Fróðskaparrit - 01.01.2002, Side 105

Fróðskaparrit - 01.01.2002, Side 105
ARKTISKA FJALLAVEÐRIÐ í 2000 Á SORNFELLI 103 Figure 7. Tlie 10 minutes mean wind speed for year 2000from the Sornfelli station. The mean annual wind speed is shown. Only a 41.34 m/s valuefrom the 31 March was removed from thefigure, andfrom 4 September values above 40 m/s was filtered out. 7 and 8). The distribution of the wind direction data for year 2000 (Fig. 8) shows three dominating wind directions from the north, southeast and southwest. The mountain set- ting of the Sornfelli station causes topo- graphic effects on the measurements. The cylinder will produce some airflow distor- tion. The effect of this has not been investi- gated. The data, however, demonstrates that the measuring site is not dominated by strong turbulence. This would have pro- duced significant variation in the wind speed values and a more uniform distribu- tion of the direction frequencies. This indi- cates that the Sornfelli station is successful- ly located for recording the general wind pattern. Presumably it is suffering from sonte lee effects, from the slightly higher located, northern part of the plateau. The gust winds with a 10 min mean wind speed above 15 m/s (Fig. 8) show that most of the storms during 2000 came from southwest. Storms from the southeast oc- curred only in January and February, while northerly storms occurred in March, April, November and December. The southwest- erly storms dominated in the spring. Al- though the summer was generally calm, 32- sec gusts of up to 28 nt/s did occur 13 June. The highest gusts recorded during 2000 were 30 m/s for the 32 sec gust 1 January, and 40.7 m/s for the 2 sec gust 3 January. Windchill The mean annual windchill value (U.S. Na- tional Weather Service, 2001) calculated based on the corrected air temperature data at Sornfelli is -7.07°C. This is 8.77°C low- er than the MAAT value, and shows the sig- nificant cooling of the mountain due to wind activity. The relationship between windchill values and wind direction (Fig. 9) shows that the coldest winds primarily come from the north and some from the southwest, whereas winds in the sector from east to southwest predominantly bring winds with windchill values frorn +5°C to
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