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Results:

• 1. VI_2014_006

  the com- plexity of the hydrological processes through modelling, but its application is usually limited to the short-range. Although the results demonstrated a great potential for this method, its success- ful application in real-time will strongly depend on the quality and availability of streamflow observations, which can be poor or simply missing during periods of variable durations, e.g /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 2. VI_2013_008

  of these two gradients in the south–north direction (l = i) and west–east direction (l = j). The best analogue with respect to the shape of the MSLP field at time t is the MSLP field at time u that minimizes S1. This score has been used by e.g. Obled et al. (2002), Wetterhall et al. (2005) and Marty et al. (2012) with either MSLP or geopotential height, to forecast precipitation. It was also applied /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 3. VI_2015_007

  M A M J J A l l l l l l l l l l l l l 0 100 200 300 30 0 50 0 70 0 Day since 1st Sept. Q m³ /s VHM 265 S O N D J F M A M J J A l l l l l l l l l l l 0 100 200 300 20 0 30 0 40 0 50 0 Day since 1st Sept. Q m³ /s VHM 277 S O N D J F M A M J J A l l l l l l l l l l l 0 100 200 300 10 20 30 40 50 Day since 1st Sept. Q m³ /s VHM 278 S O N D J F M A M J J A Figure 2. Time of occurrence of the annual /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 4. VI_2015_009

  estimates are obtained for catchments where bµ(D) is most biased, e.g. vhm116. l l l l l l l l l l l l l l l l l l l l l l l l 5 10 15 20 40 60 80 10 0 12 0 14 0 IFM no. % Figure 4. Estimated instantaneous flood quantiles with the IFM, at gauged sites treated as ungauged. Mean relative quantile RMSE (RMSET ) for the different index flood models. Large symbol corresponds to the model giving the best /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 5. VI_2014_001

  (RMSET ) (top) and bias (BIAST ) (bottom) for Region 1. The solid blue and red lines correspond to results ob- tained with the index flood method developed with WaSiM simulations within catchments vhm51 and vhm52, respectively. Best model with respect to RMSET is indicated by large symbol. l l l l l l 1 2 3 4 5 6 0 10 20 30 40 50 hn? ????m?el qM S? T (? l l l l l l Mean relative RMSE for daily /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 6. 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

• 7. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  in objectives and in our risk willingness to accept a lower reliability for supply of clean drinking water without causing adverse environmental effects. These measures could have major impacts on environment and agriculture. Similarly, the envisaged adaptation with respect to roads include both structural and non-structural measures such as new designs, real-time flood Fig. 4 Probability of mean N /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 8. IMO_AnnualReport2014

  and obtain the most recent information on the ongoing events: the eruption status, possible hazards and likely scenarios. Earthquake and cGPS data processing enabled real-time monitoring of the rifting. At the start of the dyke intrusion, new updated models of the dyke volume were presented at these meetings near daily. The rapid growth of the dyke called for a quick response; additional seismic /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 9. IPPC-2007-ar4_syr

  Core Writing Team Lenny Bernstein, Peter Bosch, Osvaldo Canziani, Zhenlin Chen, Renate Christ, Ogunlade Davidson, William Hare, Saleemul Huq, David Karoly, Vladimir Kattsov, Zbigniew Kundzewicz, Jian Liu, Ulrike Lohmann, Martin Manning, Taroh Matsuno, Bettina Menne, Bert Metz, Monirul Mirza, Neville Nicholls, Leonard Nurse, Rajendra Pachauri, Jean Palutikof, Martin Parry, Dahe Qin, Nijavalli /media/loftslag/IPPC-2007-ar4_syr.pdf

• 10. VI_2020_005

  to a theoretical mean sea level calculated from annual means where uplift and sea level rise have been taken into account (SMHI, 2016). Not only real-time and historical sea level data can be downloaded from the SMHI website, but also ocean temperature-, wave-, current-, vertical profile chemistry-, marine biology- and marine weather data can be found there. The UK National Tide Gauge Network /media/vedurstofan-utgafa-2020/VI_2020_005.pdf