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Results:

• 21. 2010_017

  of radiation are added to a classic degree-day model. For infiltration, a methodology of Peschke, based on the approach of Green and Ampt, was used. To calculate the fluxes within the unsaturated soil zone, the Richards equation was used. The groundwater table was modelled in both the unsaturated zone module and the groundwater module. The coupling between both modules was done by a net /media/ces/2010_017.pdf

• 22. NONAM_1st_workshop_summary_v3

  /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 23. 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

• 24. 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

• 25. 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

• 26. 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

• 27. VI_Arsskyrsla_2018_vef

  grundvelli myndatöku með flygildum og leysimælitæki (TLS) hefur verið notað við kortlagningu flóðfara og við mat á útbreiðslu og umfangi hlaupa. Þétt net jarðskjálftamæla, sem staðsettir eru á jökulskerjum eða grafnir í jökul, hefur gefið góða raun við ákvörðun á dýpi jarðskjálfta undir jöklum. Kvikuhreyfingar hafa þannig verið kortlagðar og myndun gosrása staðfest af meiri nákvæmni en áður. Þó /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 28. 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/

• 29. 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

• 30. Factsheet-Bardarbunga-140901

  500 earthquakes detected since midnight today. Most of the seismicity is occurring on the northern end of the dyke intrusion, covering a 15-km-long region that extends partly beneath Dyngjujökull and north of the ice margin. At 08:58 UTC today, a magnitude 5.0 earthquake was recorded on the Bárðarbunga caldera, and another of magnitude 5.2 at 11:41 UTC in the same region. It remains unclear /media/jar/Factsheet-Bardarbunga-140901.pdf