Show simple item record

dc.contributor.authorLangehaug, Helene Reinertseneng
dc.date.accessioned2011-12-13T11:05:36Z
dc.date.available2011-12-13T11:05:36Z
dc.date.issued2011-12-09eng
dc.identifier.isbn978-82-308-1903-6 (print version)eng
dc.identifier.urihttp://hdl.handle.net/1956/5282
dc.description.abstractOcean heat transport and associated heat loss to the atmosphere contributes significantly to the anomalously mild climate of northwestern Europe and its variability. In this thesis, the circulation and transformation of water masses in the northern North Atlantic and the Nordic Seas have been assessed and explored in state-of-the-art climate models. A most important aspect of model evaluation is to identify the degree of realism in model climatology and variability, e.g., for model improvement or in order to assess the potential for decadal-scale climate prediction. A main approach for assessing simulated ocean circulations herein is water mass analysis as routinely applied in observational oceanography. Air-sea exchange and water mass transformation at northern high latitudes are accordingly related to the Atlantic Meridional Overturning Circulation (AMOC). The variable overturning of the Bergen Climate Model (BCM) – the core model system in this thesis – is found to reflect decadal variability in dense water formation in the Labrador Sea and in the oceanic heat transport into the Nordic Seas, the overall constraint on the northernmost water mass transformation. The simulated AMOC is strongly interconnected with the horizontal Subpolar Gyre circulation. Decadal variability of BCM’s Subpolar Gyre, as its AMOC, can partly be explained as a response to distinct patterns of atmospheric variability. The intercomparison of BCM with two other climate models finds the model pathways for the North Atlantic Current and the model sea-ice covers to differ substantially, and hence their oceanic poleward transport of heat, their air-sea exchange, and consequent northern water mass transformation to be very different.en
dc.language.isoengeng
dc.publisherThe University of Bergeneng
dc.relation.haspartPaper I: Langehaug H. R., P. B. Rhines, T. Eldevik, J. Mignot, and K. Lohmann, 2011: Water mass transformation and the North Atlantic Current in three multi-century climate model simulations. The article is available at: <a href="http://hdl.handle.net/1956/5278" target="blank">http://hdl.handle.net/1956/5278</a>eng
dc.relation.haspartPaper II: Langehaug, H. R., I. Medhaug, T. Eldevik, and O. H. Otterå, 2011: Arctic/ Atlantic exchanges via the Subpolar Gyre. The article is available at: <a href="http://hdl.handle.net/1956/5279" target="blank">http://hdl.handle.net/1956/5279</a>eng
dc.relation.haspartPaper III: Medhaug, I., H. R. Langehaug, T. Eldevik, T. Furevik, and M. Bentsen, 2011: Mechanisms for decadal scale variability in a simulated Atlantic Meridional Overturning Circulation, Climate Dynamics, in press. Full text not available in BORA due to publisher restrictions. The article is available at: <a href="http://dx.doi.org/10.1007/s00382-011-1124-z" target="blank"> http://dx.doi.org/10.1007/s00382-011-1124-z</a>eng
dc.relation.haspartPaper IV: Langehaug, H. R. and E. Falck, 2011: Changes in the properties and distribution of the intermediate and deep waters in the Fram Strait. The article is available at: <a href="http://hdl.handle.net/1956/5280" target="blank">http://hdl.handle.net/1956/5280</a>eng
dc.titleCirculation and transformation of Atlantic and Arctic water masses in climate modelseng
dc.typeDoctoral thesiseng
dc.subject.nsiVDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452eng
dc.rights.holderCopyright the authors. All rights reserved
dcterms.hasParthttp://hdl.handle.net/1956/5278
dcterms.hasParthttp://hdl.handle.net/1956/5279
dcterms.hasParthttp://dx.doi.org/10.1007/s00382-011-1124-z
dcterms.hasParthttp://hdl.handle.net/1956/5280


Files in this item

Thumbnail
Thumbnail

This item appears in the following Collection(s)

Show simple item record