Jökull


Jökull - 01.12.1988, Side 65

Jökull - 01.12.1988, Side 65
Fig. 4 Average annual precipitation 1931-1960 in southwestem Iceland (mm). Mynd4. Meðalársúrkoma suðvestanlands 1931-1960 (mm). two weather stations, Reykjavík and Eyrarbakki, located on each side of the Reykjanes mountains. Highest monthly values occur in October while May and June are the driest months of the year. As an average for the country as a whole October’s share of the annual precipitation is about 12% and that of May about 5%. This is in agreement with the fact that average surface pressure is usually highest in spring but lowest in early winter. The fact that precipitation is larger in early winter than late winter can at least partly be explained by the fact that temperature is higher in the former period and consequently the moisture content too. Monthly values of precipitation show large year- to-year variation and months with no precipitation at all exist. Fig. 4 shows the distribution of annual precipita- tion 1931-1960 in southwestem Iceland. As a large part of the precipitation falls with winds between east and south, which prevail in the forward part of cyclones arriving from the southwest, it is to be expected that the highest precipitation values are found windward and in the mountains, with decreas- ing values on the leeward side. This is confirmed by the distribution. Values of 3000 mm or more are found in the mountain areas. The values decrease to 800 mm in Reykjavík which, because of the rain shadow, is the minimum area of the investigated region. From Reykjavík there is consequently a rapid increase in precipitation towards the JÖKULL, No. 38, 1988 63
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