59 results were found for 대방역타이녀출장♡O1O-4889-4785♡侸대방역타이마사지ᇚ대방역타이출장潈대방역태국녀출장㻙대방역태국마사지🚐considering/.

Results:

• 41. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  to a deep groundwater aquifer or to arrive at an abstraction well in a wellfield—does not fit into the ordinary ‘public common sense’ or ‘economic man way of thinking’. Economists sometimes calculate over a certain period of time e.g. 20 yr, but without considering lag time. G makes it clear that the calculation period should be much longer say 50–100 yr. The different groups (wetland people /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 42. Bárðarbunga 2014 - September events

  /earthquakes-and-volcanism/articles/nr/3001

• 43. Bardarbunga-2014_September-events

  /media/jar/Bardarbunga-2014_September-events.pdf

• 44. Bárðarbunga 2014 - September events

  /earthquakes-and-volcanism/articles/nr/3001/

• 45. Moellenkampetal_etal-2010

  /media/loftslag/Moellenkampetal_etal-2010.pdf

• 46. VI_2020_005

  By understanding the climate sensitivity, useful information and context for current and future sea level changes can be obtained (Church, Clark, et al., 2013; Quante and Colijn, 2016). When considering short term variability in relative sea level and especially extreme values, knowledge of historical events can be helpful. Written sources of the most dramatic events in the past can be used as indicators /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 47. VI_2013_008

  weather ob- served on these dates or some hours or days later. In the past decade in particular, this technique has been applied to produce probabilistic quantitative precipitation forecasts (PQPFs) (Obled et al., 2002; Hamill & Whitaker, 2006; Gibergans-Báguena & Llasat, 2007; Diomede et al., 2008; Panziera et al., 2011; Marty et al., 2012) considering that the coarse spatial resolution of NWP /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 48. GA_2009_91A_4_Andreassen

  and bs of 0.22–0.25 and0.24–0.28 m w.e. respectively in the period 1949–2006 are acceptable considering the uncertaintiesin both modelled and measured values. Althoughdiscrepancies occurred in some years, the mass bal- ance model was able to reproduce the main char-acteristics of annual and seasonal mass balance ofStorbreen. Close agreement between modelledmelt using a detailed energy balance model /media/ces/GA_2009_91A_4_Andreassen.pdf

• 49. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  are more uncertain than without considering climate change aspects, it is still important to include climate change uncertainties in the assessments now. An implementation strategy could be to design flexible action plans that can be modified, as more precise climate change predictions become available during the coming years. 5.3 Risk willingness differs among individuals and stakeholders /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 50. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  any errors that subjects make, and provides them with a logic of progression in the experiment. It may be asked whether this specific order of the games biases behavior in the sequential public good game. As subjects receive no feedback, 9Reciprocity is also found in trust games when considering the behavior of the second mover who decides how much of the amount received from the first mover /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf