(ten years) and for easy navigation the buttons + 10 and - 10 (top left) take you a decade back or forth.
The weather at six o'clock on Christmas Eve is also available.
Additionally, snow cover and snow depth at Christmas morning are listed for 1921 - 2006. A table shows snow cover in quarters where 0 means no snow and 4 means complete cover. When that criteria is met, snow depth is given
/about-imo/news/nr/1424
on data from two models. The first 48 hours will be based on HIRLAM from the Danish Meteorological Office, DMI, whereas forecasts for the third to seventh day will be based on a model from ECMWF.
Avalanche conditions are now given on a selected front page. Additionally, a forecast of avalanche danger for selected highland areas will be given twice a week. This risk estimate is designed
/about-imo/news/nr/2622
of Krossá is unusually high, with a value of 300 µS cm−1 recorded yesterday.
Additionally, the conductivity of Steinholtsá was over 170 µS cm−1 today, which is an
abnormally high level, unless geothermal water is entering the catchment. Ash fall or ash-
polluted snow are possible reasons for the high conductivity of Steinsholtsá. Likewise, lava
from the former Fimmvörðuháls eruption could also
/media/jar/Eyjafjallajokull_status_2010-04-28_IES_IMO.pdf
A minor glacial outburst flood in Skaftá
Warning - jökulhlaup in progress
23.6.2016
Within recent days, the level of the Skaftá river at Sveinstindur has risen slowly. Additionally electrical conductivity readings from the same location have increased
/about-imo/news/a-minor-glacial-outburst-flood-in-skafta
caldera. They have been meeting over the weekend to analyse recent measurements and assess the situation.The overflights were made with helicopter support from the
Icelandic Coastguard and an aircraft from Isavia. Additionally, water samples,
measurements of electrical conductivity and gas levels were made on the ground at
Kvíárjökull, a valley glacier on the southeastern flank of Öræfajökull
/about-imo/news/monitoring-oraefajokull
but the latest measurements show a slight decrease. Additionally, the discharge of both rivers is lower than earlier in the week.
The photo above was taken in the evening of 8 July 2014. It shows the new bridge over Múlakvísl (south-east of Mýrdalsjökull). In recent days a small flood was coming out of Kötlujökull and went down Múlakvísl.
At Sólheimajökull, geothermal gases continue to be released from
/about-imo/news/nr/2917
the level of Gígjukvísl began to rise steadily. Additionally, the electrical conductivity of the river has increased markedly, signifying the presence of geothermal solutes. According to information from the Institute of Earth Sciences, University of Iceland, the volume of water available for drainage is 0.2 - 0.3 cubic kilometres. This volume is similar to floods from Grímsvötn in November 2012
/about-imo/news/nr/3135
The discharge was measured twice: The flood that began at Gígjökull at around 11:30, reached a peak discharge of 250 m3/s two hours later at the old bridge. Both 28 and 29 April, mean discharge from Gígjökull was 130-150 m3/s, which was higher than the days before.
Additionally, the electrical conductivity of Krossá and Steinholtsá rivers remained high.
For more photos of the hydrological
/about-imo/news/nr/1898
discharge of water from Grímsvötn. Discharge continues to
increase in the Gígjukvísl river. Additionally, high levels of electrical
conductivity in the river indicate the presence of geothermal meltwater.
Presently, there are no detectable signs of the beginning of a volcanic
eruption at Grimsvötn.
/media/vatnafar/flod/Grimsvotn_status_2010-11-02_IES_IMO.pdf
A meteogram is a graphical display of a local-scale forecast, based on data from a nearby weather station.
Graphs for different regions are available from the top of the meteogram page; additionally, meteograms for specific stations can be viewed. The graphs are displayed in the region beneath the selection area; the entire width of the page is used to fit two meteograms
/weather/articles/nr/1217