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• 41. Flood from Skaftá

  /about-imo/news/flood-in-estern-skafta

• 42. Flood from Skaftá

  /about-imo/news/flood-in-estern-skafta/

• 43. Latest news on the eruption at Reykjanes peninsula

  /about-imo/news/a-new-eruption-has-started-at-fagradalsfjall

• 44. raisanen_ruosteenoja_CES_D2.2

  1 Probabilistic forecasts of temperature and precipitation change based on global climate model simulations (CES deliverable 2.2) Jouni Räisänen1 Kimmo Ruosteenoja2 19 December 2008 1 Department of Physics, P.O. Box 64, FI-00014 University of Helsinki, Finland Email: jouni.raisanen@helsinki.fi 2 Finnish Meteorological Institute, P.O. Box 503, FI-00101 Helsinki, Finland Email /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf

• 45. Observations - Steinar

  Observations - Steinar | Observations | Icelandic Meteorological office Observations - Steinar Mon 1.05 13 GMT 6.6° E 4 Max wind : 5 / 10Road temp. : 16.1° 12 GMT 5.8° E 3 Max wind : 5 / 8Road temp. : 14.7° 11 GMT 6.0° ESE 3 Max wind : 3 / 5Road temp. : 13.0° 10 GMT 5.5° ENE 2 Max wind : 2 /m/observations/areas

• 46. GA_2009_91A_4_Andreassen

  to highly negative summer balances, but also lower bw than the average for 1949–2006. Calculated change in specific mass balance for a ±1°C change in air tem- perature was ±0.55 m w.e., whereas a ±10 % in- crease in precipitation represented a change of ± 0.20 m w.e. Model results further indicated that for a 2°C warming, the ablation season will be extend- ed by c. 30 days and that the period /media/ces/GA_2009_91A_4_Andreassen.pdf

• 47. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  AVAILABLE FROM: http://www.atm.helsinki.fi/~jaraisan/CES_D2.3/CES_D2.3.html 2 Table of Contents Abstract 1 1. Introduction 2 2. Model simulations 4 3. Methods used for deriving probabilistic climate change forecasts 7 3.1 Resampling and variance correction 9 3.2 Relationship between local and large-scale climate changes in ENSEMBLES simulations 10 3.3 Comparison of large-scale /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 48. vanRoosmalen_etal-2009-WRR_2007WR006760

  Impact of climate and land use change on the hydrology of a large-scale agricultural catchment Lieke van Roosmalen,1 Torben O. Sonnenborg,2 and Karsten H. Jensen1 Received 5 December 2007; revised 21 November 2008; accepted 19 January 2009; published 18 March 2009. [1] This paper presents a quantitative comparison of plausible climate and land use change impacts on the hydrology of a large-scale /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 49. Forecasts - Sáta

  Forecasts - Sáta | Station forecasts | Icelandic Meteorological office Forecasts - Sáta Mon 1.05 14 GMT -2° ESE 6 Cloud cover: 100% 15 GMT -2° ESE 6 Cloud cover: 70% 16 GMT -2° ESE 6 Cloud cover: 20% 17 GMT -2° ESE 7 Cloud cover: 100% 18 GMT -2° SE 6 Cloud cover: 100% 19 GMT -2 /m/forecasts/areas

• 50. Journal_of_Hydrology_Veijalainen_etal

  to increase in Finland by 13–26% by the 2080s (Ruosteenoja and Jylhä, 2007) and extreme precipitations are expected to in- crease (Beniston et al., 2007). On the other hand, temperature in- creases of 2–6 C by the end of the century are estimated to decrease the snow accumulation by 40–70% by the same period (Vehviläinen and Huttunen, 1997; Beldring et al., 2006; Ruosteeno- ja and Jylhä, 2007 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf