72 results were found for 菲律宾圣安娜假盘菲律宾圣安娜假线【191-1999-2299】圣noiw安Fc2kG.

Results:

• 41. Traffc-maintenance_expenditures

  847 2) 59 650 88 048 4) 20 165 9 582 - 8 110 161 728 322 974 636 1 244 770 2002 .. 633 847 2) 54 354 81 892 4) 19 329 9 071 - 4 853 162 705 163 966 014 1 260 860 2001 .. 542 806 2) 81 295 50 734 4) 19 889 9 000 - 5 690 141 203 48 850 666 1 132 021 2000 .. 533 629 2) 125 273 32 157 4) 23 190 6 997 - 5 332 115 674 197 842 483 1 149 476 1999 .. 526 558 2) 141 789 8 744 4) 26 555 6 463 14 403 2 827 109 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 42. Bardarbunga_kafli20140825

  but triggered by and occurring simultaneously with eruptions on the Bárðarbunga system (yellow) are least frequent (e.g. McGarvie et al. 1990). Effusive basaltic eruptions (red) on the ice-free part of the volcanic system include the largest eruptions on the system (e.g. Jakobsson 1979; Vilmundardóttir et al. 1988, 1990, 1999, 2000; Sigvaldason 1992; Hjartarson 2011). 5 Figure 3. Proportion /media/jar/Bardarbunga_kafli20140825.pdf

• 43. Keskitalo_et_al-MLG_and_adaptation_FINAL

  experienced by different localities. The concept of multi-level governance helps to highlight this interrelation between levels by demonstrating that the steering of decision-making is no longer a function of government only, but of a broader array of actors and levels (Boland 1999; Hooghe and Marks 2003). The multi-level governance concept has been developed out of literature that shows /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 44. VI_2014_006

  method. Analogue-based methods have been used in weather forecasting (Radinovic´, 1975; Kruizinga & Murphy, 1983; Van den Dool, 1989; Fraedrich et al., 2003) and climate downscaling (Zorita & Von Storch, 1999; Wetterhall et al., 2005) to extract local weather infor- mation, which can not be simulated by coarse-resolution NWP or climate models with sufficient accuracy. In the past decade /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 45. vanRoosmalen_etal-2009-WRR_2007WR006760

  of climate change on hydrological systems in Europe [e.g., Andre´asson et al., 2004; Arnell, 1999; Caballero et al., 2007; Graham et al., 2007b; Kleinn et al., 2005; Thodsen, 2007]. Generally, the simulated impacts of climate change vary considerably as a result of contrasting climate change signals in northern and southern Europe, e.g., an increase in annual precipitation in the north /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 46. GA_2009_91A_4_Andreassen

  in southern Norway (Fig.1). The glacier has a total area of 5.4 km2 and rangesin altitude from 1390 to 2090 m a.s.l. The glacierhas been mapped repeatedly, the most recent mapis from 1997. Areas calculated from the 1951 and1997 maps reveal an area reduction of about 0.4km2 in this period (Andreassen 1999). Lengthchange observations reveal a net retreat of about 60 m from 1997 to 2006 (data: NVE; e.g /media/ces/GA_2009_91A_4_Andreassen.pdf

• 47. NOMEK09_Report

  ) for the Baltic participants and/or other participants from member states are covered by EUMETSAT. The NOMEK courses so far: 1. Oslo 1995 2. Helsinki 1996 3. Copenhagen 1997 4. Norrköping 1998 5. Tromsö 1999 6. Helsinki 2000 7. Vilnius 2001 8. Copenhagen 2002 NOMEK 2009 11-15 May, Reykjavík, Iceland 9. Norrköping 2003 10. Reykjavik 2004 11. Oslo 2005 12. Helsinki 2006 13. Denmark 2007 14. Sweden 2008 15 /media/vedurstofan/utgafa/skyrslur/2009/NOMEK09_Report.pdf

• 48. Moellenkampetal_etal-2010

  research” (Hatchuel and Molet 1986, Hatchuel 1994, Berry 1995, Checkland and Holwell 1998, Flood 1998, Avenier et al. 1999, David 2000, Midgley 2000). However, in-depth analyses and evaluation of the interventions also make the research approach a hybrid of intervention research with case-study based research (Yin 2003). Intervention research is considered by Midgley (2000) as “purposeful action /media/loftslag/Moellenkampetal_etal-2010.pdf

• 49. VI_2009_012

  susceptible to damage. The goals in SAFER include installation of real-time aftershock hazard mapping (Gerstenberger et al., 2005) and ShakeMap (Wald et al., 1999) for SW Iceland. These can enable fast estimation of seismic hazard and potential damage after an earthquake, which can be of great value for disaster management. Necessary support for the generation of such maps is the development /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 50. 2010_003rs

  (Rögnvaldsson et al., 1998a), in the Hengill area (Rögnvaldsson et al., 1999; Vogfjörð, 2000; Vogfjörd et al., 2005a), in the western volcanic zone (Hjaltadóttir and Vogfjörð, 2009) and on the Reykjanes Peninsula (Hjaltadóttir and Vogfjörð, 2006). A detailed map of sub-surface faults with slip directions can be of great value for stress-field evaluation in the seismic zone. It is also of great /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf