Glaciological investigations in Norway in 2007

An abstract characterisation of reduction operators Intuitively a reduction operation, in the sense intended in the present paper, is an operation that can be applied to inter-

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

Several parameters were recorded during each test ride: depth of snow, depth of compacted snow, depth of loose snow, depth of wheel tracks, unevenness in the snow, air

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