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
-Skaugen, T., Haugen, J.E., & Hanssen-Bauer, I. (2008). Dynamically downscaled climate scenarios available at the Norwegian Meteorological Institute - per December 2008, met.no report 24/2008.
Gregow, H. & Ruosteenoja, K. (2010). Estimating the effect of climate change on surface geostrophic winds in Northern Europe (CES Climate Modelling and Scenarios Deliverable D2.4). Finnish Meteorological
/ces/publications/nr/1680
....................................... 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
are tested: Method I (MI) that uses the same flow
law parameter, A, as in the two studies discussed above, im-
plicitly including basal sliding, and Method II (MII) that in-
cludes a Weertman type sliding law (Paterson, 1994) where
the sliding velocity is assumed to be proportional to a power
of the basal shear stress, τb, (Vslid =C · τmb ); C is the slid-
ing parameter and the exponent m= 3 in our
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.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