Jökull


Jökull - 01.12.1986, Síða 67

Jökull - 01.12.1986, Síða 67
most of this year was very good. There were four summers that were good in most places: 1731, 1733 (see below), 1736 and 1739, and three cold ones: 1737, 1738 and 1740. 1732 was cold in the north but pleasant in the west. Several autumn seasons were characterized as “good”, otherwise they wére mostly wet. Sea ice occurred in only two years of this decade: in 1732 and 1733. In the first year, a northern source states: “Drift ice came in the spring and lay close into land until the end of August when it was seen last” (B.S. Skagafjarðarsýslá). Western sources do not rnention the ice. In 1733 also, the ice is only men- tioned in the north: “Cold near the sea because of drift ice which lay off the coast all summer” (B.S. Skagafjarðarsýsla). In spite of the presence of the ice, the summer of 1733 is mainly described as good by the sources.or at least, “good at the beginning” (B.S. Skagafjarðarsýsla). No sea ice is recorded during the most severe years of the decade, 1737 and 1738. These were severe for most of the time in all districts. In 1737, Ölfusvatnsannáll, written in the south, sug- gested that this was the worst winter since the “white winter” of 1632 to 1633. 1741-1750 The most obvious features of the 1740s were the cold weather and severe sea ice (see Figures 2 and 4). During 1741 to 1750, there were seven years when sea ice was present (1741, 1742, 1743, 1745, 1748, 1749, 1750). The most severe ice-year was 1745, when ice came early to the north and west and also reached the eastern and southern coasts. There were three winters which appear to have been severe in all regions: 1742, 1745 and 1750. As may be seen from Table 1, nine winters during this decade were severe ln at least one region for part of the winter. The only winter that was reported good in all available sources was 1748. Most of the springs during this decade were severe. The summers were frequently unfavourable, either dry or wet. In no year is a good summer reported in all regions (see Table 1). The autumns were often wet and stormy. 1745 stands out in this decade as having been an unusually severe year all over the country. The dis- tinctive feature of the winter seems to have been the intensity of the frost and the lack of snow. In the south there was: “No snow until 21 March but great frost. Frost in the ground was two ells deep” (Ölfus- vatnsannáll). In the west and northwest it was recorded as “The severest frost winter that people remember in recent times” (Grímsstaðaannáll, B.S. Isafjarðarsýsla). The lack of snow is also reported in the northwest: “Severe with heavy frosts from the be- ginning although in some places there was not so much snow” (B.S. Barðastrandarsýsla). The spring in the northwest was “almost as harsh as the winter with cold, frost and snow” (B.S. Barðastrandarsýslá). In the north it was “extremely severe” (Höskuldsstaða- annáll). The summer this year was “rather wet” in tlje south (Ölfusvatnsannáll) and in the north the weather improved at the end of June. In the east and west it re- mained severe, with frost in the ground past the end of August in the west (Grímsstaðaannáll). The autumn weather seems to have improved somewhat elsewhere, but in the east, “In September, in Fljótsdal in Múla district, there was ice one and a half ells deep in the ground” (B.S. Múlasýsla). 1751-1760 Another decade of very cold weather followed in the 1750s, with cold years occurring one after the other from 1751 to 1757 (see Table 2). The last three years of the decade, 1758, 1759 and 1760, were reasonably good and mild. According to the sources used here, sea ice was present in 1751, 1756, 1757, 1759 and 1760. From 1751 to 1757, almost all springs and winters were severe, at least in part, in most regions. The coldest year this decade (and one of the coldest in the eighteenth century) was 1756. Jón Jónsson re- corded “severe weather with snow and lack of pasture all winter”. The winter in the south was “very severe with frost and snow” (B.S. Árnessýsla) and there was “a harsher spring than anyone could remember” (B.S. Árnessýsla). In the west and east the winter was also severe. Jón Jónsson records that by the “ninth week of summer” (c. 15 June) the snow had begun to melt but that there was still snow on the ground three weeks later. The situation was very similar in other parts of Iceland. In the south, “the cold and frost were so severe right up to 6 August that small ponds and streams froze almost every night, although they thawed out during the day” (B.S. Árnessýslá). In the west, one source commented: “The worst thing of all is this summer’s severity” (B.S. Dalasýsla). Sea ice surrounded the country this year. It first came to the north in March, and then spread along the eastern and southem coasts. One southern source recorded: “Drift ice came to the south on 24 June and began to break up on 6 July” (B.S. Árnessýsla). All the northern sources agree that the ice remained off the north coast until the end of August. In coastal districts there was also wet weather associated with the ice: “There was 65
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