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• 41. Articles

  Articles © Ólafur Sigurjónsson Aerial photo of Fimmvörðuháls on Eyjafjallajökull, 22nd March 2010, between 8 and 9 /earthquakes-and-volcanism/articles/bigimg/1851

• 42. The weather in Iceland 2013

  century in this area of the country. The temperature was unusually high during the first two months but for the rest of the year it was closer to the 1961 - 1990 average, relatively coldest in April when persistent snow cover caused problems in the agriculture in the Northeast. An unusually severe but short cold spell hit during the last days of April and the first days of May and resulted in new /about-imo/news/nr/2831

• 43. Status of unrest in Askja

  silent (aseismic) movement on caldera faults. Possible scenarios are still as reported before. If the magma accumulation will continue , uplift can continue for some time without an eruption. Earthquake activity is most likely the most significant indicator of an escalation in activity and an imminent eruption. The most likely scenario if there will be an eruption is a fissure eruption close /about-imo/news/status-of-unrest-in-askja

• 44. Update on the activity in the Reykjanes peninsula

  decreasing over time. The acquisition of recent satellite images enabled mapping of new surface deformation in the area associated with the sequence of large earthquakes which occurred between the 18th and 20th of July. The satellite data processing clearly shows a deformation signal corresponding to approximately 3 centimeters of movement along a NE-SW oriented fault in the region of Fagradalsfjall /about-imo/news/update-on-the-activity-in-the-reykjanes-peninsula

• 45. 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

• 46. Forecast for volcanic ashfall 2010

  the Volcanic Ash Advisory Centre in London. Nine Volcanic Ash Advisory Centres around the world are responsible for advising international aviation of the location and movement of clouds of volcanic ash. UK Met Office Zoomed Ash Concentration Charts: These charts supplement the official London VAAC graphics and advisories and are to be used with caution. Flight permission or restriction is shown as red /earthquakes-and-volcanism/articles/nr/1885

• 47. CES_D2.4_solar_CMIP3

  the A1B scenario. In the panels for winter and autumn, contour interval is 25 MJ m−2, in those for spring and summer 50 MJ m−2. The colour scale is the same in all panels. Fig. A5. The absolute insolation change under the A2 scenario. 11 Fig. A6. The absolute insolation change under the B1 scenario. 12 (B) TIME SERIES Fig. A7 shows the time series of seasonal changes in incident radiation /media/ces/CES_D2.4_solar_CMIP3.pdf

• 48. Factsheet_Bardarbunga_20150130

  ), to the east (middle) and vertical (bottom) in mm. Background signals have been removed from the time series. From May 2014 a displacement to North-West is detectable, which may be connected to the tension in Bardarbunga. Displacement towards the Bardarbunga caldera can be detected on the 16th of August (blue line), when the seismic activity started. A disturbance in the signal is detected /media/jar/Factsheet_Bardarbunga_20150130.pdf

• 49. Instructions on using the earthquake pages

  Additionally, some maps contain circular outlines; these features represent volcanic calderas and central volcanoes (Einarsson and Sæmundsson, 1987). Mapped faults and fissures are also shown on some regional maps. Earthquake graphs The graphs show the timing and size of the earthquakes depicted in the map above the graph. The same colour-coding applies to the graphs as to the maps (see /earthquakes-and-volcanism/articles/nr/1225

• 50. Bárðarbunga GPS displacements

  by the propagation of the dyke had become negligible, and from then on the displacement signals from stations around Bárðarbunga can be directly linked to the subsidence of the caldera. Monitoring ceased 19 April 2015. Enlarge. The dates are explained below. Terms, see bottom of page. Dates (yyyymmdd-yyyymmdd) above the cm/year legend. As an example, 20141213-20150113 represents displacement velocities /earthquakes-and-volcanism/gps-measurements/bardarbunga/