1999
DOI: 10.1023/a:1001878013148
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On A Low Cloud Phenomenon At The Breidamerkurjökull Glacier, Iceland

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Cited by 5 publications
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“…Two mesoscale cyclonic vortices can be seen at the northeast and southwest corners of Iceland, resulting from the convergence between the environmental circulation and the local katabatic wind. In the afternoon, the near-surface winds feature an upslope pattern because of the higher temperature over land; the observational study by Kaltenböck and Obleitner (1999) suggests that coastal sea breezes are a frequent occurrence in summer. The exception is over the Vatnajökull ice cap where downslope winds persist (cf.…”
Section: A Near-surface Wind Climate Over Icelandmentioning
confidence: 99%
“…Two mesoscale cyclonic vortices can be seen at the northeast and southwest corners of Iceland, resulting from the convergence between the environmental circulation and the local katabatic wind. In the afternoon, the near-surface winds feature an upslope pattern because of the higher temperature over land; the observational study by Kaltenböck and Obleitner (1999) suggests that coastal sea breezes are a frequent occurrence in summer. The exception is over the Vatnajökull ice cap where downslope winds persist (cf.…”
Section: A Near-surface Wind Climate Over Icelandmentioning
confidence: 99%