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Climate evolution of the last six centuries as simulated by Bergen Climate Model: the role of natural forcing. EGU General Assembly 2009. 2009;11..
Current climate change in the perspective of past variations: Forcing and response of the climate system. The winter conference of Norsk Geologisk forening. 2009..
Global climate model simulations of Holocene climate variability. 3rd Nansen-Zhu Center Summer School on Climate teleconnection between low and high latitudes. 2008..
Bergen earth system model (BCM-C): model description and regional climate-carbon cycle feedbacks assessment. Geoscientific Model Development [Internet]. 2010;3. Available from: www.geosci-model-dev.net/3/123/2010/.
Bjerknes Centre for Climate Research - combining past, present and future climate change. Norwegian Journal of Geology. 2005;85:33-44..
Climate change under aggressive mitigation: the ENSEMBLES multi-model experiment. Climate Dynamics. 2011;37(9-10):1975 - 2003.
Diapycnal mixing in transient response of the Atlantic meridional overturning circulation in an enhanced freshwater perturbation experiment. Atmospheric and oceanic science letters [Internet]. 2010;3. Available from: http://www.iapjournals.ac.cn/aosl/ch/reader/new_year_article.aspx?year_id=2010&quarter_id=4.
Impacts of a reduced thermohaline circulation on transports and growth of larvae and pelagic juveniles of Arcto-Norwegian cod (Gadus morhua). Fisheries Oceanography. 2007;16:216-228..
Inception of the Northern European ice sheet due to contrasting ocean and insolation forcing. Quaternary Research. 2007;67:128-135..
Interannual to decadal climate predictability: A multi-perfect-model-ensemble study. Journal of Climate. 2006;19:1195-1203..
Modelling late Cenozoic isostatic elevation changes in the Barents Sea and their implications for oceanic and climate regimes: preliminary results. Quaternary Science Reviews [Internet]. 2002;21:1643-1660. Available from: http://www.sciencedirect.com.pva.uib.no/science/article/pii/S0277379102000185.
A possible feedback mechanism involving the Arctic freshwater, the Arctic sea ice, and the North Atlantic Drift. Advances in Atmospheric Sciences [Internet]. 2004;21:784-801. Available from: http://www.iap.ac.cn/publ/aas/.
The sensitivity of the present-day Atlantic meridional overturning circulation to freshwater forcing. Geophysical Research Letters. 2003;30..
Simulated pre-industrial climate in Bergen Climate Model (version 2): model description and large-scale circulation features. Geoscientific Model Development. 2009..
Simulating the effects of the 1991 Mount Pinatubo volcanic eruption using the ARPEGE atmosphere general circulation model. Advances in Atmospheric Sciences [Internet]. 2008;25:213-226. Available from: http://www.springerlink.com.pva.uib.no/content/x168400650131116/.
Transient response of the Atlantic Meridional Overturning Circulation to enhanced freshwater input to the Nordic Seas - Arctic Ocean in the Bergen Climate Model. Tellus A [Internet]. 2004;56:342-361. Available from: http://www.blackwell-synergy.com/servlet/useragent?func=synergy&synergyAction=showTOC&journalCode=tea&volume=56&issue=4&year=2004&part=null.
Vulkanar i drivhuset. Klima. 2008:27-28..
What happens with the Arcto-Norwegian cod if the thermohaline circulation slows down?. GLOBEC International Newsletter. 2005;11..
Ingen ny istid i Noreg. Cicerone (KlimaProg). 2004..