station Region type Catchment area,
Q station (km2)
Lake percentage
(%)
Settlement for
inundation analysis
Boundary conditions
of the 2D model
a Köngäs Ounasjoki Small/medium,
northern river
4488 4.2 Kittilä Upstream : Q; Downstream : river WSE
b Sonkajärvi Small, lake 946 4.4 – –
c Keppo Lapuanjoki Small/medium,
coastal river
3949 3.0 Lapua Upstream : Q; Downstream river WSE
d Harjavalta
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
Av. Ed.
Belin, 31400 Toulouse, France
Received: 21 March 2011 – Published in The Cryosphere Discuss.: 6 April 2011
Revised: 5 October 2011 – Accepted: 20 October 2011 – Published: 2 November 2011
Abstract. The Little Ice Age maximum extent of glaciers in
Iceland was reached about 1890 AD and most glaciers in the
country have retreated during the 20th century. A model for
the surface mass balance
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
in Iceland: Climate projections and historical changes in precipitation type Andréa-Giorgio R. Massad, Guðrún Nína Petersen, Halldór Björnsson, Matthew J. Roberts & Tinna Þórarinsdóttir99
20,6
/about-imo/publications/2022/
.............................................................................................. 45
5.3 Present weather ..................................................................................... 45
Appendix ......................................................................................................... 47
5
List of Figures
1 How PWD22 determines the type of precipitation. ........................................ 11
2 Number of records as a function of the height
/media/vedurstofan-utgafa-2019/VI_2019_009.pdf
................................................................................................21
5.3.2 Data processing ............................................................................................21
5.3.3 Common binaries .........................................................................................23
5.4 Data storage
/media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf
will be updated when new information arrives.See also IMO's Twitter feed for important updates. Updated 23.8. 2022The eruption in Meradalir, which commenced on the
3rd of August, ceased to issue lava on the 21 of August. Volcanic tremor
started to decrease steadily from the 18th and stopped completely during the
night of 21st. The activity at the crater ceased at the same time, with no visible
/about-imo/news/a-new-eruption-has-started-at-fagradalsfjall
Seismic activity has been rather intensive over the last 24 hours. The biggest was M5,3 at 14:21 yesterday and
another one was measured M4,7 at 06:44 this morning. In total 10 earthquakes larger then M3,0 were detected in
Bardarbunga since our last meeting. Smaller earthquakes were detected in Dyngjujokull glacier and in north part of
the dyke.
GPS monitoring continue to show
/media/jar/Factsheet_Bardarbunga_20140919.pdf
is to
properly handle furniture and other interior objects so that they do not fall
off in the event of an earthquake. The effects of an earthquake on the
Reykjanes Peninsula, can be felt in a large area, and the capital area is not
excluded.The Scientific Advisory Board, therefore, encourages
people to check with their home and workplaces and fix unstable hanging
objects. Information on earthquake
/about-imo/news/seismic-activity-around-mt-thorbjorn-has-decreasing-significantly
of the Aurora Borealis on a clear night sky draws an increasing number of tourists.
During summertime tourists should bring a windbreaker, rainwear, a thick pullover (wool or fleece) and sturdy walking shoes. Travellers who are camping or heading into the interior will need warm underwear and socks, rubber boots and a warm sleeping bag.
During wintertime tourist should bring warm clothing, warm
/climatology/iceland/nr/1268
made 27 Dec. The colour code reveals windspeeds above 24 m/s upto 32 m/s forecasted. Please check the front page of the web for updated information, http://en.vedur.is/weather/forecasts/elements/#type=wind
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/about-imo/news/bigimg/2606