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• 21. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

  NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop in Reykjavík 26 – 27 August 2010 1 HORSENS FJORD CASE Jes Pedersen, Rolf Johnsen and Hans Jørgen Henriksen 1. Background to the case Introducing the catchment Horsens estuary is a shallow and eutrophic estuary located on the east side of Jutland, Denmark within the WFD catchment area Horsens Fjord (Fig. 1 /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf

• 22. Case_A___Horsens_Fjord

  NONAM Risk Assessment and Stakeholder Investment. Multidisciplinary Workshop in Reykjavík 26 – 27 August 2010 1 HORSENS FJORD CASE Jes Pedersen, Rolf Johnsen and Hans Jørgen Henriksen 1. Background to the case Introducing the catchment Horsens estuary is a shallow and eutrophic estuary located on the east side of Jutland, Denmark within the WFD catchment area Horsens Fjord (Fig. 1 /media/loftslag/Case_A___Horsens_Fjord.pdf

• 23. 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

• 24. Journal_of_Hydrology_Veijalainen_etal

  in estimation of climate change impacts on flooding. Generalisations based on only a few case studies, or large scale flood assessments using only a few climate scenarios should be avoided in countries with var- iable hydrological conditions.  2010 Elsevier B.V. All rights reserved. 1. Introduction Climate change has a multifaceted impact on river discharges: on the one hand it poses a risk of increased /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 25. NONAM_1st_workshop_summary_v3

  .......................................................... 16  Concluding remarks from the break out sessions – comparing the water sector and road infrastructure........................................................................................................................ 24  Annex 1. Task of break out groups ..................................................................................... 25  Annex 2 /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 26. 2010_017

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

• 27. 2010_016

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

• 28. Bárðarbunga 2014 - August events

  the event than in the previous eruption, but more lava is being extruded. At 07 AM the lava flow was around 1 km wide and 3 km long towards northeast. The thickness was estimated a few meters, the flow about 1000 m3 pr second. Approximately 500 earthquakes were detected in the area and smaller than before. The strongest earthquake, M3.8 was in the Bárðarbunga caldera. Poor weather conditions prevail /earthquakes-and-volcanism/articles/nr/3000

• 29. Bardarbunga-2014_August-events

  It was detected on Míla´s web-camera at 05:51 AM. Fewer earthquakes seem to follow the event than in the previous eruption, but more lava is being extruded.  At 07 AM the lava flow was around 1 km wide and 3 km long towards northeast. The thickness was estimated a few meters, the flow about 1000 m3 pr second.  Approximately 500 earthquakes were detected in the area and smaller than before /media/jar/Bardarbunga-2014_August-events.pdf

• 30. Bárðarbunga 2014 - August events

  the event than in the previous eruption, but more lava is being extruded. At 07 AM the lava flow was around 1 km wide and 3 km long towards northeast. The thickness was estimated a few meters, the flow about 1000 m3 pr second. Approximately 500 earthquakes were detected in the area and smaller than before. The strongest earthquake, M3.8 was in the Bárðarbunga caldera. Poor weather conditions prevail /earthquakes-and-volcanism/articles/nr/3000/