber: Arctic Sea Ice in a Changing Climate
21.03.2011
David Barber is a sea ice specialist as well as a Professor of Environment and Geography and Canada Research Chair in Arctic System Science at the Centre for Earth Observation Science (CEOS) at the University of Manitoba in Winnipeg.
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Bruno Danis: SCAR-MarBIN, ANTABIF and the Importance of Keeping Tabs on Biodiversity in Antarctica
24.01.2011
Dr. Bruno Danis is a marine biologist from the Royal Belgian Institute of Natural Sciences who has spent a large part of his professional career working on biodiversity databases. Since 2005, he has been working on SCAR-MarBIN – the Scientific Committee on Antarctic Research (SCAR) Marine Biodiversity Information Network –…
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Konrad Steffen: Greenland Melt and the Complexities of Sea Level Rise
10.12.2010
Professor Konrad Steffen is the Director of the Cooperative Institute for Research in Environmental Sciences (CIRES)at the University of Colorado. He has been carrying out field research and monitoring in Greenland for twenty years. He is one of the world’s leading experts in measuring and modelling the response of the Greenland…
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Beyond Oslo: Milestones, Perspectives, and Priorities for International Polar Research
13.08.2010
With the passing of the International Polar Year 2007-08, the closing of the IPY Oslo Science Conference 2010, and the continuing growing importance of the Polar Regions within the public and scientific debate surrounding climate change, this begs the question: What next for international polar research?
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Mark Drinkwater on CryoSat-2 and its Mission
03.06.2010
With the successful launch of CryoSat-2 on 8th April 2010, the European Space Agency (ESA) has put a powerful new tool for observing the cryosphere into orbit. The new satellite’s primary mission will be to measure changes in the thickness of both sea ice and land ice.
