Jökull


Jökull - 01.12.1969, Side 161

Jökull - 01.12.1969, Side 161
The Icelanders as a whole have therefore suffered from the damage caused by sea ice, and it is difficult to estimate statistically the loss of life and property involved. However, a few figures from more recent years will be mentioned in order to provide examples of mild ice years. Jn the ice year 1965, when the people of the eastern part of Iceland were the worst affect- ed, the cost of purchasing and transporting hay to that area amounted to 14,2 million Ice- landic krónur. During the comparatively mild ice year 1967, government compensation loans and hay trans- port subsidies totalled 18 million krónur. For the year 1968, which was a severer ice year, 15.1 million krónur were paid in compensa- tion loans and 4.7 million krónur in hay trans- port subsidies, amounting in all to about 20 million krónur. Taking the picture as a whole, the direct clamage for which compensation has been paid does not appear to be excessive. What is more serious is that during the 1967 ice year 870 kg less yield of hay were obtained per hectare than the average annual crop for the last 25 years. For 100,000 hectares this means a decrease of 87 million kg, the resulting loss amounting to 260 million krónur; a loss that reduced the basic product of Icelandic agriculture by one fifth compared with before. This figure does not include the loss of crop in grazing lands, or the ensuing shortage of raw material for other agricultural production, which was valu- ed that year at 2,300 million krónur. More frequent arrival of sea ice associated with a drop in mean temperature thus has similar effects on grass growth today as it did in the 18th century. The Icelanders are, how- ever, in a much better position as regards transport than they were, so that there is little question of famine. On the other hand, it is obvious that farming profits decline in pro- portion to rising operational costs, and con- stant drawing of fodder supplies from else- where may in some cases completely eliminate farming in some districts. REFERENCES Bergthórsson, P. 1966: Hitafar og búsælcl á fs- landi. Veðrið 11 (1), 15-20. Chritchfield, W. B. ir Little, E. L. 1966: Geo- graphic Distribution of the Pines of the World. U.S.D.A. Miscell. Publ. 991, Wash- ington, DC 97. Grímsstaðaannáll, 1933: Annálar 1400—1800 III, Hið íslenzka bókmenntafélag, Revkjavík, 435-657. Koch, L. 1945: The East Greenland Ice. Med- delelser om Grönland, 130 (3): 373. Löve, A. ir Löve, D. 1956: Cytotaxonomical Conspectus of the Icelandic Flora. Acta Horti. Gotoburgensis 20 (4): 65—290. Slefánsson, U. 1966: Plafið. Almenna bókafé- lagið, Reykjavík, 293. Sæmundsson, B. 1932: Spendýrin. Bókaverzlun Sigf. Eymundssonar, Reykjavík, 437. Thorarinsson, S. 1956: The Thousand Years Struggle against Ice and Fire. Mus. Nat. Hist. Iceland. Miscellaneous Papers, 11: 52. Thoroddsen, Þ. 1931: Lýsing íslands. ísafoldar- prentsmiðja, Reykjavík, I: 365; 1933: II: 683. — 1916: Árferði á íslandi í þúsund ár. Hið íslenzka fræðafélag, Kaupmannahöfn, 432. Veðráttan, 1951—68. Veðurstofa íslands, Rvík. JÖKULL 19. ÁR 157
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