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• 11. VI_2022_006_extreme

  at catchment-scale, with and without projections, the results will give insights into hydrological trends, helping in the future design of critical infrastructure. This research was funded in 2021 by Landsvirkjun, under the Orkurannsóknasjóður grant. 5 Figure 1 – 1M5 map based on 24-hour accumulated precipitation, obtained from the entire ICRA dataset using the Peak-over-Threshold method /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 12. 2010_017

  is corrected. 24 Table 5. Recession constants for the surface runoff (kD) and interflow (kI) estimated by two different methods and results without and with groundwater module. Nash-Sutcliffe coefficients (R2) are also presented along with mean percentage error (MPE) and root mean square error (RMSE) for both daily and annual discharge values. Data are from the period 1990–2005. kD (opti- mized /media/ces/2010_017.pdf

• 13. Savolainen_Ilkka_CES_2010

  reduction scenarios for limiting the emission by 50% and by 85% corresponding the overlimit emissions and underlimit emission for a temperature rise level of 2 C. 903/02/2010 WEO 2009 1003/02/2010 IPCC Special Report on Renewable Energy Sources and Climate Change Mitigation (SRREN) 1) Introduction (Renewable energy and climate change) (5% share of the whole report) 2) Bioenergy (15 %) 3) Direct /media/ces/Savolainen_Ilkka_CES_2010.pdf

• 14. Johannesson_Thomas_CES_2010

  Nigardsbrevatn annual discharge 0 5 10 15 1951 1971 1991 2011 2031 2051 2071 2091 m 3 / s year DMI ECHAM A1b with gls DMI ECHAM A1b without gls met.no HADLEY A1b with gls met.no HADLEY A1b without gls SMHI BCM A1b with gls SMHI BCM A1b without gls Discharge seasonality, HBV/GLS models 25 30 35 40 Nigardsbrevatn daily mean discharge 0 5 10 15 20 1. jan. 20. feb. 11. apr. 31. mai. 20. jul. 8. sep. 28. okt. 17 /media/ces/Johannesson_Thomas_CES_2010.pdf

• 15. Avalanche notices on the web - an improved map

  come from regions where avalanche observers work and it is imperative that the users of the web understand that more avalanches are likely to have fallen without being reported. Accordingly, people are encouraged to report avalanches that they come across. Other services The avalanche warning service of the Icelandic Meteorological Office monitors impending avalanche danger in towns and villages /about-imo/news/nr/2838

• 16. Avalanche notices on the web - an improved map

  come from regions where avalanche observers work and it is imperative that the users of the web understand that more avalanches are likely to have fallen without being reported. Accordingly, people are encouraged to report avalanches that they come across. Other services The avalanche warning service of the Icelandic Meteorological Office monitors impending avalanche danger in towns and villages /about-imo/news/nr/2838/

• 17. Bardarbunga_Daily_status_report_290814

  Heading No plume now, but winds were about 10 m/s from SE during the night. Colour No plume now. Tephra fallout No tephra fall now. Lightning No lightning during eruption according to ATDnet of the UK Met Office and WWLLN-system. Noise None. Meltwater The eruption was 5 km N of the glacier, therefore without a jökulhlaup. No indication of changes in water flow in rivers. The conductivity still /media/jar/Bardarbunga_Daily_status_report_290814.pdf

• 18. The weather in Iceland in 2022

  and Akureyri, but snow was heavy in February. February was one of the snowiest months for years in Reykjavík. Days with total snow cover in March were 5 more than average in Reykjavík but 5 less than average in Akureyri. October and November were both completely without snow cover in Reykjavík and Akureyri, but snow cover was above average in December. Bright sunshineThe number of bright /about-imo/news/the-weather-in-iceland-in-2022

• 19. A minor eruption underway

  the IMO has installed webcams which can be used to monitor the area, in case of an eruption will start without clear precursory signals. Updated 09.03. at 12.30About 5:20 this morning, the activity at Mt. Fagradalsfjall, south of the corridor, increased with a sudden increase in seismic tremor. However, the unrest soon decreased. Magma movements are a likely cause for this activity which is very /about-imo/news/earthquake-swarm-in-reykjanes-peninsula

• 20. ces-glacier-scaling-memo2009-01

  group. The file has seven columns. 1: unique id-number of the group (integer). 2: name of the group (character without spaces). 3: type (character, "ic" for ice caps, "gl" for valley glacier). 4: total ice-covered area (floating point number, m²). 5: total ice volume (floating point number, m³). 6: characteristic response time (floating point number, years). 7: coefficient giving the relative /media/ces/ces-glacier-scaling-memo2009-01.pdf