Biblio
Filtre: Forfatter er Otterå, Odd Helge [Slett Alle Filtre]
Climate change under aggressive mitigation: the ENSEMBLES multi-model experiment. Climate Dynamics. 2011;37(9-10):1975 - 2003.
. Bergen earth system model (BCM-C): model description and regional climate-carbon cycle feedbacks assessment. Geoscientific Model Development [Internett]. 2010;3. Available from: www.geosci-model-dev.net/3/123/2010/ Abstract
. 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.
. 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 [Internett]. 2008;25:213-226. Available from: http://www.springerlink.com.pva.uib.no/content/x168400650131116/ Abstract
. Global climate model simulations of Holocene climate variability. 3rd Nansen-Zhu Center Summer School on Climate teleconnection between low and high latitudes. 2008.
. Vulkanar i drivhuset. Klima. 2008:27-28.
. 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.
. Bjerknes Centre for Climate Research - combining past, present and future climate change. Norwegian Journal of Geology. 2005;85:33-44.
. What happens with the Arcto-Norwegian cod if the thermohaline circulation slows down?. GLOBEC International Newsletter. 2005;11.
. 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 [Internett]. 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 Abstract
. Effects of solar irradiance forcing on the ocean circulation and sea-ice in the North Atlantic in an isopycnic coordinate ocean general circulation model. Tellus A [Internett]. 2004;56:154-166. Available from: http://www.blackwell-synergy.com/doi/pdf/10.1111/j.1600-0870.2004.00046.x Abstract
. A possible feedback mechanism involving the Arctic freshwater, the Arctic sea ice, and the North Atlantic Drift. Advances in Atmospheric Sciences [Internett]. 2004;21:784-801. Available from: http://www.iap.ac.cn/publ/aas/ Abstract
. Ingen ny istid i Noreg. Cicerone (KlimaProg). 2004.
. The sensitivity of the present-day Atlantic meridional overturning circulation to freshwater forcing. Geophysical Research Letters. 2003;30. Abstract
. The sensitivity of the North Atlantic-Arctic climate system to isostatic elevation changes, freshwater and solar forcings. Doctoral Thesis No. 41. 2003.
. Modelling late Cenozoic isostatic elevation changes in the Barents Sea and their implications for oceanic and climate regimes: preliminary results. Quaternary Science Reviews [Internett]. 2002;21:1643-1660. Available from: http://www.sciencedirect.com.pva.uib.no/science/article/pii/S0277379102000185



