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as river discharge and
water levels. Notices on avalanches and sea-ice
are shown; short articles and news are presented.
Furthermore, web and data portals can be accessed
through the web, which is available in both Icelandic
and English. IMO uses the social networking website
Facebook for communication and feed-back. A new
web-application (App) provides access to forecasts
and warnings
/media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
....................................................................................... 10
3 September 2012 .................................................................................. 12
3 Radiation fluxes at the surface ....................................................................... 16
4 Heat fluxes at the surface .............................................................................. 21
5 Net energy
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
of Eyjafjallajo¨kul), Hveravellir (Hv; 641 m a.s.l., ca. 100 km north of Tindfjallajo¨kull
and Torfajo¨kull) and Ho´lar (Ho) in Hornafjo¨rdur (18 m a.s.l.). The plot shows the elevation distribution of the Eyjafjallajo¨kull, Tindfjallajo¨kull and
Torfajo¨kull ice caps as area (km2) per 10 m elevation interval.
Mass balance of three ice caps in southern Iceland S. Gudmundsson et al.
2
(page number
/media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
use is defined as grain and corn (56%), grass (29%),
forest (7%), heather (5%), and urban (2%) on the basis of
satellite data. Most of the forest consists of conifer trees.
Since 1990 the agricultural area covered by corn has
increased from less than 1% to approximately 10% at the
expense of root crops (primarily beets) and rape [Statistics
Denmark]. However, in this study grain and corn
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
of the model with
past observations, it is used to simulate the future response of
the glacier during the 21st century. The mass balance model
was forced with an ensemble of temperature and precipita-
tion scenarios derived from 10 global and 3 regional climate
model simulations using the A1B emission scenario. If the
average climate of 2000–2009 is maintained into the future,
the volume
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
recorded at 5-13 km depth, but fewer than
yesterday.
GPS deformation: Measurements from around Eyjafjallajökull indicate no major net
discplaceaments, suggesting a stabilization of the surface deformation
since yesterday.
Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64
km distance from the eruption site shows that about 5 % of the ash is
smaller
/media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf
22N) from till
Illulisat DMI 50 10 105 497382 7681278 Ta 1.1.81 6.4.06
Station 437 ASIAQ 275 340 311 531316 7709513 Ta 5.9.83 1.6.06
Swiss Camp GC-net 1150 1115 780 566396 7719204 Ta, Sin 1.1.95 8.5.06
Crawford GC-net 2022 1795 1982 654464 7757807 Ta, Sin 24.5.95 2.5.06
2
2.3 RCM Data
Output from two RCMs is used: (1) the regional coupled ocean-atmosphere model RCAO
(Döscher et al., 2002) and (2
/media/ces/ces_geus_paakitsoq_full_report.pdf