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• 31. Fagradalsfjall eruption unusual in many ways compared to other eruptions

  deformation and seismicity preceding the eruption that began 19 March 2021. a) Model of deformation 24 February – 19 March, showing horizontal displacements as arrows and vertical displacements with a colour scale. The red line shows the location of the dyke and the broken black line shows the central axis of the plate boundary b) Hourly earthquake rate (blue) and cumulative number of earthquakes /about-imo/news/fagradalsfjall-eruption-unusual-in-many-ways-compared-to-other-eruptions/

• 32. The weather in Iceland in 2020

  to the 10-year average. It was relatively warmer in coastal areas but colder in the inland.JuneJune was warm and favorable. It was relatively warmest in the Northeast but cooler in the southwestern part. Wind and precipitation were close to average.July July was rather cold compared to recent years, although the mean was above the 1961 to 1990 average. Yet the weather was not unfavorable /about-imo/news/the-weather-in-iceland-in-2020

• 33. New equipment at Holuhraun

  SO2, CO2, H2S and H2 which will help with forecasts of future eruptive activity. The MultiGAS instrument is part of a collaboration with the University of Palermo, thanks to the FutureVolc project. The weather station measures several local environmental parameters including wind speed and direction and humidity which helps to advise people working close to the eruption and in interpreting /about-imo/news/nr/3072

• 34. Climate of aerodromes

  BIEG and BIAR based on METAR observations 2001–2010, ANNUAL (pdf 75 Kb). Windrose, average wind speed and gusts Below are pdf-files (0.3 Mb, 17p.) for each airport. BIKF - Keflavik BIRK - Reykjavík BIAR - Akureyri BIEG - Egilsstaðir BIIS - Ísafjörður BIBD - Bíldudalur BIHU - Húsavík BIHN - Höfn BIVM - Vestmannaeyjar BITN - Þórshöfn BIGR - Grímsey BIVO - Vopnafjörður BIGJ - Gjögur Clouds /weather/aviation/climate/

• 35. 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

• 36. 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

• 37. 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

• 38. 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

• 39. Keranen_Jaana_CES_2010

  tance ◊ energy losses hot w e ather decre ase s the lifetim e of tra nsform ers increas ing w ater capa city V ery like ly, the pro bability tha t the next decad e is w arm er is 90%. Phe nom ena 1.1 - higher te m peratures, espe cially during winter Sc en ario 1. war mer clim ate Conseque nce categ ory acc ording to own ra nking Lik elihood according to own rank in g Th e op /media/ces/Keranen_Jaana_CES_2010.pdf

• 40. 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