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• 51. Gale force wind in Westfjords

  the weather will worsen considerably between 2 – 3 PM with these high winds and snow. This evening and tonight, northeasterly winds 20-28 m/s are forecasted with snow and hail in all the Westfjords. Tomorrow morning, 10 December, winds will calm down. North of Iceland there is a fast deepening low which will reach 945 hPa at the mouth of Húnaflói bay this afternoon. West of this low, the winds /about-imo/news/nr/3032

• 52. askja_minnisblad_ens

  and rescue team saw a white plume rise up above Askja at 23:27. The steam plume was created when the slide exposed shallow geothermal areas in the release area. In addition, a dust cloud created by the rock slide may have contributed to the plume. The release area of the rockslide is approximately 800 m wide and 350 m above the lake surface. It may have been a "rotational slide movement", which /media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf

• 53. 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

• 54. Lettenmaier_Dennis_CES_2010pdf

  ) Colorado River basin C) Washington climate change impacts assessment – Yakima River basin 3a) Hydrology and water management implications: Columbia River Basin PCM Business-as-Usual scenarios Columbia River Basin (Basin Averages) control (2000-2048) historical (1950-99) BAU 3-run average PCM Business-As- Usual Mean Monthly Hydrographs Columbia River Basin @ The Dalles, OR 1 month /media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf

• 55. VI2010-006_web

  milli byggðarinnar á Akureyri og í Fjörunni um aldamótin. Um 1898 var gerður skipulagsuppdráttur af Torfunefi, neðan Grófargils. Þar efldist byggðin og upp úr aldamótunum og myndaðist þar vísir að miðbæ alls kaupstaðarins. Um þetta leyti fór að gæta hnignunar í Innbænum og flestum meiriháttar byggingum var nú valinn staður í norðurhluta bæjarins. Húsbrunar settu þar að auki mark sitt á byggðina á /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 56. norsem_korja

  reactivation type (reverse, normal or strike slip) based solely on their azimuth. The earthquakes in the seismically most active area, close to Skellefteå, Sweden along the western coast of the Gulf of Bothnia and its north-easterly continuation, appear to cluster around the shoreline and along post-glacial faults, which are mostly oriented optimally for reverse or strike slip faulting /media/norsem/norsem_korja.pdf

• 57. GA_2009_91A_4_Andreassen

  (+0.09) m w.e. The model is (of course) highly sens tive to the chosen values of c0 and c1 (Table5) The model sensitivity to a decrease in ice andfirn albedo is higher when the perturbation is ap-plied in a w rmer climate. Reducing the ice albedo fr m 0.3 to 0.2 to the combined +2°C and Table 4. Modelled change in specific winter (∆bw), summer (∆bs) andnet balance (∆bn) (in m w.e.) and in days /media/ces/GA_2009_91A_4_Andreassen.pdf

• 58. hafisskyrsla-23-mars-2011

  °35V 5. 66°31N 024°55V 6. 66°42N 024°26V 7. 67°03N 023°44V 8. 67°14N 023°29V 9. 67°33N 022°26V Var ísinn 7-9/10 að þéttleika og sást greinileg nýmyndun inn á milli þar sem hann var gisnari. Ekki var að sjá stóra jaka eða borgarísjaka í jaðri ísins svo gera má ráð fyrir að hann sjáist ekki vel á ratsjá. Út frá ísröndinni sáust nokkrar ísdreifar og voru teknir staðir á þeim. 1. 65°51N 026°39V /media/hafis/skyrslur_lhg/hafisskyrsla-23-mars-2011.pdf

• 59. isskyrsla_14122010

  15.0W 9) 67 05.0N 21 52.0W 10) 66 57.0N 22 32.0W 11) 67 00.0N 23 00.0W 12) 66 38.0N 25 00.0W 13) 66 30.0N 26 40.0W Næst landi var ísinn á eftirfarandi stöðum: 1. 48 sjml vnv af Grímsey. 2. 46 sjml ana af Horni. 3. 34 sjml norður af Skagatá. 4. 25 sjml nnv af Sraumnesi. Kl 0003 Kallað í Remoy Viking k/m LLDM til að fá upplýsingar um ísinn sem hann er að sigla í gegnum /media/hafis/skyrslur_lhg/isskyrsla_14122010.pdf

• 60. CES_D2.4_task2_CMIP3_winds

  in the average wind speed between the baseline (or control) period 1971-2000 and the scenario period 2046-2065. These periods were chosen based on the availability of model output at daily time resolution. We have analyzed the surface geostrophic wind (hereafter Vg) rather than the actual simulated surface winds, because the latter are sensitive to the details of the boundary layer /media/ces/CES_D2.4_task2_CMIP3_winds.pdf