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• 81. Wind, temperature and precipitation forecasts

  code, given that NEITHER page is registered for Coordinated Webmeasure. Strict rules apply to the latter, where each visit should only be counted once. Because our web, vedur.is, is registered for Coordinated Webmeasure, our frames are registered too. Therefore, web-pages showing our frames must not be registered. As stated above, web-sites that are registered can still show our frames by having /about-imo/the-web/iframes/wind-temp-precip/

• 82. Bárðarbunga 2014 - August events

  activity in NW-Vatnajökull is still very strong, 700 earthquakes have been observed since midnight and they are somewhat larger than previous days. Two large earthquakes, over 5 where in the Bárðarbunga caldera this night. The activity under Dyngjujökull has propagated northwards and is now mostly under the edge of the glacier, where an earthquake of size 4,2 was recorded this morning /earthquakes-and-volcanism/articles/nr/3000

• 83. Bárðarbunga 2014 - August events

  activity in NW-Vatnajökull is still very strong, 700 earthquakes have been observed since midnight and they are somewhat larger than previous days. Two large earthquakes, over 5 where in the Bárðarbunga caldera this night. The activity under Dyngjujökull has propagated northwards and is now mostly under the edge of the glacier, where an earthquake of size 4,2 was recorded this morning /earthquakes-and-volcanism/articles/nr/3000/

• 84. Bardarbunga-2014_August-events

  and they are somewhat larger than previous days.  Two large earthquakes, over 5 where in the Bárðarbunga caldera this night.  The activity under Dyngjujökull has propagated northwards and is now mostly under the edge of the glacier, where an earthquake of size 4,2 was recorded this morning.  The dike under Dyngjujökull is now estimated to be approximately 30 km long /media/jar/Bardarbunga-2014_August-events.pdf

• 85. VI_2013_008

  of letters indicates the origin of flow with the first letter indicating the primary origin. Three of these catchments are partly glaciated and two of them have a large groundwater contribution (vhm 64 and vhm 66). A more detailed de- scription of the hydrology of these catchments can be found in Crochet (2013) where a study of their hydrologic response to recent climate variations is presented /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 86. Perrels-CBA

  Permanent Transient Mode I: Slow and fundamental • Sea level rise (navigation effects, flood risks) • Retreat of sea ice (with annual fluctuations) • Increased weather variability, notably worse winter conditions Mode II: Slow underlying trends culminating in quick changes • Exponential growth of algae in the Baltic Sea and in lakes (impacts or tourist travel) • Collapsing fish /media/loftslag/Perrels-CBA.pdf

• 87. VI_2017_009

  The errors in the sea ice cover and precipitation are sufficiently large that we can justify omitting these models directly in the 21st century climate projections. Table 5. Average deviations between GCMs and HAMRONIE for Ptot (Total precipitation per year) and GCMs and ERA-Interim for Tavg (Average temperature). SI (Sea ice cover): These are differences of percentages between the GCMs and ERA /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 88. Factsheet_Bardarbunga_20150106

  between M4,0-5,0. The strongest one was M4,9 last night, 5. December, at 21:53. About 50 earthquakes were detected in the dyke of the same period, most of them smaller then M1,0. One earthquake was M2,0 yesterday, 5. January, at 02:26.  Seven earthquakes were detected in Tungnafellsjokull glacier during the period. The strongest one was around M3,0 on 30. December at 16:51.  GPS /media/jar/Factsheet_Bardarbunga_20150106.pdf

• 89. Factsheet_Bardarbunga_20141103

  207 earthquakes have been detected in the caldera. Two earthquakes were bigger then M5,0, on 31. October at 21:32 an M5,2 earthquake was detected and M5,3 on 2. November at 16:02. In total 27 earthquakes between M4 and 5 were detected and 8 between M3 and 4. • The GPS station in the centre of Bardarbunga show that the subsidence of the caldera continues with similar rate as it has done over /media/jar/Factsheet_Bardarbunga_20141103.pdf

• 90. CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction

  and railway owners  Support of road and rail constructions is threatened by rising groundwater and flooding.  Need knowledge of where to reconstruct and if possible identify where roads can act as dykes or reservoirs in case of flooding. Nature  Diversity threatened due to intensive use of land.  Need to develop new biotopes. Nutrients and good ecological status of the fiord The fjord /media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf