41 results were found for ( q)1716160940在线标准北京时间校对排名代做贺...6hjlgw..83r.

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_

  Temperature . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 17 4.2 Total Precipitation . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 19 5 Seasonal Differences in Climate Trends 20 6 Conclusions 21 5 List of Figures 1 Mean annual surface air temperature during the 1961–90 control period, differ- ences in degrees between the control period and the 2021–50 reference /media/ces/2010_005_.pdf

• 33. VI_2009_012

  at the plate boundary, leading to volcanic activity and earthquakes. The geological units are shown on the map in Figure 1. The Western Volcanic Zone (WVZ) encompasses the part of the rift which enters land at the western tip of Reykjanes Peninsula (RP), runs east along the peninsula to the Hengill region, where it turns northward. East off the Hengill region the rifting shifts approximately 90 /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

  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

  towards the northern part of Vatnajökull. Table 8 – Median 1M5 values (mm 24-h-1) for eleven hydropower catchments with and without climate projections for the period 2080 – 2100. Catchment 1M5 median value mm 24-h-1 Original RCP 2.6 RCP 8.5 10% 50% 90% 10% 50% 90% Blönduvirkjun 48 41 49 58 42 50 61 Búðarháls 46 40 47 56 40 48 59 Hágöngulón 63 55 65 76 55 66 81 Hálslón 85 75 88 104 /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

  ) and are Global Navigation Satellite System (GNSS) data providers (SONEL, n.d.). The North Sea is home to one of the most dense tide gauge networks in the world, with over 15 tide gauge series that span at least 100 years along its coastline (Quante and Colijn, 2016). In Denmark, 17 the national tide gauge network consists of 90 automatic stations run in cooperation of the Danish Meteorological /media/vedurstofan-utgafa-2020/VI_2020_005.pdf