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• 41. 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

• 42. 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

• 43. 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

• 44. 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

• 45. VI_2015_009

  )=(θ0) + (θ1)(AP) Rel. RMSE= 1 NS= 0.89 MAE= 71 l l l l l l l ll ll 0 500 1500 2500 0 50 0 150 0 250 0 Pred. (m³/s) R ef . (m ³/s ) µ(D)=(θ0) + (θ1)(AP Z) Rel. RMSE= 1.2 NS= −0.095 MAE= 161 l l l l l l l ll l ll 0 400 800 1200 0 50 0 100 0 150 0 Pred. (m³/s) R ef . (m ³/s ) µ(D)=(θ0) + (θ1)(AP L) Rel. RMSE= 0.95 NS= 0.71 MAE= 138 l l l l l l l ll l ll 0 400 800 1200 0 50 0 100 0 150 0 Pred. (m³/s /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 46. 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

• 47. 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/

• 48. 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/

• 49. 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

• 50. Savolainen_Ilkka_CES_2010

  ) and other gases A wide spectrum of measures needed in order to reach deep enough emission reductions 503/02/2010 Global greenhouse gas emissions by sectors in 2005 The emissions sum up to approximately 46,000 MtCO2eq. Data source: CAIT, cait.wri.org. *) The estimated effect of land use change & forestry, 8,000 MtCO2, is for the year 2000. 603/02/2010 Raupach et al 2007; Le Quere et al. 2009 /media/ces/Savolainen_Ilkka_CES_2010.pdf