judgment and statistical analysis of a body of evidence (e.g. observations
or model results), then the following likelihood ranges are used to express the assessed probability of occurrence: virtually certain >99%;
extremely likely >95%; very likely >90%; likely >66%; more likely than not > 50%; about as likely as not 33% to 66%; unlikely <33%; very
unlikely <10%; extremely unlikely <5
/media/loftslag/IPPC-2007-ar4_syr.pdf
of the
excess warming in Iceland reflects the influence of the Arctic Amplification.
The issue under consideration here is how much of the recent warming in Iceland
is part of the anthropogenic warming and how much is a manifestation of
naturally occurring climate variability.
An examination of climate model output from the CMIP5 project for a
region surrounding Iceland (a latitude
/climatology/iceland/climate-report
of the
excess warming in Iceland reflects the influence of the Arctic Amplification.
The issue under consideration here is how much of the recent warming in Iceland
is part of the anthropogenic warming and how much is a manifestation of
naturally occurring climate variability.
An examination of climate model output from the CMIP5 project for a
region surrounding Iceland (a latitude
/climatology/iceland/climate-report/
Improving groundwater representation and
the parameterization of glacial melting and
evapotranspiration in applications of the
WaSiM hydrological model within Iceland
Bergur Einarsson
Sveinbjörn Jónsson
VÍ 2010-017
Report
Improving groundwater representation and
the parameterization of glacial melting and
evapotranspiration in applications of the
WaSiM hydrological model within
/media/ces/2010_017.pdf
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/media/loftslag/Hare-2011-ParticipatoryModelling.pdf
in flooding were evaluated at 67 sites in Finland with var-
iable sizes of runoff areas using a conceptual hydrological model and 20 climate scenarios from both glo-
bal and regional climate models with the delta change approach. Floods with a 100-year return period
were estimated with frequency analysis using the Gumbel distribution. At four study sites depicting dif-
ferent watershed types
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
computing. As a part of this development, IMO and the Danish
Meteorological Institute, DMI, have signed a co-operation agree-
ment on research and the operation of the next supercomputer of
DMI in IMO´s premises. The partners are going to work together on
climate studies, Arctic studies, development and operation of the
Harmonie model and other topics of mutual interest. The benefit to
IMO
/media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
Impact of snow and cloud cover on the
surface energy budget over Iceland
based on HARMONIE model simulations
Nikolai Nawri
VÍ 2015-006
Report
Impact of snow and cloud cover on the
surface energy budget over Iceland
based on HARMONIE model simulations
VÍ 2015-006
ISSN 1670-8261
Report
+354 522 60 00
vedur@vedur.is
Veðurstofa Íslands
Bústaðavegur 7–9
108 Reykjavík
Nikolai Nawri, Icelandic Met
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
wanted to drop you guys a line and
say thank you. I was in Iceland for 16 days in September surfing, and
your web site was so crucial to the trip on knowing when to move and
where to go. Keep up the great work. Thanks again.Preparing a visit to Iceland
Elizabeth wrote in August 2015: "I just wanted to thank you so much for your wonderful website, which is truly one of the most comprehensive
/about-imo/the-web/awards_and_press/