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  • 81. Bardarbunga-2014_October-events

    earthquakes were observed in the dike intrusion and about 20 close to Herðubreið. The eruption can not be seen on the webcams. 9 October 2014 - a high definition image of the lava Holuhraun lava field Excerpt from a satellite image 7 October 2014 for the IsViews project at LMU which Fjarkönnun is part of. This Quicklook radar image from TerraSAR-X, irrespective of weather and visibility, shows /media/jar/Bardarbunga-2014_October-events.pdf
  • 82. Bárðarbunga 2014 - October events

    Holuhraun lava field Excerpt from a satellite image 7 October 2014 for the IsViews project at LMU which Fjarkönnun is part of. This Quicklook radar image from TerraSAR-X, irrespective of weather and visibility, shows the outlines of the new lava in exceptionally high detail (see full image) as they were two days ago. Referral: (c) DLR/ Fjarkönnun ehf./IsViews 10/2014. 9 October /earthquakes-and-volcanism/articles/nr/3011/
  • 83. Gudmundsson-etal-2011-PR-7282-26519-1-PB

    from the glacier margins). This was done by shifting the x and y coordinates of the 40 m40 m DEMs in 5 m steps and calculating the correlation to the corresponding values of the 5 m5 m EMISAR DEM. In all cases, both the maximum correla- tion and minimum standard deviation yielded the same shift. After the co-registration, the same ice-free areas were used to correct the vertical offset of the DMA /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
  • 84. VI_2022_006_extreme

    of the melt season as retrieved by the third filtering method. 15 4.1.2 Results For each catchment, all the dates retrieved by the last filter were stored in a table. These dates were then plotted together, as shown for four catchments in Figure 7. Results for the other catchments are included in Appendix I (Figures I.1 – 11). On each plot, the x-axis shows the 39 years used for the study /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
  • 85. Linnet_Ulfar_CES_2010

    °C/100y 1975-2000 • 2.35 °C/100y 2000- •Change in precipitation • Average increase 4.8% / 100 y • Range 3.3 – 7.2 % •Glaciers • Results from CES • 25% decrease in volume from 2000 to 2050 Temperature transformation Com parison of series 10000 12000 14000 16000 18000 20000 22000 1 9 5 0 1 9 5 2 1 9 5 4 1 9 5 6 1 9 5 8 1 9 6 0 1 9 6 2 1 9 6 4 1 9 6 6 1 9 6 8 1 9 7 0 1 9 7 2 1 9 7 4 1 9 7 6 1 9 7 8 1 /media/ces/Linnet_Ulfar_CES_2010.pdf
  • 86. ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN

    /lexuriserv/lexuriserv.do?uri=com:2007:0002:FIN:EN:PDF, 13 April 2009. [2] WTO, World Tourism Organization (2008): “Climate Change and Tourism - Responding to Global Challenges”, UNWTO, 9 July 2008, Madrid, Spain. Available at: http://www.unwto.org/media/news/en/press_det.php?id=1411&idioma=E, 7 March 2010. [3] Mooney, J.E. y Miller, M.L. (2009): “Climate change: Creating demand for sustainable /media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf

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