41 results were found for 4100506(q)智通人才网外推代做路...petipt..ryb.

Results:

• 31. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  s fro m climat e ch ang e an d cr o ss bou ndar y adaptatio n measu res . In th e Netherl and s fo r hyd rodyna m ic mod el syst em s lik e SOB EK- W AQ UA (loca lleve l) an d e.g . fo rR hi ne flo w (ba sin wi de )c o n sid er ab le u n ce rta in tie s ex ist (W ee rts et al .200 3) D ev el op m en to fi nt eg ra te d ba sin m o de l( flo od ing an d poll ution) . 2: St at ist ic al /q ua lit /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 32. 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

• 33. VI_2009_012

  The medians of ratios from the broad-band digitizers (G24) are close to one, but the lowest median values are obtained at stations with short-period digitizers (RD3) in combination with either 1-Hz short-period (LE1) sensors, or broad-band (BB) sensors. The reason for the low ratios in the LE1-RD3 combination is obviously failure to retrieve all the low frequency amplitude through instrument /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.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. 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

• 36. 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

• 37. VI_2022_006_extreme

  77 91 109 Hraunaveita 132 116 136 159 117 140 169 Kvíslaveita 48 42 49 58 42 51 61 Sultartangi 66 57 68 80 58 69 84 Þingvallavatn 96 84 99 117 85 102 123 Þórisvatn 47 41 49 57 42 50 60 Tungnaá 76 67 79 92 67 80 98 Ufsarlón 104 92 108 126 93 112 134 36 Figure 19 – 1M5 maps for catchment Hálslón based on the ICRA dataset without projection (top left), with RCP 2.6 and 10th percentile /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 38. 2010_012rs

  and dips 89°. The strike deviates only 4° from the strike defined by the relocated aftershock distribution on the Ingólfsfjall fault, which shows an 11 km long and an 8 km deep fault, striking N181°E and dipping 89°. The mechanism of the earthquake on the Ingólfsfjall fault could therefore have been immediately inferred. However, there were only three foreshocks 25 on the (second) Kross fault /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 39. VI_2020_011_en

  : Yfirfarið af: SG Lykilsíða 5 Contents ABSTRACT .............................................................................................................................. 8 1 INTRODUCTION ............................................................................................................... 9 1.1 Long-term volcanic hazard assessment /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 40. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf