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• 31. The weather in Iceland 2006

  property. Back to top Documents Back to Annual summaries This article, The weather in Iceland 2006, can be read here in pdf (0.3 Mb) News 2023 2022 2021 2020 2019 2018 2017 2016 2015 2014 2013 /about-imo/news/2007

• 32. The weather in Iceland 2006

  property. Back to top Documents Back to Annual summaries This article, The weather in Iceland 2006, can be read here in pdf (0.3 Mb) News 2023 2022 2021 2020 2019 2018 2017 2016 2015 2014 2013 /about-imo/news/2007/

• 33. The weather in Iceland 2006

  property. Back to top Documents Back to Annual summaries This article, The weather in Iceland 2006, can be read here in pdf (0.3 Mb) News 2023 2022 2021 2020 2019 2018 2017 2016 2015 2014 2013 /about-imo/news/nr/1206

• 34. The weather in Iceland 2006

  property. Back to top Documents Back to Annual summaries This article, The weather in Iceland 2006, can be read here in pdf (0.3 Mb) News 2023 2022 2021 2020 2019 2018 2017 2016 2015 2014 2013 /about-imo/news/nr/1206/

• 35. Flood in Grímsvötn

  been measured at the glacier edge, but they are currently within the health and safety levels. The newest measurements are consistent with the flood forecast model, and it is highly likely that the flood will peak on Sunday.There are past examples of Grímsvötn eruptions started following a flood. The loss of the water from Grímsvötn lake reduces the pressure on top of the volcano /about-imo/news/icesheet-in-grimsvotn-subsiding

• 36. Minor jökulhlaup in Grímsvötn

  discharge of about 500 m3/s from Grímsvötn sub-glacial lake is expected to be reached later today or tonight. The ice-shelf on top of the sub-glacial lake has now subsided approximately 12 m since 5th of October. Since yesterday morning signals of floodwater have been detected in Gígjukvísl river by water level measurements and on images from a web camera. The discharge in Gígjukvísl river /about-imo/news/minor-jokulhlaup-in-grimsvotn

• 37. The Icelandic glaciers weighed from space

  to the diminishing mass of the Greenland ice sheet.The twin GRACE satellites orbit the Earth at 500 km altitude with a distance of 200 km. Variations in the distance between the satellites are monitored with an accuracy of a few micron to measure variations in the Earth's gravity field. (Figure at the top from John C. Ries, The University of Texas Center for Space Research.)Change in gravity field over /about-imo/news/the-icelandic-glaciers-weighed-from-space

• 38. Atlantic

  clouds. They are placed on top of a base map. The satellite images are taken from satellites belonging to the European Organisation for the Exploitation of Meteorological Satellites EUMETSAT and the National Oceanic and Atmospheric Administration NOAA. Most of the images are combined from two satellites /weather/observations/satellites/

• 39. Atlantic

  < Time - 0Time - 1Time - 2Time - 3Time - 4Time - 5Time - 6Time - 7Time - 8Time - 9Time - 10Time - 11Time - 12 > Load all The satellite images are thermal images which show clouds. They are placed on top of a base map. The satellite images are taken from satellites /weather/shipping/satellites/

• 40. Ice subsidence above eastern Skaftá cauldron

  This graph shows the ice-surface lowering (subsidence) of the eastern Skaftá ice-cauldron in Vatnajökull ice cap in October 2015. Vertical displacement (m) was monitored by near real time presentation of data from a GPS station, mounted in the middle of the cauldron. The maximum elevation above sea level, top left (hæð), refers to the zero value on the y-axis; while such value top right /hydrology/research/skafta-cauldron/