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Results:

• 1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  with whom a slot is proposed to be swapped. In the closing session on Friday afternoon another two Workshop participants will be offered the opportunity of presenting a brief summary of key impressions and messages (2 x 5 minutes). This will require some degree of co-ordination among the rapporteurs. The Conference organizers need to know in time (Friday morning at the latest) who will present /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 2. Traffc-maintenance_expenditures

  127 308 1 106 709 2007 .. 611 148 6) 2) 177 646 21 377 4) 30 820 14 021 - 10 141 165 567 319 1 031 039 1 092 234 2006 .. 612 044 6) 2) 113 312 22 002 4) 34 446 14 868 - 15 888 151 738 368 964 666 1 070 901 2005 .. 599 686 5) 2) 154 481 28 661 4) 27 846 13 748 - 12 079 159 879 379 996 759 1 169 271 2004 .. 587 176 2) 141 446 59 834 4) 24 546 10 342 - 6 326 164 502 573 994 745 1 226 881 2003 .. 627 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 3. VI_2022_006_extreme

  in the lowlands, the snow-fraction never exceeds 80%. Percentage changes, as calculated from the regression line between the beginning and the end of the ICRA time-period, are given for all the catchments. Those results are also shown with a color code on a map (see Figure 10). Overall, the catchments oriented on the southern parts of the glaciers (Sultartangi, Þórisvatn, Tungnaá /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 4. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  %) 14 (26%) 39 (74%) Gender Number (%) E I S N T F P J Male 100 (48%) 47 (47%) 53 (53%) 15 (15%) 85 (85%) 59 (59%) 41 (41%) 29 (29%) 71 (71%) Female 109 (52%) 66 (61%) 43 (39%) 22 (20%) 87 (80%) 43 (39%) 66 (61%) 21 (19%) 88 (81%) Climatic Change (2012) 112:233–242 237 symposia participants were not significantly different from the preferences of the U.S. general population, which was 49 /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 5. Sitemap

  Sitemap | Observations | Icelandic Meteorological office Invalid parameter 'g'. Its value is: 80/ but should be an integer. Sitemap Front page Text forecasts | Station forecasts | El. forecasts | Observations Large quakes | Latest quakes | © IMO - Bústaðavegur 9 | 150 Reykjavík | Tel: 522 6000 /m/observations/areas

• 6. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  of the three ice caps under consideration, the horizontal displacement of the HRS and DMA DEMs (40 m40 m spatial resolution) relative to the EMISAR DEM (5 m5 m spatial resolution) was eliminated by both maximizing the correlation and minimizing the standard deviation of the elevation differences of ice-free areas in the vicinity of the glaciers (gently sloping areas within ca. 80
  800 m away /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 7. VI_2020_008

  /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 8. Snorrason_Arni_CES_2010

  – Energy market aspects • Scale: – Total: 20.8 MNOK – TFI: 12.3 MNOK Estimated Global Sea level rise Vermeer and Rahmstorf 2009 Estimated Global Sea level rise at 2100 Rahmstorf 2010 Deformation of Iceland due to mass loss from glaciers Þ. Árnadóttir et al., GJI, 177 Area of inundation: 1m sea level rise Stability of Arctic Land Ice: SVALI • CES Snow and Ice Group • Many partners from the Nordic /media/ces/Snorrason_Arni_CES_2010.pdf

• 9. VI_2009_013

  and the Eastern Volcanic Zones (WVZ and EVZ (Figure 1). The two segments are connected through a 70–80 km long transform zone, the South Iceland Seismic Zone (SISZ), which regularly produces a sequence of large, destructive earthquakes of magnitudes up to M7 (Einarsson et al., 1981; Einarsson, 2008). The majority of the rifting is taken up by the southward propagating and much more active EVZ /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 10. The weather in Iceland 2014

  prec.days >=1.0 mm Reykjavík 963.1 121 112 37.6 223 160 Stafholtsey 829.4 97 28.0 182 144 Bláfeldur 1460.7 97 32.0 272 195 Stykkishólmur 678.8 96 87 20.0 218 136 Litla-Ávík 835.0 96 34.1 267 164 Bergstaðir 458.2 98 22.6 177 92 Sauðanesviti 1017.5 115 28.2 239 158 Akureyri 743.7 152 133 23.0 225 133 Grímsstaðir 514.8 /about-imo/news/nr/3082