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  • 11. Reykholt-abstracts

    in July 2016 on a Delta II rocket from Vandenberg Air Force Base in California. ICESat-2 will carry the Advanced Topographic Laser Altimeter System (ATLAS) and collect data to a latitudinal limit of 88 degrees. In contrast to Geoscience Laser Altimeter System (GLAS) on ICESat, ATLAS employs a 6-beam micro-pulse laser photon-counting approach. It uses a high repetition rate (10 kHz; 70 cm /media/vatnafar/joklar/Reykholt-abstracts.pdf
  • 12. VI_2009_013

    to locate earthquakes in Iceland but the SIL-crustal model has no Moho boundary. Using this model in the routine, daily analysis, the majority of the earthquakes in Eyjafjallajökull form a 3-km-wide chimney between 1 and 10 km depth beneath the northern flank of the volcano. A smaller cloud is also visible between 19 and 25 km depth, about 1.5 km west of the main activity/cluster. 13 Figure 3 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf
  • 13. Journal_of_Hydrology_Veijalainen_etal

    A second, but usually smaller, increase in runoff oc- curs in the autumn. In northern Finland more than 95% of annual maximum floods are caused by spring snowmelt (cf. Fig. 7a). Also the small upstream lakes in the northern part of the lake area and the northernmost of the coastal rivers fall mainly into this cat- egory. In most coastal rivers the major floods can be caused by either snowmelt /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
  • 14. Trausti_Jonsson_(IMO,_Ice)

    Trausti Jónsson (IMO, Ice) - The UN International Strategy for Disaster Reduction (ISDR) - the WMO method and its application in Iceland Abstract Natural hazards have always been a major threat to individuals and the society in Iceland. During a period of optimism after the Second World War it was assumed that progress and modern development would soon marginalize such threats. A series /media/loftslag/Trausti_Jonsson_(IMO,_Ice).pdf
  • 15. A lecture on dust storms from glacial outwash plains

    - The dust could impact on air quality in the British Isles and Europe (in addition to Iceland) - The dust could play a role in ocean biogeochemistry in the high latitudes - Iceland dust may be having an impact on the dust deposition on Summit where dust in ice/snow cores is used as a climate proxy - With global warming and with the retreat of glaciers, we might expect outwash regions to become /about-imo/news/nr/1331
  • 16. Eyjafjallajokull_status_2010-05-15_IES_IMO

    on the ATDnet during the last 24 hours. Noises: No reports. Meltwater: Low water discharge at Gígjökull. Conditions at eruption site: No flight observations, but according to web cameras and instruments there are no major changes. Seismic tremor: Similar to previous week. Earthquakes: An earthquake swarm started beneath Eyjafjallajökull just before midnight. In the period between 23 /media/jar/Eyjafjallajokull_status_2010-05-15_IES_IMO.pdf
  • 17. Eyjafjallajokull_status_2010-05-16_IES_IMO

    Earthquakes: Three small earthquakes were detected beneath Eyjafjallajökull during the night. They were of shallow, intermediate and deep origin. A few shallow earthquakes occurred around 3 pm. GPS deformation: Horizontal displacements towards the center of Eyjafjallajökull volcano and subsidence. Overall assessment: No major changes are seen in the activity. The ash cloud has been /media/jar/Eyjafjallajokull_status_2010-05-16_IES_IMO.pdf
  • 18. norsem_giulia

    a major source of hazard for people and infrastructure. Due to the flank instability of volcanic edifices, landslides, or flank collapses, at active volcanoes can trigger major eruptions or produce tsunami waves when the material enters open or enclosed water bodies. A large landslide occurred at Askja Volcano, Iceland, on July 21st, 2014. The landslide had a total volume between 30 and 50 /media/norsem/norsem_giulia.pdf
  • 19. VI_2020_008

    by the Peak-over-Threshold with MLE applied on daily and 24-hour accumulated precipitation from the ICRA. ............................... 58 8 Glossary 1M5 – Daily or 24-hour precipitation return level with a 5-year return period AMSAnnual Maxima Series CCCloseness Coefficient CDOClimate Data Operator EVA – Extreme Value Analysis GP – Generalized Pareto ICRA – Icelandic /media/vedurstofan-utgafa-2020/VI_2020_008.pdf
  • 20. VI_2009_006_tt

    lake in a volcanic caldera in the interior of the Vatnajökull ice cap (Björns- son, 1988). Jökulhlaups from Grímsvötn have been known since at least the fourteenth century (Þórarinsson, 1939, 1974). In the beginning of the twentieth century there were about ten years between outbursts but the floods diminished with time and became more frequent. After a catastrophic, rapidly rising flood caused /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

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