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DIADEM - A monitoring and prediction system for the North Atlantic and Nordic seas. Proceedings from the PORSEC conference, Goa, India, 5-8 December 2000. 2000..
The DIADEM/TOPAZ monitoring and prediction system for the North Atlantic. 3rd EuroGOOS conference: Building the European capacity in Operational Oceanography, Athens, Greece 3-6 Dec 2002. Elsevier Oceanography Series. 2003..
Distribution of the northern water mass formation completing the Atlantic Meridional Overturning Circulation (talk). American Geophysical Union Fall Meeting. 2010..
Dypvannsdannelse i ny form. Cicerone (in Norwegian). 2002:20-22..
The effect of baroclinicity on the depth of neutral and stable planetary boundary layers. Quart, J. Roy. Met. Soc. 2003:3339-3356..
The effect of baroclinicity on the depth of neutrally stratified Ekman boundary layer. Abstracts: 27th EGS General Assembly, Nice, France, 21-26 April 2002. 2002..
The effect of large eddies on the convective heat/mass transfer over complex terrain: Advanced theory and its validation against experimental and LES data. Croatian Meteorological Journal. 2005:20-26.
Efficiency of high order numerical schemes for momentum advection. Journal of Marine Systems. 2007:31-46..
En ny istid truer?. Dagbladet. 2006..
Energy- and flux-budget (EFB) turbulence closure model for stably stratified flows. Part I: steady-state, homogeneous regimes. Boundary-layer Meteorology [Internet]. 2007;125:167-191. Available from: http://www.springerlink.com.pva.uib.no/content/l474p1v14h966357/.
Energy- and flux-budget (EFB) turbulence closure model for stably stratified flows. Part I: steady-state, homogeneous regimes. In: Atmospheric Boundary Layers: Nature, Theory and Applications to Environmental Modelling and Security. Atmospheric Boundary Layers: Nature, Theory and Applications to Environmental Modelling and Security. ; 2007. p. 11-35. Available from: http://www.springerlink.com.pva.uib.no/content/h813u00q9x3j2726/.
Energy- and flux-budget (EFB) turbulence closure model for stably stratified flows. Part II: The role of internal gravity waves. Boundary-Layer Meteorology. 2009..
Energy- and flux-budget turbulence closure model for stably stratified geophysical flows. In: 4th International Conference on Frontiers of Nonlinear Physics. 4th International Conference on Frontiers of Nonlinear Physics. 13 - 20 July, Nizhny Novgorod, Russia; 2010. p. ..
Energy-similarity a new turbulence closure model for stably stratified atmospheric boundary layers. Journal of Atmospheric Sciences. 2004..
Enhancement of turbulent mixing over thermally heterogeneous surfaces. General EGU assembly, 15-20 April, Vienna, Austria, Geophysical Research Abstracts, 9, 01057. 2007..
The ensemble Kalman filter for combined state and parameter estimation. Control systems magazine [Internet]. 2009;29:83-104. Available from: http://ieeexplore.ieee.org/xpl/freeabs_all.jsp?arnumber=4939313.
The Ensemble Kalman Filter: Theoretical Formulation and Practical Implementation. Ocean Dynamics. 2003:343-367..
An Ensemble Kalman Filter with a 1-D Marine Ecosystem Model. Journal of Marine Systems. 2002:75-100..
An Ensemble Kalman Filter with a complex marine ecosystem model: Hindcasting phytoplankton in the Cretan Sea. Annales Geophysics. 2002:1-13..
An Ensemble Kalman Smoother for Nonlinear Dynamics. Monthly Weather Review. 2000;128:1852-1867..
Ensemble-based data assimilation with an eddy-resolving model of the Gulf of Mexico. Doctoral Thesis No. 75. 2008..
Entrainment into sheared convective boundary layers as predicted by different large eddy simulation codes. 16th AMS Symposium on Boundary Layers and Turbulence, August 2004, Portland, Main. 2004..