Biblio
Filtre: Forfatter er Bentsen, Mats [Slett Alle Filtre]
Early Eocene Asian climate dominated by desert and steppe with limited monsoons. Journal of Asian Earth Sciences 44, (2012).
Bergen earth system model (BCM-C): model description and regional climate-carbon cycle feedbacks assessment. Geoscientific Model Development 3, (2010). Abstract
Ocean biogeochemistry in the Norwegian Earth System Model version 2 (NorESM2). Geoscientific Model Development 13, (2020).
External forcing of the early 20th century Arctic warming. Tellus. Series A, Dynamic meteorology and oceanography 65, (2013).
Role of the atmospheric and oceanic circulation in the tropical Pacific SST changes. Journal of Climate 21, 2019-2034 (2008).
Lovende resultater for nyutviklet klimamodell. Cicerone (RegClim) 16-19 (2002).
Økt CO2 gir forandring i sirkulasjonsmønsteret. Cicerone (RegClim) 30-32 (2002).
Overview of the Norwegian Earth System Model (NorESM2) and key climate response of CMIP6 DECK, historical, and scenario simulations. Geoscientific Model Development 13, (2020).
Mechanisms for variable North Atlantic-Nordic seas exchanges. Journal of Geophysical Research (JGR): Oceans 117, (2012).
Climate evolution of the last six centuries as simulated by Bergen Climate Model: the role of natural forcing. EGU General Assembly 2009 11, (2009).
The sensitivity of the present-day Atlantic meridional overturning circulation to freshwater forcing. Geophysical Research Letters 30, (2003). Abstract
Simulated pre-industrial climate in Bergen Climate Model (version 2): model description and large-scale circulation features. Geoscientific Model Development (2009).
Simulating transport of 129I and idealized tracers in the northern North Atlantic Ocean. Environmental Fluid Mechanics (2010).doi:10.1007/s10652-009-9138-3 Abstract
Simulated North Atlantic -Nordic Seas water mass exchanges in an isopycnic coordinate OGCM. Geophysical Research Letters 30, 1536-1539 (2003). Abstract
Mechanisms for decadal scale variability in a simulated Atlantic meridional overturning circulation (paper). Climate Dynamics (2012).doi:DOI 10.1007/s00382-011-1124-z
Mechanisms for decadal scale variability in a simulated Atlantic Meridional Overturning Circulation. Climate Dynamics 39, (2012).
Mechanisms for decadal scale variability in the North Atlantic Ocean circulation in the Bergen Climate Model (talk). European Geophysical Union (2012).
A possible mechanism for the strong weakening of the North Atlantic subpolar gyre in the mid-1990s. Geophysical Research Letters 36, (2009).
Response of the North Atlantic subpolar gyre to persistent North Atlantic oscillation like forcing. Climate dynamics 32, 273-285 (2008). Abstract
Mechanisms for decadal scale variability in the North Atlantic Ocean circulation in the BCM (talk). Joint ASOF/THOR workshop (2011).
Simulated Atlantic Meridional Overturning Circulation in the 20th century with an ocean model forced by reanalysis-based atmospheric data sets. Ocean Modelling 100, 31 - 48 (2016).
