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Results:

• 31. The weather in Iceland in 2020

  30.2 220 131 Brjánslækur 1293.6 # 122 69 186 144 Litla-Ávík 1033.2 # 119 35.6 250 164 Litla-Hlíð 472.2 # 123 19.1 204 111 Sauðanesviti 1028.7 # 114 28.8 251 154 Akureyri 762.1 147 121 50.2 212 132 Grímsstaðir 482.4 137 111 33.7 204 105 /about-imo/news/the-weather-in-iceland-in-2020

• 32. VI_Arsskyrsla_2018_vef

  grundvelli myndatöku með flygildum og leysimælitæki (TLS) hefur verið notað við kortlagningu flóðfara og við mat á útbreiðslu og umfangi hlaupa. Þétt net jarðskjálftamæla, sem staðsettir eru á jökulskerjum eða grafnir í jökul, hefur gefið góða raun við ákvörðun á dýpi jarðskjálfta undir jöklum. Kvikuhreyfingar hafa þannig verið kortlagðar og myndun gosrása staðfest af meiri nákvæmni en áður. Þó /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 33. GA_2009_91A_4_Andreassen

  ). Meteorological observations carried out on Storbreen in the summer of 1955 (Liestøl1967) revealed that net radiation is the most impor-tant contributor to the ablation at Storbreen. An au-tomatic weather station (AWS) has bee operatedin the ablation zone of Storbreen since September2001 providing a near-continuous series of meteor- ology and surface energy balance data. Analysis ofthe first five years /media/ces/GA_2009_91A_4_Andreassen.pdf

• 34. CES_BioFuels_Flyer_new

  Participants and organization of project For queries, please contact to: Prof. Seppo Kellomäki (Co-ordinator) Ashraful Alam (Researcher) Faculty of Forest Sciences University of Joensuu P.O. Box 111, FI-80101 Joensuu, Finland. Email: firstname.lastname@joensuu.fi Bioenergy production potential increased due to the climate change both in energy wood thinnings and in final fellings (FF). In addition /media/ces/CES_BioFuels_Flyer_new.pdf

• 35. Crochet_Philippe_CES_2010

  Spring-fed SW Highlands S+(G)+D VHM-66 (G) VHM-64 (G) VHM-43 Glacier covered Central Highlands D+G+S VHM-144 VHM-145 VHM-96 Ice free SW D+S+(L) VHM-81 VHM-301 25% coldest 25% warmest Change in mean yearly maximum discharge ∆Qpeak 100(warmest-coldest)/coldest ∆timing warmest-coldest +1.7°C barb2right +8 % barb2right -25 % barb2right -12 days barb2right -111 days Catchment name Catchment name /media/ces/Crochet_Philippe_CES_2010.pdf

• 36. The weather in Iceland 2014

  146 128 22.5 228 133 Miðfjarðarnes 765.0 120 36.4 233 130 Skjaldþingsstaðir 1980.1 179 115.6 237 162 Dalatangi 2069.6 147 132 72.6 275 189 Höfn í Hornafirði 2060.9 162 57.4 253 189 Vatnsskarðshólar 1851.9 119 111 58.9 270 213 Eyrarbakki 1486.1 108 87 50.0 234 200 Hjarðarland 1203.8 89 35.7 198 158 Keflavíkurflugvöllur /about-imo/news/nr/3082

• 37. ved-eng-2014

  130 Skjaldþingsstaðir 1980.1 179 115.6 237 162 Dalatangi 2069.6 147 132 72.6 275 189 Höfn í Hornafirði 2060.9 162 57.4 253 189 Vatnsskarðshólar 1851.9 119 111 58.9 270 213 Eyrarbakki 1486.1 108 87 50.0 234 200 Hjarðarland 1203.8 89 35.7 198 158 Keflavíkurflugvöllur 1130.6 105 105 43.6 249 172 Precipitation equal to or exceeding 1.0 mm was measured on 160 days in Reykjavik, 12 more /media/vedurstofan/utgafa/skylduskil/ved-eng-2014.pdf

• 38. IPPC-2007-ar4_syr

  a near-zero pre-industrial background concentration, primarily due to human activities. {WGI 2.3, SPM; SROC SPM} There is very high confidence that the global average net effect of human activities since 1750 has been one of warm- ing, with a radiative forcing of +1.6 [+0.6 to +2.4] W/m2 (Figure 2.4). {WGI 2.3, 6.5, 2.9, SPM} The combined radiative forcing due to increases in CO2, CH4 and N2O /media/loftslag/IPPC-2007-ar4_syr.pdf

• 39. VED_AnnualReport-2013_screen

  as river discharge and water levels. Notices on avalanches and sea-ice are shown; short articles and news are presented. Furthermore, web and data portals can be accessed through the web, which is available in both Icelandic and English. IMO uses the social networking website Facebook for communication and feed-back. A new web-application (App) provides access to forecasts and warnings /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 40. Group4

  ); new long-term investment strategy prioritizing low- or zero-net carbon forms of mobility 2040 Modal shift in logistics chains, especially within heavy industry. 3.3 Backcasting scenario narrative Low-Impact Mobility Project Evaluation (LIMPE) Climate change is occurring. Is it natural or anthropogenic? It doesn’t matter. Even though the future is inherently uncertain, one certainty /media/loftslag/Group4.pdf