41 results were found for 首商网外推排名495455411(Q)冯...ecr7ni..fnz.

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_

  are the shorter-term TP trends, which are significant on the 95% confidence level. Over the longer periods, linear TP trends over the ocean are robust with respect to changing beginning and end years. Over the land, there is a 10% difference between trends with either specific or randomised beginning and end years. Additionally, the tabulated values of TP differences between the 1961–90 control period /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

  /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 36. 2010_003rs

  ................ 91 Figure B.5. Rake distribution for mapped faults/clusters in boxes E and F, Brennisteinsfjöll-Bláfjöll. ................................................................................. 92 Figure B.6. Rake distribution for mapped faults/clusters in box G, Ölfus. ......................... 93 Figure B.7. Rake distribution for mapped faults/clusters in box H, Hengill, active between January /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

  : 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

  ) 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