Biblio
Filters: Author is Kvamstø, N. G. [Clear All Filters]
Certain aspects of high-latitude climate variability. 188 (2014).
Simulated pre-industrial climate in Bergen Climate Model (version 2): model description and large-scale circulation features. Geoscientific Model Development (2009).
Sensitivity of simulated wintertime Arctic atmosphere to vertical resolution in the ARPEGE/IFS model. Climate Dynamics 30, 687-701 (2008). Abstract
Download: Byrkjedal_et_al_220606.pdf (1.26 MB)
Applications of extreme value theory in temperature records in Extra-tropical and Arctic regions. Doctoral Thesis No. 76 (2008).
A Cautionary Note on the Use of the Kolmogorov-Smirnov Test for Normality. Monthly Weather Review 135, 1151-1157 (2007).
Sensitivity of simulated wintertime Arctic atmosphere to vertical resolution in the ARPEGE/IFS model. Open science conference Polar Dynamics: Monitoring, Understanding, and Prediction, August 29-31, Bergen, Norway (2007).
Effects of simulated natural variability on Arctic temperature projections. Geophysical Research Letters 32, (2005). Download: 2005GL023404.pdf (306.73 KB)
Ingen ny istid i Noreg. Cicerone (KlimaProg) (2004).
The sensitivity of the present-day Atlantic meridional overturning circulation to freshwater forcing. Geophysical Research Letters 30, (2003). Abstract
Download: 2003GL017578.pdf (517.4 KB)
Description and evaluation of the Bergen climate model: ARPEGE coupled with MICOM. Climate Dynamics 27-51 (2003).
Lovende resultater for nyutviklet klimamodell. Cicerone (RegClim) 16-19 (2002).
Økt CO2 gir forandring i sirkulasjonsmønsteret. Cicerone (RegClim) 30-32 (2002).
The Bergen Climate Model (BMC) - a fully coupled, global atmosphere-sea ice-ocean climate Model. China-Norway Joint Symposium on Polar Science, July 30 - August 2, Shanghai, China (2001).
Ny modell gir mer realistiske klimaberegninger. Cicerone 28-31 (2000).
Preliminary results from a coupled atmosphere-ocean-sea ice model. RegClim, General Technical Report, 4/2000 (2000).
Technical Coupling of ARPEGE/MICOM. RegClim, General Technical Report, 5/2000 45-57 (2000).
