49 results were found for 缅甸迪威国际开户【18O-8833-OOOO】国nbasz际Z.

Results:

• 31. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 32. 2011_005

  /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

• 33. Journal_of_Hydrology_Veijalainen_etal

  20 0 60 0 J F M A M J J A S O N D 0 20 0 60 0 J F M A M J J A S O N D 0 50 10 0 15 0 J F M A M J J A S O N D 0 50 10 0 15 0 J F M A M J J A S O N D 0 10 0 20 0 30 0 J F M A M J J A S O N D 0 10 0 20 0 30 0 J F M A M J J A S O N D 0 40 0 80 0 120 0 J F M A M J J A S O N D 0 40 0 80 0 120 0 J F M A M J J A S O N D 0 40 80 12 0 J F M A M J J A S O N D 0 40 80 12 0 J F M A M J J A S O N D /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 34. ces-oslo2010_proceedings

  Roald, L.A. and Engen-Skaugen, T. Projected effects of climate change on the hydrology of Norway ........................................................................ 80 Duncan, N.J., Harrison, G.P. and Wallace, A.R. Modelling the Scottish hydropower resource ........................................................................................................ 82 Einarsson, B /media/ces/ces-oslo2010_proceedings.pdf

• 35. 2010_016

  –5 months per year depending on watershed. Mean yearly maximum snow thickness decreases by 0–80%. Winter flow is predicted to increase on average due to a higher number of melt events at relatively high and flat heath areas of the watersheds. For Sandá í Þistilfirði, vhm 26, the snowmelt generated spring/summer discharge peak largely disappears and the seasonal discharge becomes more evenly /media/ces/2010_016.pdf

• 36. VI_2015_007

  ] m ³/s l l l l l l l l l l l l l l l l l l l l l l E[Q(D=0)] vhm148 l l REF IFM−ROI IFM−CLU l IFM−WaSiM l l l l l l l l l l l l 2 4 6 8 10 12 20 0 40 0 60 0 80 0 IFM no. E[ Q] m ³/s l l l l l l l l l l l l l l l l l l l l l l l E[Q(D=0)] vhm149 l l REF IFM−ROI IFM−CLU l IFM−WaSiM l l l l l l l l l l l l 2 4 6 8 10 12 20 0 40 0 60 0 80 0 IFM no. E[ Q] m ³/s l l l l l l l l l l l l l l l l l l l l /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 37. VI_2014_006

  /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 38. 2010_003rs

  við strik sprungunnar í heild, en þó er hún samhangandi við botninn. Hestvatnssprungan er einnig nær lóðrétt og um 15,5 km löng og með strikstefnu N179°A. Hún er ólík Holtasprungunni að því leyti að hún dýpkar til suðurs, úr 6 í 9 km en jafnframt virðist hún mynduð úr tveimur mishallandi flötum. Rétt sunnan skjálftamiðjunnar er sprungan nær lóðrétt (88° halli) en norðan upptakanna hallar /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 39. 2010_005_

  A conservative enhancement of the reduced IPCC ensemble mean warming rate would therefore result in 0.37 K per decade for the Icelandic elevated terrain. 17 Table 4. Linear trends of surface air temperature in Kelvin per decade between specific years in different zones (ocean / land / low terrain / high terrain). 2004–50 2004–80 2004–99 IPCC GCM Mean 0.30 / 0.31 / - / - 0.28 / 0.29 / - / - 0.23 / 0.24 /media/ces/2010_005_.pdf

• 40. VI_2015_005

  is on the northern North Atlantic and the Nordic Seas. With the southern boundary at 47 N, the study domain covers Newfoundland, but excludes various marginal and inland seas with significant independent storm activity, such as the Mediterranean and Adriatic Seas, as well as the Black and Caspian Seas. The northern boundary at 80 N takes the domain up to Fram Strait, including Svalbard, but excluding /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf