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Results:

• 1. Sitemap

  Sitemap | Observations | Icelandic Meteorological office Invalid parameter 'g'. Its value is: 58/ but should be an integer. Sitemap Front page Text forecasts | Station forecasts | El. forecasts | Observations Large quakes | Latest quakes | © IMO - Bústaðavegur 9 | 150 Reykjavík | Tel: 522 6000 /m/observations/areas

• 2. Traffc-maintenance_expenditures

  Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009 ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost operating manage- ment develop- poned-, of land grants ons European tax over- level costs ment ment comprehen- build- and com- Regional De- heads 1991- 1991- sive- and ings pensation /media/loftslag/Traffc-maintenance_expenditures.pdf

• 3. CES_D2.4_task1

  SE +56:52:00 +14:48:00 166 TP 2 FALUN SE +60:37:00 +15:37:00 160 T 4 LINKOEPING SE +58:24:00 +15:31:59 93 T 5 LINKOEPING-MALMSLAETT SE +58:24:00 +15:31:59 93 T 8 OESTERSUND SE +63:10:59 +14:28:59 376 T 9 OESTERSUND-FROESOEN SE +63:10:59 +14:28:59 376 T 10 STOCKHOLM /media/ces/CES_D2.4_task1.pdf

• 4. Earthquake sequence at Kleifarvatn

  ). It was widely felt in the capital area and in Akranes. Another magnitude 3.1 event was measured earlier the same day at 11:58 at the same location. Hypocenter depths of the earthquakes were around 3-4 km. This earthquake sequence started in the morning around 10:00 and so far more than 100 events have been detected. Focal mechanisms of the largest events show normal faulting movements (vertical /about-imo/news/nr/3138

• 5. Wind and snow

  in Reykjavík 6.3.2013 As everyone is aware of, very bad weather is prevalent in all of the country. Reykjavík is unusually hard hit by winds and snow. Following is the weather forecast, issued at 15:58, but users of the web are advised to observe the frequently updated maps /about-imo/news/nr/2665

• 6. VI_2015_006

  ....................................................................................... 10 3 September 2012 .................................................................................. 12 3 Radiation fluxes at the surface ....................................................................... 16 4 Heat fluxes at the surface .............................................................................. 21 5 Net energy /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 7. Bardarbunga_Daily_status_report_250814

  Bárðarbunga update 25082014 2014-08-25 13:58 UTC Bárðarbunga update Compiled by Hildur María Friðriksdóttir, Benedikt G. Ófeigsson, Melissa Anne Pfeffer, Sara Barsotti, Kristjana Eyþórsdóttir Based on Seismic, GPS, Hydrology Eruption plume Height (a.s.l.) No eruption and no eruption cloud. Heading No eruption and no eruption cloud. Colour No eruption and no eruption cloud. Tephra fallout /media/jar/Bardarbunga_Daily_status_report_250814.pdf

• 8. GA_2009_91A_4_Andreassen

  and asimplified mass balance model suggests that airtemperature and albedo is satisfactorily parameter-ised, at least for the AWS altitude. However, thecompared period covers only 5 of the 58 modelledyears in this study. Furthermore, the specific win-ter, summer and net balances measured at Stor-breen in 2001–2006 deviate markedly from the mean for the whole observation period. A combi-nation /media/ces/GA_2009_91A_4_Andreassen.pdf

• 9. VONA message

  and gave a flux of SO2 between 48 and 58 kg/s. All the activity is taking place in the area where, prior to the eruption, a magmatic intrusion was detected and mapped. In light of the recent developments, it cannot be excluded that more fractures will open along the same alignment. Because of the lack of ash and the minor tephra emission in the atmosphere, the aviation color code /earthquakes-and-volcanism/volcanoes/vona-notifications/

• 10. Bardarbunga_daily_status_report_21082014

  the Dyngjujökull glacier at 5 - 10 km depth. The dyke has not propagated to the north-east, nor has it progressed to shallower depth. Today three earthquakes exceeding three in magnitude have occurred on the caldera rim of Bárðarbunga (M 3.7 at 10:29, M 4.0 at 10:58 and M 3.4 at 13:02). These earthquakes were at depths around 2 - 5 km. They are interpreted as possible adjustments of the caldera due to changing /media/jar/Bardarbunga_daily_status_report_21082014.pdf