Jørgen S Christiansen

Prof. Jørgen S Christiansen


Research Focus & Metrics

Academic Career Length

36Years (1991-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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16 December 2013 in Global Change Biology
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Journal Article
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JCJørgen S Christiansen
Jørgen S Christiansen
CMCatherine W. Mecklenburg
Catherine W. Mecklenburg
OKOleg V. Karamushko
Oleg V. Karamushko
In light of ocean warming and loss of Arctic sea ice, harvested marine fishes of boreal origin (and their fisheries) move poleward into yet unexploited parts of the Arctic seas. Industrial fisheries, already in place on many Arctic shelves, will radically affect the local fish species as they turn up as unprecedented bycatch. Arctic marine fishes are indispensable to ecosystem structuring and functioning, but they are still beyond credible assessment due to lack of basic biological data. The time for conservation actions is now, and precautionary management practices by the Arctic coastal states are needed to mitigate the impact of industrial fisheries in Arctic waters. We outline four possible conservation actions: scientific credibility, ‘green technology’, legitimate management and overarching coordination.

8 March 2012 in Polar Biology
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Journal Article
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JCJørgen S Christiansen
Jørgen S Christiansen
HHHaakon Hop
Haakon Hop
ENEinar M. Nilssen
Einar M. Nilssen
JJJohn Joensen
John Joensen


10 December 2022 in Nature Communications
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CGCaroline V. B. Gjelstrup
Caroline V. B. Gjelstrup
MSMikael K. Sejr
Mikael K. Sejr
LSLaura de Steur
Laura de Steur
JCJørgen S Christiansen
Jørgen S Christiansen
MGMats A. Granskog
Mats A. Granskog
CSColin A. Stedmon
Colin A. Stedmon
The Northeast Greenland shelf (NEGS) is a recipient of Polar Water (PW) from the Arctic Ocean, Greenland Ice Sheet melt, and Atlantic Water (AW). Here, we compile hydrographical measurements to quantify long-term changes in fjords and coastal waters. We find a profound change in the vertical distribution of water masses, with AW shoaling >60 m and PW thinning >50 m since early 2000’s. The properties of these waters have also changed. AW is now 1 °C warmer and the salinity of surface waters and PW are 1.8 and 0.68 lower, respectively. The AW changes have substantially weakened stratification south of ~74°N, indicating increased accessibility of heat and potentially nutrients associated with AW. The Atlantification earlier reported for the eastern Fram Strait and Barents Sea region has also propagated to the NEGS. The increased presence of AW, is an important driver for regional change leading to a likely shift in ecosystem structure and function.

13 January 2016 in The Science of Nature
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JCJørgen S Christiansen
Jørgen S Christiansen
EBErik Bonsdorff
Erik Bonsdorff
IBIngvar Byrkjedal
Ingvar Byrkjedal
SFSvein-Erik Fevolden
Svein-Erik Fevolden
OKOleg V. Karamushko
Oleg V. Karamushko
RWRupert M. Wienerroither
Rupert M. Wienerroither

18 February 2015 in Diversity and Distributions
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JCJørgen S Christiansen
Jørgen S Christiansen
MSMaria Sparboe
Maria Sparboe
BSBjørn‐S. Sæther
Bjørn‐S. Sæther
SSSten I. Siikavuopio
Sten I. Siikavuopio