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• 31. VI_2020_005

  and CNES, n.d.; National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 32. VI_2017_009

  we take the corresponding data from the CMIP5 project. Table 1. All GCMs and RCMs used in this study. If a model is available for any of the domains Arctic-44, EURO-44, or EURO-11, it is marked with a v, but with an x if it is unavailable. Model name Type EURO-11 EURO-44 Arctic-44 CCCma-CanESM2 GCM x v v COSMO-CLM4-8-17 RCM v v x CNRM-CERFACS-CNRM-CM5 GCM v v x IHCEC-EC-Earth GCM v v v /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 33. VI_2015_005

  Franz Josef Land. The western boundary at 71 W excludes Hudson Bay and Foxe Basin, both associated with their own storm climate. Baffin Bay is included in its entirety, since storm activity in that region is closely linked to that over the western North Atlantic (Dacre & Gray, 2009). The eastern boundary at 55 E is chosen to completely include the Barents Sea. This results in an area of 21,625,566 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 34. CES_D2.4_task1

  is projected to approach 90%. The impact of anthropogenic climate change on precipitation is still estimated to be very small at present. In the middle of this century, typically about 60% of all months are projected to have above-median precipitation in northern Europe, although with a substantial variation with the time of the year. An on-line appendix of this report provides detailed tables /media/ces/CES_D2.4_task1.pdf

• 35. VI_2016_006_rs

  of 100–140 m a.s.l. Several debris flows are recorded in Búðará since the beginning of the 20th century. It is not clear whether the upper or lower area is the main source for these debris flows. The return time for sizeable debris flows in Búðará is around 20 years. It appears that the land- slide activity has been more frequent in the last 30 years than earlier in the 20th century. 4.5 Areas 7 /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 36. VI_2019_009

  26 36 40 41 46 50 51 52 53 54 58 60 61 62 63 64 65 68 70 71 72 73 74 80 81 83 84 85 86 87 92 Present weather (Manual) Present weather ( Automatic ) Number of records a71 a71 a71 250 500 750 250 500 750 Number of records Figure 15. Automatic station as a function of manual station. a71 a71a71a71a71a71 a71a71 a71a71a71 a71a71 a71 a71 a71a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71a71a71 /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 37. VI_2015_007

  of Iceland, Science Institute, University of Iceland, and National Energy Authority. 2004), a soil map from the Agricultural University of Iceland and a vegetation map from the Icelandic Institute of Natural history were also used in this study. 8 Table 1. Main characteristics of river basins used in this study. Catchment Name Area Mean Mean annual Available period / (km2) elevation precipitation /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 38. VI_2020_011_en

  particles formed as the magmatic gases age (most notably, SO4 aerosol is formed from SO2 gas), and from tephra particles (the finest ash can be breathed in, and the acidic coatings on tephra particles can acidify and pollute fresh water). One person died due to CO2 accumulation in a basement during the 1973 Eldfell eruption. During the eruption, rescue 22 workers needed to be aware of escape /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 39. 2010_003rs

  ................ 91 Figure B.5. Rake distribution for mapped faults/clusters in boxes E and F, Brennisteinsfjöll-Bláfjöll. ................................................................................. 92 Figure B.6. Rake distribution for mapped faults/clusters in box G, Ölfus. ......................... 93 Figure B.7. Rake distribution for mapped faults/clusters in box H, Hengill, active between January /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 40. VI_2013_008

  on the use of analogues. Analogue-based methods have been used with success in streamflow forecasting. They are often referred to as nearest-neighbor methods (Karlsson & Yakowitz, 1987; Galeati, 1990; Akbari et al., 2011). The first step of the technique is to compare a current situation to all past situations collected in an historical archive, according to a set of attributes describing /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf