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Results:

• 31. VI_2022_006_extreme

  no direct glacial influence within its catchment. The glacial cover varies greatly between the catchments, reaching 74% for Hálslón, the only one with a glacial coverage above 50%. Three other catchments have glaciers occupying more than 10% of their surface: Hágöngulón, Sultartangi, and Ufsarlón. Table 1 – Properties of the eleven hydropower catchments. Note that the values are derived from /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 32. 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

• 33. 2010_005_

  day during the 1961–90 control period, differences in percent of the control period between the control period and the 2021–50 reference period, and linear trends in percent of the control period per decade within the 2004–50 period, for the IPCC GCM ensemble mean, the SMHI-RCAO, the MetNo-HIRHAM, and the DMI-HIRHAM5. . . . . . . . . . . 31 10 Mean annual air pressure at mean sea level /media/ces/2010_005_.pdf

• 34. ces-glacier-scaling-memo2009-01

  and ice caps may be derived from data about the area distribution of ice bodies in the drainage basin. Since the exponents g in the volume–area scalings v = csg for both ice caps and glaciers TóJ 3 5.12.2009 Memo Area (km2) Volume (km 3 ) 50 100 50 100 150 200 250 50 100 150 200 250 a71 a71a71 a71 a71 10 50 500 500020 1000 1 5 10 0 100 0 2 2 0 20 0 200 0 100 10000 Icelandic ice /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 35. VI_2015_009

  J600v berg 2.utg) were also used in this study. Table 1. Main characteristics of river basins used in this study. River Name Type Area Mean Percentage Mean annual Period / (km2) elevation glacier precipitation for Gauging (m a.s.l) (mm) streamflow station (1961-2014) data vhm59 Ytri-Rangá L 622 365 0 1564 1961–2014 vhm64 Ölfusá L+D+J+S 5687 480 12.2 2003 1950–2014 vhm66 Hvítá (Borgarfirði) L+J 1577 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 36. VI_2014_006

  The analogue method.............................................................................. 9 2.2.1 Principle and background .............................................................. 9 2.2.2 Prerequisites............................................................................... 10 2.2.3 Predictors .................................................................................. 11 /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 37. Observations - Þverfjall II

  Observations - Þverfjall II | Observations | Icelandic Meteorological office Observations - Þverfjall II Mon 1.05 14 GMT E 10 Max wind : 10 / 12 13 GMT E 9 Max wind : 10 / 11 12 GMT E 9 Max wind : 9 / 10 11 GMT E 8 Max wind : 10 / 12 10 GMT ENE 9 Max wind : 10 / 12 09 GMT ENE 8 Max wind /m/observations/areas

• 38. Daniell_etal-2010

  in the Dhuenn process for various reasons. While the Wupperverband aimed at initiating a participatory process in order to step into an emerging field of power (participatory water management on the way towards WFD implementation) [1; 10; 4; 6], it lacked procedural knowledge on how to design and conduct a participatory process, as well as financial and human resources in this field [1; 5]. The researchers /media/loftslag/Daniell_etal-2010.pdf

• 39. VI_2009_006_tt

  236 1992 09 167 124 167 98 1995 07 1994 1759 599 368 1995 10 96 62 73 37 1997 07 921 728 330 184 2000 08 1240 1083 365 221 2002 09 689 582 267 160 2003 11 241 207 139 98 2006 04 1370 1340 300 270 2008 10 1350 1290 300 265 The origin of the 1957, 1960, 1964 and 1966 jökulhlaups is not certain but is most likely the eastern cauldron. The discharge and volume for the 1995 jökulhlaup are a sum from /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 40. Session program Thursday 13. October

  08:30 – 10:10 Oral session - Chair: Martin Hensch 08:30 – 08:50 Ambient noise tomography of Eyjafjallajökull Ásdís Benediktsdóttir, Ólafur Guðmundsson, Bryndís Brandsdóttir 08:50 – 09:10 Long-period earthquakes recorded on a dense seismic array during the 2014 Bárðarbunga rifting event Bryndís /norsem/norsem2016/program/thursday