was closest to land in the following locations: 56 nm from Látrabjarg, 38 nm from Barði, 38 nm from Kögur and 50 nm from Hornbjarg. No large floes or icebergs were seen at the margin of the ice, but some scattered ice was seen off the ice edge.
An observation from ship off Víkuráll was received 20th March, describing a strip of ice and large dispersed floes, implying the need of caution for passing ships
/sea-ice/monthly/2011/nr/2374
Elvehøy, H., Guðmundsson, S., Hock, R., Machguth, H., Melvold, K., Pálsson, F., Radic, V.,
Sigurðsson, O. and Þorsteinsson, Þ.
The impact of climate change on glaciers and glacial runoff in the Nordic countries .......................................... 38
Radic, V. and Hock, R.
Volume changes of the glaciers in Scandinavia and Iceland in the 21st century
/media/ces/ces-oslo2010_proceedings.pdf
CMIP3 Multimodel Dataset: A New Era in Climate
Change Research. Bulletin of the Americal Meteorological Society, 88, 1383-1394.
Naki enovi , N. and R. Swart (Eds.) 2000: Emission Scenarios. A Special Report of Working
Group III of the Intergovernmental Panel on Climate Change. Cambridge University Press,
599 pp.
Räisänen, J. and L. Ruokolainen 2006: Probabilistic forecasts of near-term climate
/media/ces/CES_D2_2_poster_3x3.pdf
are not included. ............................................................. 36
32 Automatic records as a function of manual observations. ................................ 36
33 Frequency of present weather (SYNOP codes) observed by both stations. .......... 38
34 Frequency of present weather (SYNOP codes) observed by both stations without
the most frequent value (0
/media/vedurstofan-utgafa-2019/VI_2019_009.pdf