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    1928 research outputs found

    Mr. Edward Itta, Mayor of North Slope Borough, Alaska

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    Mr. Edward Itta, Mayor of North Slope Borough, Alaska talks here in the NRFP 6th open assembly in Hveragerði, Iceland, in September of 2011. The sessions name is Humanity, communities, Minds, Perceptions and Knowledge on Ice. His speech was excellent and showed the life of local communities in rural Alaska. Please click on the link above to see the video

    The Northern Research Forum, a case study for High Northern cooperation.

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    Margret Cela, University of Lapland, Finland / Iceland, talks here in the NRF 6th open assembly in Hveragerði, Iceland, in September of 2011. Please click on the link above to see the video

    Human Rights on Ice

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    Professor Guðmundur Alfreðsson, University of Strasbourg, France & University of Akureyri, Iceland, talks here in the NRF 6th open assembly in Hveragerði, Iceland, in September of 2011. Please click on the link above to see the video

    The state of the Arctic

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    Professor Matthias Finger, EPFL - the Ecole Polytechnique Fédérale de Lausanne, Switzerland, talks here in the NRF 6th open assembly in Hveragerði, Iceland, in September of 2011. Please click on the link above to see the video

    Sea Ice melting in Arctic

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    Yongjia Song, University of Wisconsin-Madison, USA / China, at the NRF 6th open Assembly in Hveragerði, Iceland. September 2011

    Arctic Shipping Development Prospects Evaluation: Nuclear Icebreaker Fleet in the Northern Sea Route.

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    Dr.Tatiana Khomiakova, Academy of National Economy, Russia, at the NRF 6th open Assembly in Hveragerði, Iceland. September 2011

    European Parliament resolution of 20 January 2011 on a sustainable EU policy for the High North

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    CROSS-POLAR AIRCRAFT TRAJECTORY OPTIMIZATION AND THE POTENTIAL CLIMATE IMPACT

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    Monograph describes the potential impact of aviation on climate change in the Arctic. It creates optimization algorithm to minimize climate impact of aircraft in terms of global warming potentials

    Temperature variations at the Great Wall and Zhongshan stations

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    Surface meteorological observations have been carried out at the Great Wall station (GW) and Zhongshan station (ZS) from 1984 to 2008 and from 1989 to 2008 respectively. The variation in mean air temperature and its trends are derived from the meteorological observation data recorded at both stations. The warming rate of the annual mean temperature at GW is similar to that at Bellingshausen station, which is about 3 km distant. Thus, the warming trend is representative of the King George Island region. The warming rate of ZS is less different from that at Davis station, which is about 100 km from ZS. It can be said that the meteorological data recorded at both stations are representative of the regions of the King George Island and east coast of the Antarctic

    Spatial heterogeneity of a microbial community in Kongsfjorden, Svalbard during late summer 2006 and its relationship to biotic and abiotic factors

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    The 16S and 18S ribosomal ribonucleic acid genes of microbial organisms collected from the contrasting environments (temperature, salinity, silicate, phosphate and nitrate, p <0.05) of the inner and outer basins of Kongsfjorden (Spitsbergen, Arctic) were studied using polymerase chain reaction-denaturing gradient gel electrophoresis(DGGE) fingerprinting. Comparison of the microbial fingerprints and the physicochemical parameters revealed that molecular methodology exhibited a greater sensitivity. Sequences obtained from bacterial DGGE were affiliated with four main phylogenetic groups of bacteria: Proteobacteria(Alpha, Beta and Gamma), Bacteroidetes, Verrucomicrobia and Cyanobacteria. The relationships between the genotype distribution of these microbes and associated biotic/abiotic factors, revealed by canonical correspondence analysis, showed that Station 1 at 30 m (outer fjord) was grouped separately from the other sites. This difference could be a consequence of the thermocline and base of the euphotic layer at this depth where the Atlantic and Arctic-type waters overlapped

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