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• 21. Reykholt-abstracts

  and Gareth Rees Scott Polar Research Institute (SPRI), University of Cambridge, UK Calculation of glacier velocity from repeat lidar survey Lidar measurements of the cryosphere Reykholt, Iceland, June 20–21, 2013 5 Tómas Jóhannesson Icelandic Meteorological Office, Iceland Flow paths of subglacial water detected by lidar measurements of changes in the ice surface elevation of glaciers /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 22. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

  is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and scattered habitation. One of the most important plant community on the islands are along the East coast /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf

• 23. Case_A___Horsens_Fjord

  is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and scattered habitation. One of the most important plant community on the islands are along the East coast /media/loftslag/Case_A___Horsens_Fjord.pdf

• 24. 2010_017

  Iceland VÍ 2010-017 ISSN 1670-8261 Report +354 522 60 00 +354 522 60 06 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 9 150 Reykjavík Bergur Einarsson, Icelandic Meteorological Office Sveinbjörn Jónsson, Icelandic Meteorological Office   5 Contents FIGURES /media/ces/2010_017.pdf

• 25. 2010_016

  Sveinbjörn Jónsson, Icelandic Meteorological Office 4 5 Contents FIGURES .............................................................................................................................. 5 TABLES ................................................................................................................................ 6 1 ABSTRACT /media/ces/2010_016.pdf

• 26. Bardarbunga-2014_August-events

  Office, Institute of Earth Sciences and Cambridge University confirmed the location of the eruption.  The eruption occurred on an old volcanic fissure on the Holuhraun lava field, about 5 km north of the Dyngjujökull ice margin. The active fissure was about 600 m in length.  A small amount of lava drained from the fissure and by around 04:00 UTC, lava flow is thought to have stopped /media/jar/Bardarbunga-2014_August-events.pdf

• 27. VI_2022_006_extreme

  J. Roberts Tinna Þórarinsdóttir VÍ 2022-006 Skýrsla +3 5 4 522 6000 vedur@ve d u r.i s Veðursto f a Ísland s B ú sta ð a rve g u r 7–9 108 Reyk j a vík Contents 1 INTRODUCTION .................................................................................................................. 4 2 STUDY AREA /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 28. Bárðarbunga 2014 - August events

  field, about 5 km north of the Dyngjujökull ice margin. The active fissure was about 600 m in length. A small amount of lava drained from the fissure and by around 04:00 UTC, lava flow is thought to have stopped. According to seismic data and web-camera imagery, the eruption peaked between 00:40 and 01:00 UTC. At the beginning of the eruption, seismic activity decreased, although seismicity has /earthquakes-and-volcanism/articles/nr/3000

• 29. Bárðarbunga 2014 - August events

  field, about 5 km north of the Dyngjujökull ice margin. The active fissure was about 600 m in length. A small amount of lava drained from the fissure and by around 04:00 UTC, lava flow is thought to have stopped. According to seismic data and web-camera imagery, the eruption peaked between 00:40 and 01:00 UTC. At the beginning of the eruption, seismic activity decreased, although seismicity has /earthquakes-and-volcanism/articles/nr/3000/

• 30. Outline_for_the_case_Road_maintenance_in_a_changing_climate

  NONAM PhD course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011 …………………………………………………………………………………………………………………………………………………………………… 1 Outline for the case Road maintenance in a changing climate Introduction Roads and transport systems are vulnerable to climate change impacts (VTT 2011; Koetse and Rietveld, 2009; Regmi & Hanaoka, 2011; Road ERA-net 2009 & 2010 /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf