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A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö
A
A: Icelandic abbreviation of East (compass direction, easterly, eastern).
ANA: Icelandic abbreviation of Eastnorthesast (compass direction).
ASA: Icelandic
/weather/articles/nr/1208/
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
fatalities occurred in
mobile homes,
although only 7.6% of
U.S. housing units in
2000.
• A one standard
deviation in the
proportion of mobile
homes in housing stock
(8.3 percentage
points) increases
fatalities by 36% and
injuries by 18%.
The Mobile Home Problem
50
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/media/loftslag/Tornado_Impacts_-_FMI_Presentation.pdf
glacier, and a general land rise
along the southern coast and in the countries interior (figure 1). This rise results from recent melt
of the Icelandic glaciers, which have been melting since the late 19th century. An acceleration in
land uplift is even evident in the Southeast. STL analysis of vertical GPS measurements in 1997-
2015 from Höfn in Hornafjörður show over 8 mm/yr uplift in the first
/media/vedurstofan-utgafa-2020/VI_2020_005.pdf
Dashed lines encompass the V-shaped zone of tephra deposition. (c)
Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall
from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November.
The top portion shows its projection on an EW-vertical plane. The minimum detection height for
Grímsvötn is seen at 6 km, and the plume extends
/media/jar/myndsafn/2005EO260001.pdf
by season (%) between
1991-2007 and 1961-1990 in the Baltic countries
1
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/media/ces/ces_SA_group_flyer_new.pdf
Neotectonics in Nordland; NEONOR 2
C. Lindholm, O. Olesen, I. Janutyte, S. Gradman, M. Keiding, H. Kierulf,
M. Ask, J. Dehls, Y. Maystrenko, F. Riis, L. Rise and other project partners
The Nordland shore region is known to be seismically active with deep local sediment basins on the
continental shelf that stretches some 200 km west of the coastline. The offshore areas west of Nordland
have
/media/norsem/norsem_lindholm.pdf
h
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in
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/media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
A. (2010b). 21st century changes in the European climate: uncertainties derived from an ensemble of regional climate model simulations. Tellus, published online. DOI: 10.1111/j.1600-0870.2010.00475.
Ólafsson H, & Rögnvaldsson Ó. (2010). Regional and Seasonal Variability in Precipitation Scenarios For Iceland. Hydrology Research, in revision.
Peltonen-Sainio, P., Hakala, K., Jauhiainen, L/ces/publications/nr/1680