Glaciological investigations in Norway in 2009

“Synthetic decision making”. These games, designed as simplified land combat simulation models, are defined and some of their properties described. We give a theoretical and

The Autodyn simulation code with the smooth particle hydrodynamic (SPH) method and Impetus Afea Solver with the corpuscular model are used and the results are compared with

Fig. Modeling is done with the composite-roughness surface scattering kernel for the same type of bottom as in Fig. There are 10 dB between the thick marks on the vertical axes.

Faraday rotation receivers on the rocket and the EISCAT UHF incoherent scatter radar provided simulta- neous electron density profiles whereas the ALOMAR Na lidar and meteor

[2012] revisited the spacecraft potential technique and used calibrated Cluster data combined with measurements of solar irradiance to calculate more accurate cold plasma density

The winter maximum probably occurred around 5 th May (www.senorge.no). Based on the snow depth measurements the spatial distribution of the winter balance was interpolated using

Altitudinal distribution of winter, summer and annual mass balance at Rembesdalskåka in 2019. Based on the snow depth measurements the spatial distribution of the winter balance was

Altitudinal distribution of winter, summer and annual mass balance at Rembesdalskåka in 2020. Based on the snow depth measurements the spatial distribution of the winter balance was