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• 11. A small jökulhlaup in Gígjukvísl

  The event originates from the subglacial lake Grímsvötn. The event is expected to be small, with maximum discharge on the order of magnitude 1000 cubic meters per second. The maximum of the flood is expected to be around the end of the week. Conductivity measurements indicate a considerable increase of geothermal contribution to the water of the river. Simultaneously, the ice on the subglacial lake /about-imo/news/nr/2859

• 12. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  2004 after finishing the case study. Newspapers were distributed to 1000 households in the local area. At the final joint meeting where both groups participated in March 2004 (step 7), the stakeholder groups were asked to comment on the involvement process on the basis of four questions: (1) Is there a need for further initiatives for the protection of groundwater? (2) How have you experienced /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 13. VI_2020_005

  flooding, sea level, sea level rise, risk assessment, natural hazard This work was carried out for the Icelandic Meteorological Office and is a part of Masters Thesis ISSN 1650-6553 No. 470, published by the Department of Earth Sciences at Uppsala University in 2019. The Masters Thesis is available as a whole at www.diva-portal.org. Copyright c Guðrún Elín Jóhannsdóttir Contents 1 Introduction /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 14. VI_2019_009

  To distinguish between rain and snow, the volume is com- pared to the water equivalent but the volume of snow is ten times larger. Figure 1. How PWD22 determines the type of precipitation. Using the information about the changes of the backscatter signal, water equivalent and temper- ature the Vaisala Present Weather Detector can give information about the type of precipitation. It is also used /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 15. Bardarbunga_daily_status_report_31082014

  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 rate about 1000 m3 per second. There has been poor visibility until 11:30 UTC, then it has been moderate. The eruptive fissure is visible since then and magma extrusion is still ongoing. White steam rising from the eruption is also visible. Seismic tremor /media/jar/Bardarbunga_daily_status_report_31082014.pdf

• 16. Journal_of_Hydrology_Veijalainen_etal

  in autumn and winter in the 100a flood from observations (m3 s) 100a flood from simulation s (m 3 s) a 1 10 10 0 100 0 1000 0 1 10 100 1000 10000 0. 1 1 10 10 0 100 0 0.1 1 10 100 1000 Average discharge from observations (m3 s) Average discharge from simulation s (m 3 s) b Fig. 4. Comparison of simulated (with observed temperatures and precipitations) and observed values in 1971–2000 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 17. VI_2020_004

  49 Probabilistic hazard map for a load ≥1000 kg/m2 (Öræfajökull) ............................ 78 Figure 50 Seasonal analysis for 1 kg/m2 (~1mm) tephra ground load (Öræfajökull). ............ 79 Figure 51 Seasonal analysis for 10 kg/m2 (~1 cm) tephra ground load (Öræfajökull). ........... 80 Figure 52 Impact map for roads in case of an eruption like 1362 at Öræfajökull ................... 81 /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 18. ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN

  changes in many natural systems. Moreover, it also presents, in a greater or lesser extent, economical effects in nearly every sector of activity. In this context, the tourism will be particularly affected [1; 2]. There will be regional and seasonal shifts in global tourist flows, leaving some countries more vulnerable to shifting climatic conditions [3]. European Mediterranean countries /media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf

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

  ; Guðmundsson et al., 2009b; see locations of the ice caps in Fig. 1). Constant lin- ear vertical and horizontal precipitation gradients (0.5 per 100 m in vertical, 0.005 and −0.008 per 1000 m in hori- zontal east and north direction, respectively) are used in the model to take into account observed precipitation vari- ations, assuming a constant snow/rain threshold of 1 ◦C. In a previous study /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 20. Bardarbunga_kafli20140825

  (km3): No information Longest lava flow, km: No information Gas emissions, sulphur: No information Interval between eruptions, years: (last 1000 years) Max: >100 years, min: <1 year Last significant eruption: 1910 CE Seismic characteristics Persistent seismic activity. No information on previous eruptions. Seismic swarms expected Deformation characteristics No information on previous /media/jar/Bardarbunga_kafli20140825.pdf