85 results were found for X 홈타이△ㄲr톡 gttg5△苄신봉동오전출장魁신봉동오후출장㷕신봉동외국녀출장신봉동외국인여성출장🚆periodically/.

Results:

• 31. Hare-2011-ParticipatoryModelling

  stage )Suppor t an d ski lls n ee de d Har e et a l. (2003 ) X X An aly se lin ks be tw ee n participator y structur e an d proces s implementatio n Ba rr et ea u et a l. (2010 ) X X X Pr o vid e cle ar de sc rip tio n o fproces s (m an ag e ex pe ct at io n s); monitorin g an d evaluatio n Bot s an d va n Daale n (2008 ) X X X X X Su pp o rt pr o ce ss de sig n Ad ap te d fra m ew o rk u se d in th /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 32. 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

• 33. 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

• 34. 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

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

  + x−k) (1) Public Choice (2012) 151:91–119 95 with k = 1,2, and −k = 1 if k = 2, −k = 2 if k = 1. The variables xik and x−k are the contributions to the public good of subject i as mover k and mover −k, respectively. The contribution of the first mover is an integer x1 ∈ [0,10] and that of the second mover takes one of the two values x2 ∈ {0, x1}. 2.2 Theoretical predictions As noted /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 36. 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

• 37. 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

• 38. CES_D2.4_task1

  about 20-25% in 2010 to about 50% in 2050. Perhaps surprisingly, a particularly high probability is found in Iceland, most likely as a result of the small 12 interannual variability there. As expected, the probability of very warn years rises even faster than that of warm months – in northern Europe from typically 30-40% in 2010 to about 60- 80% in 2030 and to 85-95% or even more in 2050 /media/ces/CES_D2.4_task1.pdf

• 39. VI_2017_009

  % 20% Langjökull 42% 81% 21% Mýrdalsjökull 38% 74% 17% Reykjavík 23% 45% 4% Vatnajökull 89% 98% 47% 2081–2100 RCP4.5 Akureyri 25% 52% 11% Langjökull 28% 61% 10% Mýrdalsjökull 23% 49% 13% Reykjavík 15% 24% 1% Vatnajökull 70% 81% 22% 2081–2100 RCP8.5 Akureyri 17% 41% 5% Langjökull 21% 43% 5% Mýrdalsjökull 18% 40% 7% Reykjavík 11% 19% 0.5% Vatnajökull 65% 75% 18% 4.2 Precipitation /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 40. VI_2009_006_tt

  236 1992 09 167 124 167 98 1995 07 1994 1759 599 368 1995 10 96 62 73 37 1997 07 921 728 330 184 2000 08 1240 1083 365 221 2002 09 689 582 267 160 2003 11 241 207 139 98 2006 04 1370 1340 300 270 2008 10 1350 1290 300 265 The origin of the 1957, 1960, 1964 and 1966 jökulhlaups is not certain but is most likely the eastern cauldron. The discharge and volume for the 1995 jökulhlaup are a sum from /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf