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Mean annual temperature difference
Difference relative to 1971-2000
Difference between 25% warmest and 25% coldest years
barb2right +1°C (25% warmest)
barb2right -0.7°C (25% coldest)
barb2right +1.7°C
Catchment elevation (m.a.s.l)
Catchment elevation (m.a.s.l)
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/media/ces/Crochet_Philippe_CES_2010.pdf
financial contributions from the
Icelandic Road and Coastal Administration and the National Power
Company.Published materialPagneux, E., Gudmundsson, M. T., Karlsdóttir, S., & Roberts, M. J. (Eds.) (2015). Volcanogenic floods in Iceland: An assessment of hazards and risks at Öræfajökull and on the Markarfljót outwash plain. Reykjavík: IMO, IES-UI, NCIP-DCPEM.Under the links below, each
/volcanoes/about-volcanoes/oraefajokull/new-research/
1
Probability distributions of monthly-to-annual mean temperature and
precipitation in a changing climate (CES Climate Modelling and Scenarios
Deliverable D2.4, task I)
Jouni Räisänen
Department of Physics, P.O. Box 48, FI-00014 University of Helsinki, Finland
Email: jouni.raisanen@helsinki.fi
17 November 2009
AVAILABLE FROM:
http://www.atm.helsinki.fi/~jaraisan/CES_D2.4
/media/ces/CES_D2.4_task1.pdf
over the past 130 years
A scientific
article by Icelandic glaciologists is an important contribution to global studies
and assessments of climate change. The average mass loss of the Icelandic
glaciers per unit area in recent decades is among the highest on Earth.
7.12.2020
/about-imo/news/new-article-on-glacier-changes-in-iceland-over-the-past-130-years
)
Evaluation of two delineation methods for regional flood frequency analysis in Northern Iceland (2012)
The effect of climate change on runoff from two watersheds in Iceland (2010)
Examples of peer-reviewed papers and book chapters
Tómas Jóhannesson, Helgi Björnsson, Eyjólfur Magnússon, Sverrir Guðmundsson, Finnur Pálsson, Oddur Sigurðsson, Þorsteinn Þorsteinsson & E. Berthier (2013). Ice-volume
/about-imo/arctic/completed-projects/publications/
publication of IMO to be challenges for adaptation
and risk management in Iceland as we undergo climate change.
Finally, I would like to thank the sta?of IMO for their continuous e?ort to monitor all natural hazards 24/7 year
around which is unique within the 192 member states of the World Meteorological Organization and something
which we are very proud of!
6
ÁRSSKÝRSLA 2019
Ljósmynd: Einar Guðmann
/media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf
figure per 100,000
in the decade 2020–2030 compared to the period 2005–2015;c) Reduce direct disaster economic loss in
relation to global gross domestic product (GDP) by 2030;d) Substantially reduce disaster damage to
critical infrastructure and disruption of basic services, among them health and
educational facilities, including through developing their resilience by 2030;e) Substantially
/about-imo/news/international-day-for-disaster-reduction-13th-of-october-2017-home-safe-home
in Finland
Noora Veijalainen a,*, Eliisa Lotsari b, Petteri Alho b, Bertel Vehviläinen a, Jukka Käyhkö b
a Freshwater Centre, Finnish Environment Institute, Mechelininkatu 34a, P.O. Box 140, FI-00251, Helsinki, Finland
b Department of Geography, FI-20014 University of Turku, Turku, Finland
a r t i c l ei n f o
Article history:
Received 7 January 2010
Received in revised form 13 June 2010
Accepted
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
to +0.4°C per decade in the 21st century. Vavrus et al. (2011) find +0.3 to +0.6°C
per decade and Koenigk et al. (2015) around +0.4°C. Both Nawri and Björnsson (2010) and
Koenigk et al. (2015) expect the warming to be greatest in the winter.
Model tend to disagree on precipitation changes. Differences can be found between scenarios
and models, both in terms of spatial details and seasonality
/media/vedurstofan-utgafa-2017/VI_2017_009.pdf