of the glaciers at their maximum at the end of the Little Ice Age (about 1890) and also at the end of the 20th century. On the map surge-type glaciers are distinguished from non-surge-type glaciers with a darker green color. A symbol shows volcanic calderas which are located underneath the glaciers. Also shown are place-names of all of the glaciers that have been given names.
An explanatory
/about-imo/news/nr/2712
........................................ 34
Bergström, S. and Andréasson, J.
Swedish Guidelines for Design Floods for Dams in a Changing Climate ............................................................ 36
3
HYDROLOGICAL PROJECTIONS, GLACIERS AND ICE-SHEETS
Jóhannesson, T., Aðalgeirsdóttir, G., Ahlstrøm, A., Andreassen, L.M., Beldring, S., Björnsson, H., Crochet, P.,
Einarsson, B
/media/ces/ces-oslo2010_proceedings.pdf
and the groundwater module. The coupling
between both modules was done by a net boundary flux between the unsaturated zone and
the groundwater (Schulla & Jasper, 2007).
Information on land use, soil type, elevation and other general properties of the watershed
are given in static distributed grids while a number of parameters describing specific
processes are adjusted to the properties of each
/media/ces/2010_016.pdf
to “bookshelf” type
faulting. In June 2000, two large earthquakes of magnitudes ML6.4 and ML6.5 struck in the
SISZ, three and a half days and approximately 17 km apart. Seismicity greatly increased in
all Southwest Iceland and during 2000, roughly nineteen thousand microearthquakes were
recorded there. The aim of this research is to relocate the earthquakes using a double-
difference relative
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
-type mechanisms all
contained significant volumetric components. Dahm and Brandsdóttir (1997) interpreted
the distribution of event locations and mechanisms with a vertical dyke intrusion beneath
the northern flank of the volcano. Over the same period, between 3 August 1993 and 6
June 2005, more than 15 cm of deformation was observed in InSAR data, but was centred
just south of the glacier
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf
is taken into account, and
consequently the estimated incremental impacts tend to be near the upper bound. If over the
course of time (i.e. as climate change proceeds) road users and road administrations get convinced
that the frequency of some adverse events has increased, adaptation will start to occur, e.g. by
using another type of asphalt, favoring cars with more intelligent braking
/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
center. The pass-band is within 0.075 to 3 Hz and is
applied to both velocity and acceleration records, whereas in ElarmS the acceleration record is
only low-pass filtered (Allen and Kanamori, 2003; Shieh et al., 2008). The process was
implemented on 9 stations of the SIL seismic network at month 36 (see Figure 1). The SIL
network consists mostly of combinations of short-period sensors
/media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf
commercial use.
Data means any type of forecast, measurement, observation, calculated result or derived data (i.e. from model calculations). Many pages on the IMO web-site contain real-time data that has not been assessed; note that these data are preliminary and that they might change after revision. The Icelandic Meteorological Office does not guarantee that data on its web-site will always
/about-imo/the-web/conditions
commercial use.
Data means any type of forecast, measurement, observation, calculated result or derived data (i.e. from model calculations). Many pages on the IMO web-site contain real-time data that has not been assessed; note that these data are preliminary and that they might change after revision. The Icelandic Meteorological Office does not guarantee that data on its web-site will always
/about-imo/the-web/conditions/
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To show other areas, a different digit must be entered after 'Vi.ifrm.area'. The area codes are as follows:
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/about-imo/the-web/iframes/wind-temp-precip/