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

    During the conference all of you are requested to act as rapporteur in two or three sessions. A preliminary allocation of rapporteur sessions has been made (see below), while accounting for your expertise in certain areas. Participants can suggest changes in the rapporteur session allocation, on the condition a convincing argumentation is provided as well as a confirmed alternative rapporteur /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
  • 2. hafisskyrsla_11052011

    Hafísskýrsla TF-SIF 11. maí 2011 Flug nr. 03511.025 Ískönnunarflug 11. maí 2011 Í dag var farið í ískönnunarflug um vesturmið. Enginn hafís var sjáanlegur í íslenskri lögsögu, en þéttur hafís rétt inn þeirrar grænlensku. Gerðum hafískönnun með SLAR ratsjá og ELTA eftirlitsratsjá. Skyggni á svæðinu leifði ekki athugun með berum augum. Hér neðan fylgir punktalisti yfir legu /media/hafis/skyrslur_lhg/hafisskyrsla_11052011.pdf
  • 3. Publications 2014

    on the combined use of a hydrological model and an analogue method Philippe Crochet 68 2,8 2014-005 Evaluation of HARMONIE reanalyses of surface air temperature and wind speed over Iceland Nikolai Nawri 31 12 2014-001 Flood frequency estimation for ungauged catchments in Iceland by combined hydrological modeling and regional frequency analysis Philippe Crochet & Tinna /about-imo/publications/2014/
  • 4. 2010_005_

    Century control runs, as well as 21st Century forecast runs, submitted by various institutions to the Intergovernmental Panel on Climate Change (IPCC) for their Forth 11 Table 1. General circulation and regional climate models that were considered in this study. Model Version Model Name, Institute BCCR BCM 2.0 Bergen Climate Model, Bjerknes Centre for Climate Research, Bergen, Norway CCCMA CGCM 3.1 /media/ces/2010_005_.pdf
  • 5. 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 fá upplýsingar um ísinn sem hann er sigla í gegnum /media/hafis/skyrslur_lhg/isskyrsla_14122010.pdf
  • 6. norsem_mantyniemi

    The standard practice in Finland is to conduct macroseismic questionnaire surveys remotely. However, observations have occasionally been collected at interviews and questionnaires distributed during field trips, mainly in the 1900s. No networks of permanent correspondents have been arranged in Finland for the purpose of macroseismic surveys, so respondents have to be found in the affected area /media/norsem/norsem_mantyniemi.pdf
  • 7. VI_2009_006_tt

    lake in a volcanic caldera in the interior of the Vatnajökull ice cap (Björns- son, 1988). Jökulhlaups from Grímsvötn have been known since at least the fourteenth century (Þórarinsson, 1939, 1974). In the beginning of the twentieth century there were about ten years between outbursts but the floods diminished with time and became more frequent. After a catastrophic, rapidly rising flood caused /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
  • 8. Eriksson_2-Acceptability-of-policy

    (Stern, 2002) 4 5 (1) Concepts • Acceptability - attitude toward policy (e.g., Schade, 2003). Salient beliefs attitudes (Eagly & Chaiken, 1993). • Acceptability (before implementation) versus acceptance (after implementation) (Gärling et al. 2008) • Attitude (acceptability/acceptance) versus behaviour (Eagly & Chaiken, 1993) (2) Factors important for acceptabilityAcceptability /media/loftslag/Eriksson_2-Acceptability-of-policy.pdf
  • 9. ces-oslo2010_proceedings

    change over the North Atlantic and in some simulations also for Iceland. In all areas, including the North Atlantic and Iceland, a clear climate change signal compared to the spread between the simulations is seen. The standard deviation calculated from 17 of the simulations are less than 1°C in all areas apart from Iceland where it reaches between 1 and 2°C and in parts of the Barents Sea where /media/ces/ces-oslo2010_proceedings.pdf
  • 10. IPPC-2007-ar4_syr

    Approximate CO2-eq concentrations corresponding to the computed radiative forcing due to anthropogenic GHGs and aerosols in 2100 (see p. 823 of the WGI TAR) for the SRES B1, AIT, B2, A1B, A2 and A1FI illustrative marker scenarios are about 600, 700, 800, 850, 1250 and 1550ppm, respectively. d) Temperature changes are expressed as the difference from the period 1980-1999. To express the change relative /media/loftslag/IPPC-2007-ar4_syr.pdf

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