85 results were found for x 도지코인거래「wwwͺbybͺpw」 도지코인매매 도지코인투자☊도지코인리딩㋈자연과환경 ska.

Results:

• 31. Gradual fading of seismic activity at Bárðarbunga and the dyke intrusion

  with the general observation of a slowly fading activity in almost all other data sets. Inter-event waiting time For the Bárðarbunga caldera, inter-event waiting time for earthquakes equal to or larger than M5 has been plotted* during the four months period from the onset of events until 15 Dec 2014. On the y-axis, waiting time is given in hours. The x-axis shows the relevant earthquakes /earthquakes-and-volcanism/articles/nr/3039

• 32. Group5-Stakeholders_involvement

  - m a k e r P u b l i c S t ron g Go v ernanc e I n s u re r s Pri v a t e S t ron g M ar k e t S c ie n t i f i c e x per t s ( g eo s c ie n c e s , e c o n o m i c s , s o c iolog y , p s y c hol o g y ) Publi c / pri v a t e - - I nd u s t ri e s Pri v a t e S t ron g M ar k e t W a t e r s upplie r P u b l i c S t ron g M ar k e t F ar m er s /media/loftslag/Group5-Stakeholders_involvement.pdf

• 33. Group-1_Scenarios-for-AWM

  i on c a p ac i t y A r ea of r e s i d en c e (Flood p r one /non p r one a r eas) Un c e r t a n t i e s H i g h wi l l i n g n e s s t o p a y L o w wi l l i n g nes to pay D i k e s H i gh t a x a t i on - E arly w arn i n g s y s t e m s - Sof t s t r uct u r a l m e as u r e s -Community training L o w taxation Risk P e r c e p t i o n B e n e f i /media/loftslag/Group-1_Scenarios-for-AWM.pdf

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

  aversion should influence the first mover’s decision. The 98 Public Choice (2012) 151:91–119 Fi g. 1 O pt im al co n tr ib u tio n de pe nd in g o n α , r an d p Public Choice (2012) 151:91–119 99 Table 1 The predicted effect of intrinsic preferences on first and second movers’ contributions 1st mover 2nd mover Disadvantageous Negative None inequity aversion Advantageous None Positive inequity /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 35. ces-glacier-scaling-memo2009-01

  of melt water from glaciated areas in long integrations for a warming climate. Glacier dynamics This problem can be qualitatively analysed by considering the continuity equation for ice vol- ume, which may be expressed as ¶h ¶t + ¶q ¶x = b or ¶h ¶t +~ ~q = b ; (1) for a one-dimensional ice flow channel or an ice cap that flows in two horizontal dimensions, respectively. h is ice thickness, q or ~q /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 36. 2013_001_Nawri_et_al

  the Fljótsdalsheiði region . . . . . . . 47 18 Seasonal mean wind power density within the Fljótsdalsheiði region . . . . . . . . 48 19 Directional mean wind power density within the Gufuskálar region . . . . . . . . . 49 20 Seasonal mean wind power density within the Gufuskálar region . . . . . . . . . . 50 21 Directional mean wind power density within the Hellisheiði region . . . . . . . . . 51 22 Seasonal mean /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 37. CES_D2.4_task1

  was observed in 1961-2008 (80% vs. 61%), whereas the difference in January is only 9% (71% vs. 62%). In absolute terms, however, the projected warming is larger in January than in April. Note that Fig. 3.1 hides the latter difference, because the horizontal axis is scaled according to the range of interannual variability. x The two observation-based distributions (1961-1990 and 1961-2008) differ /media/ces/CES_D2.4_task1.pdf

• 38. VI_2017_009

  we take the corresponding data from the CMIP5 project. Table 1. All GCMs and RCMs used in this study. If a model is available for any of the domains Arctic-44, EURO-44, or EURO-11, it is marked with a v, but with an x if it is unavailable. Model name Type EURO-11 EURO-44 Arctic-44 CCCma-CanESM2 GCM x v v COSMO-CLM4-8-17 RCM v v x CNRM-CERFACS-CNRM-CM5 GCM v v x IHCEC-EC-Earth GCM v v v /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 39. VI_2020_004

  & Höskuldsson, 2008; Thordarson & Larsen, 2007). Highly active volcanic systems as Hekla, Katla, Bárðarbunga and Grímsvötn, have explosive eruptions rates of 82%, 97%, 90% and 95%, respectively (Gudmundsson & Larsen, 2016; Larsen & Gudmundsson, 2016b, 2016a; Larsen & Thordarson, 2016). Volcanic eruptions are quite common in Iceland and occur on average every two to five years (Larsen & Eiríksson /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 40. VI_2009_006_tt

  was therefore formed by ice lifting and deformation induced by subglacial water pressures higher than ice overburden pressure. The discharge data and the derived size of the subglacial flood path, as indicated by the volume of water stored subglacially, indicates a development towards more efficient subglacial flow over the course of the jökulhlaup. Thus, a discharge in the iii range 80–90 m3 s 1 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf