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Results:

• 71. Moellenkampetal_etal-2010

  supported by the majority of responses to one of the quantitative questions (to which 13 out of 20 participants responded on a five-point Likert scale—strongly agree, agree, neither agree or disagree, disagree, strongly disagree), where 11 respondents “agreed” that the activities in the workshop helped them to share their views and opinions with others, and the other two “neither agreed nor disagreed /media/loftslag/Moellenkampetal_etal-2010.pdf

• 72. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  The Rhine River Basin The Rhine basin (Fig. 3) covers an area of approximately 185,000 km2, distributed between nine countries. Two third of the basin is located in Germany, whereas the alpine countries of which Switzerland is the most important form 20% of the area (Buck et al. 1993). With its 1,320 km, of which 880 km is navigable, the Rhine is one of the longest rivers in Europe (Frijters /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 73. Horsens_case

  level coursed by tides is small with a range of less than 0.5 m. Figur 1. Horsens Fjord catchment. WFD main catchment area is 794 km2 NONAM Summerschool Copenhagen 22-26 August 2011 2 Physical features and ecosystem The fjord landscape is formed by glacial deposits. The average depth is 5 meters and the residence time of water in the fjord is about 20 days. As to tidal variations /media/loftslag/Horsens_case.pdf

• 74. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  more uncertain than the changes in temperature. The 5th percentile of annual mean precipitation change is positive in northern Russia, Finland and large parts of Sweden; elsewhere, it is generally negative. Conversely, the 95th percentile is in the range 10-20%. The uncertainty in seasonal mean precipitation changes is larger than that of the annual mean change. In particular, the 5-95% range /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 75. Station forecasts, text forecasts or observations

  /about-imo/the-web/iframes/wst-txt-obs/

• 76. aerodrome_summaries_20140603

  AERODROME CLIMATOLOGICAL SUMMARY: BIEG - TABLE A..................... 20 AERODROME CLIMATOLOGICAL SUMMARY: BIEG - TABLE B ..................... 21 AERODROME CLIMATOLOGICAL SUMMARY: BIEG - TABLE C ..................... 22 AERODROME CLIMATOLOGICAL SUMMARY: BIEG - TABLE D..................... 24 AERODROME CLIMATOLOGICAL SUMMARY: BIEG - TABLE E ..................... 25 AERODROME CLIMATOLOGICAL /media/vedur/aerodrome_summaries_20140603.pdf

• 77. Adalgeirsdottir-etal-tc-5-961-2011

  Av. Ed. Belin, 31400 Toulouse, France Received: 21 March 2011 – Published in The Cryosphere Discuss.: 6 April 2011 Revised: 5 October 2011 – Accepted: 20 October 2011 – Published: 2 November 2011 Abstract. The Little Ice Age maximum extent of glaciers in Iceland was reached about 1890 AD and most glaciers in the country have retreated during the 20th century. A model for the surface mass balance /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 78. VI_2014_005

  ......................... 17 8 Monthly averages of SURFEX or projected 2-m air temperature ...................... 18 9 Local correction factors for 10-m wind speed ............................................... 19 10 Interpolated correction factors for 10-m wind speed ...................................... 20 11 Monthly averages of original or corrected temperature and wind speed .............. 21 12 /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 79. VI2010-006_web

  á við um aðrar veðurstöðvar innarlega í firðinum. Utar er úrkomuákefð norðanáttarinnar meiri. Eyjafjörður stýrir vindi í stefnu sína. Í ríkjandi norðaustan- og norðanáttum er vindátt á Akureyri því yfirleitt úr hánorðri eða af áttum vestan við norður. Langmestur hluti úrkomu á Ak- ureyri fellur þegar vindur er á milli 290◦ (um norður) yfir í 20◦ og ákefðin er mest þegar vindur blæs úr 330◦. Mikil /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 80. Kok_2-scenarios-lecture-2

  /media/loftslag/Kok_2-scenarios-lecture-2.pdf