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Results:

• 11. Adalgeirsdottir-etal-tc-5-961-2011

  (DGPS) equipment in 2001. Continuous profiles, approximately 1 km apart, were measured in the accumulation zone and a dense net- work of point measurements were carried out in the abla- tion zone. Digital Elevation Models (DEMs) of the surface and bedrock were created from these data (Fig. 2; Björns- son and Pálsson, 2004). The estimated errors are at most 1–5 m (bias less than 1 m) for the surface /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 12. Bardarbunga_Daily_status_report_260814

  by the current seismic activity in the past 24 hours. Model calculations, based on GPS data suggest that a total volume of up to 350 million cubic meters have intruded into the crust since the activity started. Overall assessment There are no indications that the intensity of the activity declining. Currently, three scenarios are considered most likely: 1) The migration of magma could stop, attended /media/jar/Bardarbunga_Daily_status_report_260814.pdf

• 13. VI_2014_005

  , Veðurstofu Íslands   Contents 1 Introduction ................................................................................................ 7 2 Model setup and data ................................................................................... 7 3 Model terrain and surface type ...................................................................... 9 4 Impact of initial conditions in blending /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 14. ces-oslo2010_proceedings

  Conference on Future Climate and Renewable Energy: Impacts, Risks and Adaptation 31 May - 2 June 2010 Soria Moria Hotel and Conference Center, Oslo, Norway Conference proceedings 1 Conference proceedings Future Climate and Renewable Energy: Impacts, Risks and Adaptation 31 May – 2 June 2010 Soria Moria Hotel and Conference Center, Oslo Norway Published by: Norwegian Water /media/ces/ces-oslo2010_proceedings.pdf

• 15. ces_geus_paakitsoq_full_report

  ) is shown. At the margin the grid boxes of the RCAO RCM are visible. The area between Illulisat and Swiss camp is commonly called Paakitsôq. respectively. The Automatic Weather Stations (AWS) Swiss Camp and Crawford are located on the ice sheet and are operated by the Greenland Climate Network (GC-net) (Steffen and Box, 2001). The locations of the stations are indicated in Fig. 1, further details /media/ces/ces_geus_paakitsoq_full_report.pdf

• 16. Reykholt-abstracts

  Reykholt, Iceland, June 20–21, 2013 1 Content Sessions ...................................................................................................................................... 4 Programme ............................................................................................................................... 4 List of participants /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 17. Lawrence_Deborah_CES_2010

  ECHAM4/OPYC3 NorClim/HIRHAM 25x25 km 'Empirical Adjustment' to 1 x 1 km 100 150 200 250 300 350 400 450 500 550 600 650 700 750 800 850 900 1 10 100 1000 Return period (years) P e a k d a i l y d i s c h a r g e ( m 3 / s ) 1981-2010 GEV from annual max series 2021-2050 GEV from annual max series 2021 - 2050 Annual maximum series 1981 - 2010 Annual maximum series 1981-2010 200-year flood 2021 /media/ces/Lawrence_Deborah_CES_2010.pdf

• 18. 2010_017

  ............................................................................................................................... 5 TABLES ................................................................................................................................. 6 1 ABSTRACT ..................................................................................................................... 7 2 INTRODUCTION /media/ces/2010_017.pdf

• 19. Hazard zoning

  in the legend (left part of the map) and in the figure caption (the phrase below the map). The colour scale reports different values of likelihood (under 1% has no colour). The maps have been made considering 10 years of meteorological data and computing the ground concentration each hour with the CALPUFF gas dispersion model. The results have been plotted considering the wind variability across /pollution-and-radiation/volcanic-gas/hazard-zoning/

• 20. feltvinna-JHI_2015feb_11-12

  gosopa um miðbik Baugs, sem eru aðskilin af um 350 m. Mynd 1. Tekin að kveldi 11. febrúar úr vestri. Gosop um miðbik áberandi. Seinna gosop er til hægri á mynd en ekki eins kröftugt. 12. febrúar 2015 Í dag var stefnan sett á að klífa suðurhlíðar Baugs og líta yfir hrauntjörnina. Suðurbarmar eru um 400 m frá syðsta gosopi. Veður var hagstætt, gosgufur leggur til austurs. Komnir á gígbarma upp úr /media/jar/feltvinna-JHI_2015feb_11-12.pdf