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• 41. Observations - Húsafell

  GMT -1.1° NE 3 Max wind : 4 / 6 Sun 30.04 23 GMT -1.0° NE 4 Max wind : 5 / 10 22 GMT -0.7° NNE 5 Max wind : 5 / 9 21 GMT -0.5° NNE 5 Max wind : 6 / 10 20 GMT 0.9° NNE 5 Max wind : 6 / 10 19 GMT 2.6° NNE 5 Max wind : 6 / 11 18 GMT 3.9° NNE 6 Max wind : 6 / 12 17 GMT 4.8° NNE 5 Max wind : 5 / 10 16 GMT 4.6° NNE 5 Max wind /m/observations/areas

• 42. 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

• 43. Kok_2-scenarios-lecture-2

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

• 44. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

  on the mean of the 20 temperature change projections is modest in absolute terms, almost invariably less than 0.3°C (fourth column). The most notable features in the Nordic area include a slight increase in warming in western Norway, and a slight decrease in warming in northeastern Fennoscandia. Figure 4.2. As Figure 4.1, but for the standard deviation of temperature change (unit: °C). The last /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf

• 45. Kriauciuniene_Jurate_CES_2010

  of temperature anomaly (ºC) between 1991-2007 and 1961-1990 Variation of annual T anomaly (ºC) between 1991-2007 and 1961-1990 Seasonal differences of P anomaly (in %) between 1991-2007 and 1961-1990 Seasonal differences of Q anomaly (in %) between 1991-2007 and 1961-1990 Variation of annual P and Q anomaly (%) between 1991-2007 and 1961-1990 -40 -25 -10 5 20 35 50 1 9 2 0 1 9 4 0 1 9 6 /media/ces/Kriauciuniene_Jurate_CES_2010.pdf

• 46. ces_geus_paakitsoq_full_report

  conditions as a lower boundary condition from the driving GCM. The RCAO model-output is from a pan-arctic run for the years 1960–2080 at approx. 50 km resolution. The first 20 years of the model run must be considered as spin-up time for the ocean module. The RCAO run is experimental since the model is in a development state and the output has not yet been evaluated over Greenland (Ralf Döscher, personal /media/ces/ces_geus_paakitsoq_full_report.pdf

• 47. Demers_Claude_CES_2010

  /media/ces/Demers_Claude_CES_2010.pdf

• 48. VI_2017_009

  % 20% Langjökull 42% 81% 21% Mýrdalsjökull 38% 74% 17% Reykjavík 23% 45% 4% Vatnajökull 89% 98% 47% 2081–2100 RCP4.5 Akureyri 25% 52% 11% Langjökull 28% 61% 10% Mýrdalsjökull 23% 49% 13% Reykjavík 15% 24% 1% Vatnajökull 70% 81% 22% 2081–2100 RCP8.5 Akureyri 17% 41% 5% Langjökull 21% 43% 5% Mýrdalsjökull 18% 40% 7% Reykjavík 11% 19% 0.5% Vatnajökull 65% 75% 18% 4.2 Precipitation /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 49. Wind Energy

  ) Clausen, N-E. (2008). Et bud på fremtidens vindkraft-med vægt på landbaseret vind. Vind-workshop om arealplanlægning på Örenäs Slott 26.-27. nov. 2008. Pryor S.C. (2009): Wind climates: Variability and change. AWEA Fall conference on wind resource estimation. Orlando, Florida, 18-20 November 2009. Pryor S.C. (2009): Extreme and intense winds. Presentation at Workshop on Climate Scenarios 13 /ces/publications/nr/1944

• 50. Kok_JGEC658_2009

  after 20–30 iterations, although total stabilisation can take more than 100 iterations. Fig. 2 shows two directed graphs of the Fuzzy Cognitive Map and the development of the values of state vector A for the first 30 iterations. The right-hand side graph has one additional relationship e23 = 0.5. 2.5. Interpretation of Fuzzy Cognitive Maps All input and output of a Fuzzy Cognitive Map is semi /media/loftslag/Kok_JGEC658_2009.pdf