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Results:

• 31. 2016-10-18_Ovedur_en

  100 mm over 24 hours. Rising stream and river levels are likely on the Snæfellsnes peninsula, around the Eyjafjallajökull and Mýrdalsjökull ice-caps, and south of the Vatnajökull ice cap. Travellers are cautioned against fording rivers in these regions. On behalf of IMO Elín Björk Jónasdóttir, coordinator of public weather services. Hrafn Guðmundsson, forecaster on duty Þorsteinn V. Jónsson /media/frettir/vedur/2016-10-18_Ovedur_en.pdf

• 32. Instructions on using Atlantic Ocean forecasts

  of the wind direction. Wind-speed is symbolised by diagonal lines at the end of the barb; a long line represents 5 m/s, a short line 2.5 m/s and a triangle represents 25 m/s. Temperature forecast: Temperature levels are shown over the Atlantic Ocean in degrees Celsius (°C) at an altitude of about 1,500 m above the ocean surface. This altitude equates to an air pressure of 850 hPa /weather/articles/nr/1218

• 33. ces_cg_flyer

  and regional models all under the IPCCA1B emission scenario (right) have been accomplished, see http://ensemblesrt3.dmi.dk Relative changes comparing 2021-2050 to 1961-1990 in three of the CES RCMs are shown for annual mean precipitation (above) and 10m-wind speed (below). Units: %. Partners The work in the Climate modelling and scenarios group is carried out by a network of scientists from the national /media/ces/ces_cg_flyer.pdf

• 34. CES_D2.4_task2_CMIP3_winds

  in the average wind speed between the baseline (or control) period 1971-2000 and the scenario period 2046-2065. These periods were chosen based on the availability of model output at daily time resolution. We have analyzed the surface geostrophic wind (hereafter Vg) rather than the actual simulated surface winds, because the latter are sensitive to the details of the boundary layer /media/ces/CES_D2.4_task2_CMIP3_winds.pdf

• 35. The weather in Iceland 2011

  December. April and November were unusually warm. At a few stations in the east and northern coastal areas April was warmer than June. This has not happened before in Iceland at any station since the beginning of instrumental recording. Temperature The average temperature of 2011 in Reykjavík was 5.4 °C, 1.1 °C above the 1961 to 1990 mean. This is the 16th consecutive year of above normal /weather/articles/nr/2439

• 36. ved-eng-2011

  in Iceland. The minimum temperature was -27.8 degrees at Upptyppingar in the northeastern inland on 8 December, close to the average annual absolute minimum in Iceland. Precipitation The precipitation was above normal. In Reykjavík it exceeded the 1961 to 1990 mean by about 13%. April was the wettest with more than the double normal amount. June and August were the driest. At Akureyri /media/vedurstofan/utgafa/skylduskil/ved-eng-2011.pdf

• 37. Pyroclastic flow

  of the volcano.Because eruption column density is lower than the atmosphere, the column in most cases ascends many kilometres above the volcano. Finally, it spreads out and forms a cloud and the ash coming from the column is dispersed with the wind. However, when the eruption column can't intake enough air it cools down and becomes denser than the surrounding air. When this happens the column collapses /volcanoes/volcanic-hazards/pyroclastic-flow/

• 38. Kjellstrom_Erik_CES_2010

  ANN−10 −5 0 5 10 15 20 delta w (% ) 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17C h a n g e i n g e o s t r o p h i c w i n d s p e e d ( % ) Change in wind over the Baltic Sea in 70 years time at the time of CO2-doubling Chen and Aschberger, 2006 17 CM IP G CM s A need for regional ensemble simulations head2right Changes are uncertain head2right Size and sometimes even sign /media/ces/Kjellstrom_Erik_CES_2010.pdf

• 39. The

  in Akureyri in April and June. August was sunny but sunshine duration was close to normal during the other months of the year. Sea level pressure The annual average in Reykjavík was 1005.2 hPa, 0.7 below the 1961 to 1990 mean. The absolute highest pressure of the year was measured at Reykjavík airport on 1 January, 1041.0 hPa, but the lowest at Gufuskálar in the West on 24 February, 951.7 hPa /about-imo/news/the-weather-in-iceland-in-2017

• 40. Landslides

  is usually easily eroded. If the mass is big enough, the momentum and speed can become sufficiently large to snatch up bridges, buildings or other infrastructure and therefore cause large amount of damages. One of the most infamous hazard caused by lahars occurred after the eruption in Pinatubo in 1991. https://pubs.usgs.gov/fs/1997/fs114-97/ Another example is the devastating lahar /volcanoes/volcanic-hazards/landslides/