Fróðskaparrit - 01.01.2002, Side 107

Fróðskaparrit - 01.01.2002, Side 107
ARKTISKA FJALLAVEÐRIÐ í 2000 Á SORNFELLI 105 0 45 90 135 180 225 270 315 380 Winđ direction, degrees Figure 9. Windchill as a function ofwind direction at tlie Sornfelli meteorological station. The windchill values are calculated hased on tlie corrected air temperature data for 2000. for the Sund station was 7.3°C, a value somewhat warmer than the Torshavn 1961 - 1990 annual mean of 6.5°C (Table 1). The mean annual lapse rate was -0.0077°C/m (Fig. 10). This value is well above the standard value of -0.0065°C/m (Ahrens, 2000) for oceanic regions, and shows that the atmosphere in general is un- stable. Winter lapse rates generally between -0.007°C/m and -0.009°C/m, and summer values of -0.004°C/m and -0.005°C/m are recorded for temperatures close to the ground surface in the Slættaratindur moun- tain area, in the northern part of the Faroe Islands, in the period 1995-2001 (Chris- tiansen and Humlum, submitted). The sea- sonal variation in the lapse rate (Fig. 10) shows the atmosphere to be generally unstable all the year, but with several sum- mer periods with stable conditions, when values above -0.0065°C/m occur. During summer temperature inversions occurred primarily during calm conditions, when the Sornfelli mountain received more direct insulation than the more shaded, lower located Kaldbaksfjørður valley, where also moist air and fog occurred at the coast. Freezing, thawing and growing indices at Sornfelli The corrected air temperature (Fig. 6) was used to calculate freezing, thawing and growing degree days (FDD, TDD and GDD) (Andersland and Ladanyi, 1994; Molau and Mølgárd, 1996) at Sornfelli (Fig. 11), based on daily mean air tempera- tures. The annual TDD sum of 973 is much larger than the 361 FDD sum, indicating a positive ground thermal regime without permafrost. The annual sum of GDD is 160, which is significantly less than found at the same al- titude at the Slættaratindur area by Hum- lum and Christiansen (1998b, Fig. 5: 178), based on ground surface temperatures. Discussion The new concept of the Sornfelli meteoro- logical station, with a heated cylinder hous- ing the instruments in an advanced auto-
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