91 results were found for Y アイリス〈ωωω,RTЗЗ,TOP〉コード:B77〉ミップスロット༿トラットfc🤞サッカートトサイト💛マカオベネシアン╜ソマリアの国家戦㍁パワーボールピクスター∿ジョージアサッカー␇プロトライブスコア∔.adq/.

Results:

• 51. 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

• 52. 2010_017

  ) [hours] kD (from hydro- graph) [hours] kI (opti- mized) [hours] kI (from hydro- graph) [hours] R2 R2log MPE annual [%] RMSE annual [m3/s] MPE daily [%] RMSE daily [m3/s] Austari- Jökulsá, vhm 144 Without g.w. module 81 20–50 5000 120–240 0.65 0.66 2.3 4.0 7.9 14.1 With g.w. module 50 20–50 150 120–240 0.68 0.75 5.5 3.7 9.1 13.6 Sandá í Þistilfirði /media/ces/2010_017.pdf

• 53. Paper-Olafur-Rognvaldsson_91

  The role of orography was found to be crucial in determining the precipitation dis- tribution and amount. Atmospheric flow over Iceland was simulated for the period January 1961 through June 2006 using version 3–7–3 of the PSU/NCAR MM5 mesoscale model (Grell et al., 1995). The domain used is 123× 95 points, centered at 64◦ N and 19.5◦ W, with a horizontal resolution of 8 km. There are 23 vertical /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 54. 2010_003rs

  A (A1, A2, A3). ........................................................................................... 89 Figure B.2. Rake distribution for mapped faults/clusters in box B, Fagradalsfjall-W. ...... 90 Figure B.3. Rake distribution for mapped faults/clusters in box C, Fagdaralsfjall-E. ....... 90 Figure B.4. Rake distribution for mapped faults/clusters in box D, Kleifarvatn /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 55. 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

• 56. Eriksson_Garvill_Nordlund_2006

  (see e.g. Steg, 2003). In studies from several countries, push measures are perceived as less acceptable compared to pull measures (e.g. Ho¨lzer, 2003; Rienstra, Rietveld, & Verhoef, 1999; Steg & Vlek, 1997). For example, in a European study, over 90% of the car users supported improved public transport and park-and-ride schemes, while less than 20% approved of reduced parking space and cordon /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 57. Refsgaard_etal-2007-Uncertainty-EMS

  Discrete numerical Categorical Narrative Constant in space and time A1 A2 A3 4Varies in time, not in space B1 B2 B3 Varies in space, not in time C1 C2 C3 It is noticed that the matrix is in reality three-dimensional (source, type, nature). Thus, the categories type and nature are not mutually exclusive, and it may be argued that the ma- trix should be modified in such a way that the two uncer /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 58. 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

• 59. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  2.8090.60 2.9590.65 1.7090.30 1.4090.20 To 0 2.1090.35 2.3090.45 1.4090.20 1.2590.20 Ti B5 2.0590.35 2.2090.40 1.3590.20 1.2090.15 S. Gudmundsson et al. Mass balance of three ice caps in southern Iceland Citation: Polar Research 2011, 30, 7282, DOI: 10.3402/polar.v30i0.7282 7 (page number not for citation purpose) An AAR of 20
  25% is obtained for Eyjafjallajo¨kull (using the same 2004 /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 60. Bárðarbunga 2014 - December events

  ). The largest one, M4.1 occurred at 7:14, another, M4.0 at 18:11 and the third, M4.0 at 09:45 this morning. Ca 15 earthquakes between M3 and M4 were detected in Bárðarbunga. Yesterday evening at 23:18 an earthquake M4.4 was detected in the ocean, ca 20 km north of Kolbeinsey and some smaller followed. Similar pattern is common in the area. The lava almost 83 square kilometers? An overview map /earthquakes-and-volcanism/articles/nr/3055