Fróðskaparrit - 01.01.2002, Qupperneq 109

Fróðskaparrit - 01.01.2002, Qupperneq 109
ARKTISKA FJALLAVEÐRIÐ í 2000 Á SORNFELLI 107 The lower limit of the ET climate type is located where the mean air temperature of the warmest month is 10°C, corresponding to the tree limit. Using the Sornfelli mean August air temperature of 6.5 °C and the lo- cal August lapse rate of -0.0068°C/m, the limit between the polar and temperate cli- mate is located at 216 m asl. in the Sornfel- li region in the year 2000. Thus the data from the Sornfelli meteorological station emphasize that about 68% (Fig. 1) of the land area of the islands had a polar climate in 2000. The lower limit of the periglacial zone, based on the distribution of peri- glacial landforms in the Faroe Islands, have previously been located at 250-450 m asl. (Humlum and Christiansen, 1998a;b) (see Fig. 1), which corresponds very well with the suggested 200 m asl. lower limit of the low arctic. Biogeographically, Tuhkanen (1987) located the Faroe Islands in the hemiboreal zone at sea level, but with a hemioroarctic zone in areas above 700 m. He stressed that even lower oroarctic zones may well be found at levels below 700 m asl. His vertical zonation is based on mete- orological data from the 1931-1960 period, which was slightly warmer than the 1961- 1990 period, and on a too low standard Fennoscandinavian lapse rate of only -0.0053°C/m, as he did not have access to any local lapse rates. Therefore his arctic zone probably would also be significantly lowered using the Sornfelli meteorological data. The potential tree line has been locat- ed at 150 m asl. (Ødum, 1991) and later at 300 m asl. (Feivsson, 1993) for sheltered locations. These values also largely agree with the lower boundary of the low arctic zone located around 200 m asl. Traditionally the polar climate of the northern Hemisphere is also known as the arctic climate. In the southern parts a low arctic climate exist, in which the mean air temperature of the warmest month is below 10°C, but above 5°C. At the highest moun- Figure II. Cumulative indices offreezing (FDD), thawing (TDD) anci growing (CDD) degree daysfor the year 2000 at Sornfelli, calculatedfrom the corrected air temperature data. L
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