74 results were found for 【77AGG.COM】slot gacor-lpo88 apk hoki time slot free bet slot slot gacor homebet88 dy2.

Results:

• 41. Refsgaard_etal-2007-Uncertainty-EMS

  in the outcome (mainly to save computation time). A number of commercial and free software packages are available to do Monte Carlo analysis, e.g. Crystal Ball (2000) and @risk (Palisade Corporation, 2000) and SimLab (Saltelli et al., 2004). In addition Monte Carlo functionality is built into many modelling software packages. EPA (1997) provides a good guidance for use of Monte Carlo analysis /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 42. Daniell_etal-2010

  pressure from existing regimes. Although this definition is influenced by the literature on transition management (e.g., Geels 2002, Raven et al. 2007), we use the term in a broader sense, considering it as a place and time for learning and experimentation. Secondly, we discuss how a process can be adaptively co-designed by water management practitioners, researchers, and consultants. We consider /media/loftslag/Daniell_etal-2010.pdf

• 43. Bárðarbunga 2014 - December events

  of activity in Bárðarbunga in mid-August. 16 December 2014 - analysis of activity during the first 4 months Today, there are four months since the onset of the Bárðarbunga seismic events. Preliminary analysis of the decrease of seismic moment release and numbers of events with time has been done (see link). The situation is quite evident for the dyke intrusion (upper panels): The highest /earthquakes-and-volcanism/articles/nr/3055

• 44. Bárðarbunga 2014 - December events

  of activity in Bárðarbunga in mid-August. 16 December 2014 - analysis of activity during the first 4 months Today, there are four months since the onset of the Bárðarbunga seismic events. Preliminary analysis of the decrease of seismic moment release and numbers of events with time has been done (see link). The situation is quite evident for the dyke intrusion (upper panels): The highest /earthquakes-and-volcanism/articles/nr/3055/

• 45. Bardarbunga-2014_December-events

  quakes were observed north of Tungnafellsjökull, the largest M2.5. This area has been quite active since the onset of activity in Bárðarbunga in mid-August. 16 December 2014 - analysis of activity during the first 4 months Today, there are four months since the onset of the Bárðarbunga seismic events. Preliminary analysis of the decrease of seismic moment release and numbers of events with time /media/jar/Bardarbunga-2014_December-events.pdf

• 46. VI_2009_012

  global change and ecosystem priority 6.3.iv.2.1: reduction of seismic risks D5.2 Improve PGA- and VGA-distance relations, determine long-term background seismic hazard estimate and derive clustering properties (space-time-magnitude) for SW Iceland. 6 SAFER Rannsóknaverkefnið Í Evrópusamstarfsverkefninu SAFER (Seismic eArly warning For EuRope) var unnið að rannsóknum og þróun á /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 47. Cooperation is a must for adaptation to and

  the long-term background warming. Mild and snow-free conditions in winters will reduce the number of extreme cold events. For summers more heat waves and droughts may be expected as a result of a longer season with high temperatures in combination with relatively small increases, or even regional decreases, in precipitation. Other, more uncertain impacts on the large-scale circulation /about-imo/news/cooperation-is-a-must-for-adaptation-to-and-mitigation-of-climate-change

• 48. The weather in Iceland in 2016

  heavy precipitation for a period in the South and West, the monthly totals were record high at a few stations. The month was totally frost-free in most coastal areas, which is unusual. NovemberThe month was a warm one with heavy precipitation and the weather was favourable but dark and gloomy. DecemberThe warm weather continued until just before Christmas, in the East this was the warmest /about-imo/news/the-weather-in-iceland-in-2016

• 49. Glacial outburst floods

  from ice-dammed marginal lakes. Such lakes often form when an outlet glacier closes off an ice-free side valley. Grænalón is an Icelandic example of such a lake.Jökulhlaups from supraglacial lakes which have formed by accumulation of meltwater in depressions on the surface of the glacier. Such floods are generally small in Iceland but can be of substantial magnitude on the Greenland ice /volcanoes/volcanic-hazards/glacial-outburst/

• 50. Eriksson_2-Acceptability-of-policy

  and the collective • Why doesn’t everybody cooperate? Low response efficacy, “sucker effect”, free riders 3 (1) Environmental policy measures • Structural versus psychological solutions (Vlek, 1996) • Legal policies, economic policies, measures changing the physical context and informational/educational measures (Steg, 2003) • Targeting technological solutions versus curtailment behaviour /media/loftslag/Eriksson_2-Acceptability-of-policy.pdf