32 results were found for 足球欧洲杯⒛⒚赛程时间表_50⒔4.com竞彩足球比分直播—竞彩258网.

Results:

• 11. 2005EO260001

  lake within the caldera until the surrounding ice is breached. When that happens, water escapes to cause a jökulhlaup in the river Skeidará, after having traveled ~50 km beneath the Skeidarárjökull outlet glacier (Figure 1b). Jökulhlaups occur there every 1–10 years and last from days to weeks, each time releasing 0.4–4 km3 of water [Björnsson, 2002]. Volcanic eruptions in Gríms- vötn often /media/jar/myndsafn/2005EO260001.pdf

• 12. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 13. Daniell_etal-2010

  Copyright © 2010 by the author(s). Published here under license by the Resilience Alliance. Moellenkamp, S., M. Lamers, C. Huesmann, S. Rotter, C. Pahl-Wostl, K. Speil, and W. Pohl. 2010. Informal participatory platforms for adaptive management. insights into niche-finding, collaborative design and outcomes from a participatory process in the rhine basin. Ecology and Society 15(4): 41. [online /media/loftslag/Daniell_etal-2010.pdf

• 14. vanRoosmalen_etal-2009-WRR_2007WR006760

  have a consider- able impact in an area where surface runoff is the dominant process, but have a smaller impact on groundwater-fed systems. Owing to the heterogeneity of the meteorological conditions and the heterogeneous physiographical condi- tions, climate and land use change impact studies on hydrology often have a local to regional character. [4] The majority of hydrological climate change /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 15. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 16. Observations - Borgarhöfn

  Observations - Borgarhöfn | Observations | Icelandic Meteorological office Observations - Borgarhöfn Mon 1.05 14 GMT 5.7° S 4 Max wind : 4 / 6 13 GMT 6.4° S 4 Max wind : 4 / 6 12 GMT 5.4° S 3 Max wind : 4 / 6 11 GMT 4.7° S 4 Max wind : 4 / 6 10 GMT 4.8° SE 3 Max wind : 3 / 4 09 GMT /m/observations/areas

• 17. 2010_005_

  Björnsson, Icelandic Meteorological Office   Contents 1 Introduction 9 2 Data and Methodology 11 3 Spatial Variability of Climate Trends 13 3.1 Surface Air Temperature . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 13 3.2 Total Precipitation . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 15 4 Long-Term Trends of Annual Mean Values 16 4.1 Surface Air /media/ces/2010_005_.pdf

• 18. VI_2015_009

  4 Contents 1 Introduction ................................................................................................ 7 2 Study area and data ..................................................................................... 7 2.1 River basins .......................................................................................... 7 2.2 Streamflow data /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 19. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  2007a, b). BNs were tested in a recent EU research project MERIT (Bromley, 2005; www.merit- eu.net) 2001–2004, and this tool is currently considered in Uncer wate NeWa an tainty is a central theme in integrated and adaptive r management, where different disciplines need to be Monitor and evaluate outcomes; apply learning to develop a better understanding of the system. (4) Implement policies;(3 /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 20. VI_2014_005

  , Veðurstofu Íslands   Contents 1 Introduction ................................................................................................ 7 2 Model setup and data ................................................................................... 7 3 Model terrain and surface type ...................................................................... 9 4 Impact of initial conditions in blending /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf