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Results:

• 31. “The small eruption” in

  and deformation may precede many eruptions this is not always the case and depends on how much stress has already been released and the strength of the upper crust”, says Michelle.Figure 2. A) GPS data from the station KRI in Krísuvík. The blue line indicates the beginning of the eartquake swarm (24.02) and the red line shows the beginning of the eruption (19.03). A rapid deformation was detected /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months/

• 32. Past temperature conditions in Iceland

  Figure 5. Spring temperature (April and May) in Stykkishólmur. The red line corresponds to a linear trend of about 0.7°C per century. The temperature variations in the spring (April and May) are similar in timing to the winter. The 1840s had the warmest spring temperatures in the 19th century corresponding to a minimum extent of sea ice at that time. This was followed by a very /climatology/articles/nr/1213

• 33. Past temperature conditions in Iceland

  Figure 5. Spring temperature (April and May) in Stykkishólmur. The red line corresponds to a linear trend of about 0.7°C per century. The temperature variations in the spring (April and May) are similar in timing to the winter. The 1840s had the warmest spring temperatures in the 19th century corresponding to a minimum extent of sea ice at that time. This was followed by a very /climatology/articles/nr/1213/

• 34. Jökulhlaup from Grímsvötn subsides

  that previously flowed into the Skeiðará river breached this sediment bank in 2009, leading to the start of meltwater flow along the margin and into Gígjukvísl. Photo: Þorsteinn Þorsteinsson. Figure 5 shows the location where the greatest amount of upwelling of water was observed and Figure 6 shows a scientist measuring the water temperature at this site. Earlier data from the subglacial lake /about-imo/news/2010/nr/2042

• 35. Jökulhlaup from Grímsvötn subsides

  that previously flowed into the Skeiðará river breached this sediment bank in 2009, leading to the start of meltwater flow along the margin and into Gígjukvísl. Photo: Þorsteinn Þorsteinsson. Figure 5 shows the location where the greatest amount of upwelling of water was observed and Figure 6 shows a scientist measuring the water temperature at this site. Earlier data from the subglacial lake /about-imo/news/nr/2042

• 36. VI_2020_011_en

  Veðurstofa Íslands 2 Almannavarnadeild Ríkislögreglustjóra 3 Jarðvísindastofnun Háskólans 4 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Bologna 5 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Pisa 6 Jarðvísindadeild Háskóla Íslands 7 Agricultural University of Iceland 8 Consultant Skýrsla nr. Dags. ISSN Opin Lokuð VÍ 2020-011 Desember 2020 1670-8261 Skilmálar: Heiti skýrslu /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 37. Keranen_Jaana_CES_2010

  / opportunity identification 4. Risk / opportunity estimation (consequences, probabilities) 1. Scope definition Targets 5. Risk / opportunity evaluation Adaptation, mitigation Risk management Risk analysis Action plan Risk assessment 2. Data collection 2 .2 - … very likely2 .1 – L isääntyvä sadan ta vuositasolla 0-8 % 2. Lisääntyvä sadanta 1 .2 - … 3very likely T urbii nien kapasioteett ia vo idaan /media/ces/Keranen_Jaana_CES_2010.pdf

• 38. Latest news on the eruption at Reykjanes peninsula

  the area and to follow instructions and advice as given by the local Police and Civil Protection authorities.Updated 8.8. at 13:00Gas pollution at the eruption site can at any time exceed danger levels. The eruptive plume follows the wind direction, and it is therefore safer to watch the eruption with the wind direction behind you, rather than towards you.In calm/light wind (<5 m/s) gas can /about-imo/news/a-new-eruption-has-started-at-fagradalsfjall

• 39. Joining forces in weather forecasting and climate research

  Snorrason, Director General of the IMO. The new supercomputer can perform 4,000 trillion calculations per second, which is more than half a million calculations per second for every person on the planet. It will handle state of the art weather models with more than 6 million lines of code –the Mars Curiosity Rover was built on 5 million- which will produce high resolution weather predictions /about-imo/news/joining-forces-in-weather-forecasting-and-climate-research

• 40. Paper-Olafur-Rognvaldsson_91

  of precipitation have been made in recent years. Chiao et al. (2004) used the MM5 model at a 5 km horizontal resolution to simulate a heavy precipitation event during MAP IOP– 2B. The precipitation was satisfactorily reproduced by the model although the total amount of precipitation was slightly higher than measured by rain-gauges. Buzzi et al. (1998) simulated a 1994 flooding event in northwestern Italy /media/ces/Paper-Olafur-Rognvaldsson_91.pdf