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• 31. The weather in Iceland in 2018

  was below normal in May and June, slightly above normal in July and August, and again below normal in September and October. It was exceptionally warm in Reykjavík in November and December. In Akureyri, the temperature was above normal in all months except August. Precipitation The year was relatively wet and the precipitation was above the 1971 to 2000 mean at most stations. The number of days /about-imo/news/the-weather-in-iceland-in-2018

• 32. The weather in Iceland in 2020

  over five-day period in Iceland. Several landslides hit the town of Seyðisfjörður during these days, the largest on 18 December. It ranks as the most damaging landslide to have affected an urban area in Iceland.Table 2: Precipitation overview 2020 from several stations. (1) Total precipitation (mm). (2) Percentage of the 1971 to 2000 average precipitation. (3) Percentage of the 10-year /about-imo/news/the-weather-in-iceland-in-2020

• 33. The

  and the minimum was -17.9 on 29 December. PrecipitationThe precipitation was above the 1971 to 2000 mean at most stations. The excess was largest in the East. Heavy rainfall in the East and Southeast at the end of September resulted in extensive flooding from major rivers in the area. The annual total in Reykjavík was 900.4 mm, 10 percent above the 1971 to 2000 mean. In Akureyri /about-imo/news/the-weather-in-iceland-in-2017

• 34. Future Climate and Renewable Energy - Impacts, Risks and Adaptation 31 May - 2 June Presentations

  : model evaluation and future projections Hanna Tietäväinen Summertime precipitation in Finland under recent and projected climate Sara C. Pryor Intense and extreme wind speeds over the Nordic countries Hydrological projections, runoff Keynote Dennis Lettenmaier Runoff projections and impacts on water resources Liga Kurpniece Climate change impacts on the hydrological regime in Latvia Deborah /ces/publications/nr/2016

• 35. VI_2017_009

  The temporal resolution of the selected data varies from daily to annual. Simulations for the 20th century are available, extending to 2005 when the RCP (Representative Concentration Pathways) simulations start. Furthermore, reanalysis products are available between 1981 and 2000. The reference period for this study is therefore chosen to be from 1981 to 2000. We use CORDEX simulations from /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 36. 2010_003rs

  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

• 37. Twenty years of multinational earthquake prediction research in Iceland, and the future

  for an alert system. The alert system has been in operation for almost two decades and is in further development. The SIL system also provides a basis for all the later prediction research projects. The PRENLAB and PRENLAB-2 projects of several European countries, 1996-2000 (EC supported projects) were a direct continuation of the SIL project, but with a more multidisciplinary approach. PRENLAB /earthquakes-and-volcanism/conferences/jsr-2009/earthquake-prediction/

• 38. Earthquakes

  most active volcanoes. Earthquake activity in the vicinity of Hekla is usually quite low, but seems to increase abruptly before an eruption. Before the eruption in Hekla in 2000, increased earthquake activity was measured in the area and a seismic swarm occurred just about an hour before the eruption. In addition to the earthquake activity, there were some significant changes in nearby strain /volcanoes/volcanic-hazards/earthquakes/

• 39. Dyrrdal_Anita_CES_2010

  • Analyse future snow scenarios Introduction Data & Methods Results 0 50 100 150 200 250 300 350 400 450 0-100 100- 200 200- 300 300- 400 400- 500 500- 600 600- 700 700- 800 800- 900 900- 1000 1000- 1100 1100- 1200 1200- 1300 1300- 1400 1400- 1500 1500- 1600 1600- 1700 1700- 1800 1800- 1900 1900- 2000 2000- 2100 2100- 2200 Høyde (m o.h.) A n t a l l v æ r s t a s j o n e r Elevation of met.no /media/ces/Dyrrdal_Anita_CES_2010.pdf

• 40. Linnet_Ulfar_CES_2010

  °C/100y 1975-2000 • 2.35 °C/100y 2000- •Change in precipitation • Average increase 4.8% / 100 y • Range 3.3 – 7.2 % •Glaciers • Results from CES • 25% decrease in volume from 2000 to 2050 Temperature transformation Com parison of series 10000 12000 14000 16000 18000 20000 22000 1 9 5 0 1 9 5 2 1 9 5 4 1 9 5 6 1 9 5 8 1 9 6 0 1 9 6 2 1 9 6 4 1 9 6 6 1 9 6 8 1 9 7 0 1 9 7 2 1 9 7 4 1 9 7 6 1 9 7 8 1 /media/ces/Linnet_Ulfar_CES_2010.pdf