We have compared differences between radiosonde observations in SW-Iceland and 48 hour forecast by a numerical weather prediction model over a period of five years (2000-2004). Temperature and height of the pressure levels of 925, 850 and 500 hPa were compared in search for systematic errors. In the overall mean, the predictions have little error and very limited bias. There are however slight seasonal variations and indications of situations where the model does relatively poorly. At 500 hPa there is a cold bias in the forecasts in late winter, but no such bias in the autumn and early winter. At the lowest level there is a tendency of a cyclonic bias in the forecasted wind direction in northeasterly winds and in westerly flow, there is a w...
Spatial distribution of precipitation in complex terrain can be very uneven and there are many facto...
For a targeted observations case, the dependence of the size of the forecast impact on the targeted ...
The spatial and temporal distributions of a cold air outbreak (CAO) event over the Iceland- and sout...
We have compared differences between radiosonde observations in SW-Iceland and 48 hour forecast by a...
Forecasts of the 8 January Denmark Windstorm are compared. In a wrong forecast, the Greenland-lee lo...
The water equivalent of snow on the ground is calculated from snow observations from Hveravellir, Ic...
Abstract: Forecasts of the 8 January Denmark Windstorm are compared. In a wrong forecast, the Greenl...
The weather and climate in Iceland is to a large degree governed by synoptic scale weather systems a...
Katabatic flows during the night of 11–12 August 2004 in Iceland are studied using observations and ...
The climatology of mean bias errors (relative to 1-day forecasts) was examined in a 20-year hindcast...
Atmospheric flow over Iceland has been simulated for the period September 1987 through June 2003, us...
The variability of the North Atlantic Oscillation is a key aspect of Northern Hemisphere atmospheric...
The study of atmospheric chemistry relies on data from weather models to determine how air parcels m...
Abstract: Flow over Iceland has been simulated over a fifteen year period using the PSU/NCAR MM5 mes...
A satellite image of blowing dust is compared to a simulation of winds during a major erosion event ...
Spatial distribution of precipitation in complex terrain can be very uneven and there are many facto...
For a targeted observations case, the dependence of the size of the forecast impact on the targeted ...
The spatial and temporal distributions of a cold air outbreak (CAO) event over the Iceland- and sout...
We have compared differences between radiosonde observations in SW-Iceland and 48 hour forecast by a...
Forecasts of the 8 January Denmark Windstorm are compared. In a wrong forecast, the Greenland-lee lo...
The water equivalent of snow on the ground is calculated from snow observations from Hveravellir, Ic...
Abstract: Forecasts of the 8 January Denmark Windstorm are compared. In a wrong forecast, the Greenl...
The weather and climate in Iceland is to a large degree governed by synoptic scale weather systems a...
Katabatic flows during the night of 11–12 August 2004 in Iceland are studied using observations and ...
The climatology of mean bias errors (relative to 1-day forecasts) was examined in a 20-year hindcast...
Atmospheric flow over Iceland has been simulated for the period September 1987 through June 2003, us...
The variability of the North Atlantic Oscillation is a key aspect of Northern Hemisphere atmospheric...
The study of atmospheric chemistry relies on data from weather models to determine how air parcels m...
Abstract: Flow over Iceland has been simulated over a fifteen year period using the PSU/NCAR MM5 mes...
A satellite image of blowing dust is compared to a simulation of winds during a major erosion event ...
Spatial distribution of precipitation in complex terrain can be very uneven and there are many facto...
For a targeted observations case, the dependence of the size of the forecast impact on the targeted ...
The spatial and temporal distributions of a cold air outbreak (CAO) event over the Iceland- and sout...