to theoretical framework. I do also want to thank him for an
enjoyable time during this work, both in the office and in the field.
This work was carried out as a part of the Skaftá cauldrons research project which
was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja-
sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com-
pany), the National Energy
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
....................................... 16
CLIMATE PROJECTIONS
Kjellström, E., Drews, M., Christensen, J.H., Haugen, J.E., Haakenstad, H. and Shkolnik, I.
An ensemble of regional climate change scenarios for the Nordic countries........................................................ 18
Benestad, R.E.
An analysis of simulated and observed storm characteristics
/media/ces/ces-oslo2010_proceedings.pdf
level in Skeidará waned. The last sign of a
crater explosion was seen at GRF early on 6
November, leaving only a weak tremor signal
from the remnants of the jökulhlaup. The
jökulhlaup fi nally ended in early December,
after ~0.8 km3 of water had drained from the
Grímsvötn lake (J. Hardardóttir, personal com-
munication, 2005).
Location and Volume Constraints
Earthquake locations at Grímsvötn
/media/jar/myndsafn/2005EO260001.pdf
in sessions organised in conjunction with Arctic Circle by the
World Council of Churches and the Church of Iceland on "Just Peace with
the Earth", Thursday, and "Climate Justice" on Saturday. In both
events he gave a presentation and took part in round table discussions. Bartholomew I patriarch of the Orthodox church also
participated in the latter event.Sigrún Karlsdóttir, director of Natural Hazards
/about-imo/news/imo-at-the-arctic-circle-assembly-2017
movement. The operation of the seismographs was ceased in 1914 due to funding restrictions during World War I.
The operation of the seismographs was recommenced in 1925 and 1927 at the Icelandic Meteorological Office (IMO), where data processing was also conducted. Amplification of ground motion was low and even several felt earthquakes were not recorded. In 1951-1952, three Sprengnether short-period
/earthquakes-and-volcanism/conferences/jsr-2009/100_years/
(i. e. the location of the measuring point at each river) is also available as pdf (7.2 Mb). See Jökulsá á Fjöllum in the northeast, Markarfljót in the south and Haffjarðará in the west. The volcanic eruptions in March, April and May 2010 are shown in red.
Related topics
/hydrology/articles/nr/2110
The majority of the grid cells show
no significant change, however a
rising trend towards the end of the
century is noted (red curve).
2071 -2100 relative to 1961-90 [%]
Rossby Centre
i l d l Declines No change Increases
Changes in % for grid cells
with significant changes
Activities and results
reg ona mo e
and ECHAM4
Rossby Centre
regional model
and HadAM3
ECHAM4: A2 0.1 73.2 26.7
ECHAM4: B2 0.1
/media/ces/ces_wind_flyer-hq.pdf