Jökull


Jökull - 01.10.1998, Side 6

Jökull - 01.10.1998, Side 6
servations is, however, not a complete cataloguing of all available evidence of that kind. The compilation of the regular observations of glacier variations in Ice- land presented here is, on the other hand, meant to be a complete catalogue of the data in the archives of the Iceland Glaciological Society from 1930 to 1995. The data published in this paper are available from the anonymous ftp site of the National Energy Au- thority in Iceland (net address: ftp.os.is, location: /publglacierslvariations, files: advret.zip or advret.gz). OBSERVATIONS OF GLACIER VARIATIONS IN ICELAND In addition to the work started by Jón Eyþórsson in the 1930s, the variations of glaciers in Iceland have been observed or derived by indirect means by sever- al other workers. Jón Eyþórsson (1935) wrote an arti- cle on the variation of Drangajökull from historical accounts. Sigurður Þórarinsson used information from annals and other sources to derive the variations of outlet glaciers from Drangajökull and of south flowing glaciers from Vatnajökull after 1690 (Tho- rarinsson, 1943; Þórarinsson 1974). He also used old historical accounts to derive the variations of Breiðamerkurjökull which has in recent centuries ad- vanced over a region which was populated for several centuries after the settlement of Iceland in the 9th century (Thorarinsson, 1941, 1956; Þórarinsson, 1974; Björnsson, 1996). F. Björnsson (1998) de- scribes information from various sources about the lo- cation of the terminus of Breiðamerkurjökull in this and the previous century and concludes that the re- treat of both Breiðamerkurjökull and other glaciers in the vicinity was very slow during the first quarter of the 20th century. Glaciers in Iceland are described in an extensive chapter in Thoroddsen's (1932) geographical descrip- - Yfirlitskort. 4 JOKULL, No. 45, 1998
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Jökull

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