BORA - UiB

Bergen Open Research Archive

Arctic climate change: observed and modelled temperature and sea-ice variability

Bergen Open Research Archive

Show simple item record

dc.contributor.author Johannessen, Ola M.
dc.contributor.author Bengtsson, Lennart
dc.contributor.author Miles, Martin W.
dc.contributor.author Kuzmina, Svetlana I.
dc.contributor.author Semenov, Vladimir A.
dc.contributor.author Alekseev, Genrikh V.
dc.contributor.author Nagurnyi, Andrei P.
dc.contributor.author Zakharov, Victor F.
dc.contributor.author Bobylev, Leonid P.
dc.contributor.author Pettersson, Lasse H.
dc.contributor.author Hasselmann, Klaus
dc.contributor.author Cattle, Howard P.
dc.date.accessioned 2008-07-09T12:02:03Z
dc.date.available 2008-07-09T12:02:03Z
dc.date.issued 2004-07-09
dc.identifier.citation http://www3.interscience.wiley.com/journal/118775463/issue en
dc.identifier.issn 0280-6495 (print version)
dc.identifier.issn 1600-0870 (electronic version)
dc.identifier.uri http://dx.doi.org/10.1111/j.1600-0870.2004.00060.x
dc.identifier.uri http://hdl.handle.net/1956/2728
dc.description.abstract Changes apparent in the arctic climate system in recent years require evaluation in a century-scale perspective in order to assess the Arctic's response to increasing anthropogenic greenhouse-gas forcing. Here, a new set of century- and multidecadal-scale observational data of surface air temperature (SAT) and sea ice is used in combination with ECHAM4 and HadCM3 coupled atmosphere-ice-ocean global model simulations in order to better determine and understand arctic climate variability. We show that two pronounced twentieth-century warming events, both amplified in the Arctic, were linked to sea-ice variability. SAT observations and model simulations indicate that the nature of the arctic warming in the last two decades is distinct from the early twentieth-century warm period. It is suggested strongly that the earlier warming was natural internal climate-system variability, whereas the recent SAT changes are a response to anthropogenic forcing. The area of arctic sea ice is furthermore observed to have decreased ~8 x 105 km2 (7.4%) in the past quarter century, with record-low summer ice coverage in September 2002. A set of model predictions is used to quantify changes in the ice cover through the twenty-first century, with greater reductions expected in summer than winter. In summer, a predominantly sea-ice-free Arctic is predicted for the end of this century. en
dc.language.iso eng en
dc.publisher Blackwell Munksgaard en
dc.relation.ispartofseries Tellus A 56A(4) en
dc.subject Climatology en
dc.subject Meteorology en
dc.title Arctic climate change: observed and modelled temperature and sea-ice variability en
dc.type Peer reviewed en
dc.type Journal article en
dc.subject.nsi VDP::Matematikk og Naturvitenskap: 400 en
dc.subject.nsi VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Meteorologi: 453 en


Files in this item

 

This item appears in the following Collection(s)

Show simple item record

Search BORA


Browse

My Account