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Results:

• 41. Eyjafjallajokull_status__2010-04-25_IES_IMO

  advanced 400-500 m northwards from crater, forming an ice depression extending some 700 m from vents. Seismic tremor: Magnitude similar to what it has been over the last few days. Earthquakes: An earthquake of magnitude 1.4 occurred under NE-part of Eyjafjallajökull this morning. GPS deformation: Indicates very minor subsidence towards the center of the volcano. Magma flow: No observations /media/jar/Eyjafjallajokull_status__2010-04-25_IES_IMO.pdf

• 42. 2010_016

  and the groundwater module. The coupling between both modules was done by a net boundary flux between the unsaturated zone and the groundwater (Schulla & Jasper, 2007). Information on land use, soil type, elevation and other general properties of the watershed are given in static distributed grids while a number of parameters describing specific processes are adjusted to the properties of each /media/ces/2010_016.pdf

• 43. 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

• 44. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 45. NONAM_1st_workshop_summary_v3

  /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 46. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  in the data used in making the decision and the factors are interlinked, all of which makes the problem highly complex. The part of the net defined by variables and links is relatively easily communicated to stakeholders (Henriksen et al., 2007b). However the tal Management 88 (2008) 1025–1036 quantitative part, with the conditional probability tables (CPTs), the numbers, is the step where /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 47. Dyrrdal_Anita_CES_2010

  • Analyse future snow scenarios Introduction Data & Methods Results 0 50 100 150 200 250 300 350 400 450 0-100 100- 200 200- 300 300- 400 400- 500 500- 600 600- 700 700- 800 800- 900 900- 1000 1000- 1100 1100- 1200 1200- 1300 1300- 1400 1400- 1500 1500- 1600 1600- 1700 1700- 1800 1800- 1900 1900- 2000 2000- 2100 2100- 2200 Høyde (m o.h.) A n t a l l v æ r s t a s j o n e r Elevation of met.no /media/ces/Dyrrdal_Anita_CES_2010.pdf

• 48. Katla eruptions

  covered. The central volcano, also called Katla, is located under the Mýrdalsjökull ice-cap but its ice-thickness goes up to 700 m. The associated fissure swarm reaches ~70 km NE towards Vatnajökull. The Katla volcanic system is the fourth most active system in Iceland and has erupted at least 21 times during the last 1100 years. During historical time, the average repose period between /volcanoes/katla/katla-eruptions/

• 49. Daily_status_report_200814

  caldera.Throughout the whole sequence until now, the majority of seismic events have been calculated to be at 5-10 km depth. There is no sign of upward migration. The event rate is still high. ~4000 events have been automatically detected since the beginning of the swarm on Saturday morning, ~700 since midnight today. Activity ebbs and flows in pulses of several hours lengths. The last pulse of high /media/jar/Daily_status_report_200814.pdf

• 50. Avalanche bulletin - Eastfjords

  .a tspan, .sa-active .text .sa tspan, .s-active .text .s tspan, .sv-active .text .sv tspan, .v-active .text .v tspan, .nv-active .text .nv tspan { fill: #1F4E78; font-size: 120%; font-weight: 700; font-size: 120%; } /* Staða */ .status { /* width: 267px; height: 249px; */ width: 80px; height: 74px; } .status .arrow { fill: #6d8fae; display: none; } .status .indic /avalanches/forecast/east_fjords