41 results were found for ( q)4100506医美留痕代发廖...1tfllk..o49.

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_

  in the ENSEMBLES project. . . . . . . . . . . . . . . . . . . . . . . . . 37 16 Mean seasonal cycle during the 1961–90 control period, the 2021–50 reference period, and the 2070–99 reference period, for the IPCC ensemble mean, the SMHI- RCAO, the MetNo-HIRHAM, and the DMI-HIRHAM5. . . . . . . . . . . . . . . 38 17 Changes in the mean seasonal cycle from the 1961–90 control to the 2021–50 refer- ence /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

  Resources and Energy Directorate Edited by: Heidi H. Pikkarainen Print: Norwegian Water Resources and Energy Directorate Number printed: 130 Cover design: Rune Stubrud Prepared for: The CES project Norwegian Water Resources and Energy Directorate Middelthunsgate 29 P.O. Box 5091 Majorstua N-0301 OSLO NORWAY Telephone: +47 22 95 95 95 Fax: +47 22 95 90 00 /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

  and May. ............................................................................... 94 Figure B.8. Rake distribution for mapped faults/clusters in box H, Hengill, active between June and December. .......................................................................... 95 Figure B.9. Rake distribution for mapped faults/clusters in box I, Flói. ............................. 96 Figure B /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

  /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 39. VI_2020_011_en

  –8% likelihood that a vent will open on Heimaey. In other words, there is a 92–97% likelihood that the next eruption within the volcanic system will not be on Heimaey. The most densely populated parts of Heimaey in the north and around the harbor are the most vulnerable to Moderate and Large lava flows originating on the island. Almost all infrastructure on the island is vulnerable to lava /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 40. VI_2020_005

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