2010, as seen at 12:00 GMT at an elevation of 3-3.6 km (10-12,000 ft). Light coloured, low-lying clouds of steam were observed over the eruption site, together with occasional bursts of grey to black-coloured cloud, which rise to up to half of the total height of the eruption plume. Above this level, the plume was lighter in colour with a capping of white cloud (not visible here
/about-imo/news/bigimg/1891
as in total during the 40 days of the Eyjafjallajökull eruption a year earlier, i.e. in spring 2010.
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/about-imo/news/bigimg/2421
the beginning of observations.
The year was sunny in Akureyri and the total number of
sunshine hours in Akureyri has only once been more.The winter (December 2020 to March 2021)
was in general favorable. Especially in the Southwest, where it was
relatively warm, dry and had particularly
little snow. It was wetter in the Northeast. Stormy weather
was rather uncommon this winter.
The spring
/about-imo/news/the-weather-in-iceland-in-2021
and the minimum was -17.9 on 29
December.
PrecipitationThe
precipitation was above the 1971 to 2000 mean at most stations. The
excess was largest in the East. Heavy
rainfall in the East and Southeast at
the
end of September resulted in extensive
flooding
from
major rivers in the area.
The
annual total in Reykjavík was 900.4 mm, 10 percent above the 1971 to
2000 mean. In Akureyri
/about-imo/news/the-weather-in-iceland-in-2017
on the map.
When future maps are viewed only the cloud cover forecast is displayed and not any observations.
Cloud cover forecasts appear as variegated patches over the country. The maps display cloud forecasts in eight units of cloudiness.
0/8 signifies a clear sky, 4/8 partly cloudy and 8/8 cloudy.
A forecast for total cloud cover is displayed, along with a forecast for low cloud and middle cloud
/weather/articles/nr/1219
networks. Two of these applications have now been funded: SVALI (Stability and Variations of Arctic Land Ice, ~40 million NOK applied for to the TRI), under the sub-programme Interaction between Climate Change and the Cryosphere of the TRI; and ICEWIND (Icing and Wind Energy Integration in Northern Norden, total budget ~25 million NOK, ~12 million NOK applied for to the TRI), under the sub-programme
/ces/nr/1978
Reference period: 1961 to 1990.
The total precipitation of 2009 in Reykjavík was 713 mm, which is about 10% below the 1961 to 1990 mean. This was the driest year in Reykjavík since 1995. The first part of the summer was unusually dry in Reykjavík and in most of the South and West. The total precipitation in Akureyri was 652 mm, which is more than 30% above the 1961 to 1990 mean
/weather/articles/nr/1802