Jökull - 01.12.1983, Page 12
12070), about 600 m of displacement had occurred
(Williams etal., 1974 and 1975).
Area calculations from Landsat images for Ice-
land’s glaciers have been carried out by Williams et
al., (1975), and Bjömsson (1980b). Bjömsson (1980b)
included some unpublished data of Williams, added
his own calculations, compared the results with
Thorarinssson’s previous area calculations (1958),
and showed the percentage decrease in area for each
of the principal glaciers of Iceland. Table 1
summarizes excerpts from the work of many
scientists who have calculated the area of Iceland’s
glaciers from published maps, aerial photographs,
and Landsat images.
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Bjömsson, H., 1975: Explanation ofjökulhlaups from
Grímsvötn, Vatnajökull, Iceland. Jökull 24: 1-
26.
Bjömsson, H., 1978: Könnun á jöklum med rafsegul-
bylgjum. Náttúrufraedingurinn 47 (3-4): 184-
194. (In Icelandic).
Bjömsson, H., 1980a: Glaciers in Iceland. Jökull 29:
74-80.
Bjömsson, H., 1980b: The surface area ofglaciers in
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Munzer, U. and J. Bodechtel, 1980: Digitale Ver-
arbeitung von Landsat-Daten úber Eis-und
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messung und Luftbildwesen 48: 21-28. (In
German)
Norlund, N.E., 1938: Denmark. Photogrammetric
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Pálsson, S., 1795 (unpub.): Forsög til en physisk,
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islandske Isbjorge i Anledning afen Reise til de
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Rist, S., 1967: Jöklabreytingar 1964/65, 1965/66 og
1966/67. Jökull 17: 321-325. (In Icelandic).
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10 JÖKULL 33. ÁR