84 results were found for X 홈타이{ㄲr톡 gttg5}新원미구아로마출장烆원미구아로마테라피訮원미구아줌마출장骶원미구알바녀출장📞evasively/.

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

  + 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

• 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

  approximately centred around Iceland: the outer domain with 43 42 grid points spaced at 27 km (1134 1107 km), the intermediate domain with 95 90 grid points spaced at 9 km, and the inner domain with 196 148 grid points spaced at 3 km. The northwest corner of the outer domain covers a part of the southeast coastal region of Greenland. Otherwise, the only landmass included in the model domain /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 37. 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

• 38. VI_2017_009

  11 / 12 MPI-ESM-LR REMO2009 45 / 85 13 / 14 IHCEC-EC-Earth RCA4 45 / 85 15 / 16 IHCEC-EC-Earth COSMO-CLM4-8-17 45 / 85 17 / 18 CNRM-CERFACS-CM5 RCA4 45 / 85 19 / 20 CNRM-CERFACS-CM5 COSMO-CLM4-8-17 45 / 85 11 3 Which domain, resolution, and models of the CORDEX project should be selected for the analysis of 21st century climate change in Iceland? The subject of this chapter /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 39. VI_2020_004

  .................... 85 8 Figure 57 50% PM10 probability map for an eruption like 1362 at Öræfajökull ..................... 86 Figure 58 The probability of exceedance curve at key locations (Öræfajökull) ...................... 87 Figure 59 Tephra accumulation rate on the ground on 7 May 1982 (Öræfajökull) ................. 88 Figure 60 Tephra accumulation rate on the ground on 5 May 1981 (Öræfajökull /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 40. VI_2009_006_tt

  farvegarins undir jöklinum út frá rúmmáli vatns sem þar hefur safnast fyrir benda til þess að viðnám gegn vatnsrennsli við jökul- botn minnki eftir því sem líður á hlaupið. Undir lok hlaupsins runnu á bilinu 80– 90 m3 s 1 um farveg sem var einungis einn þriðji hluti af rúmmáli farvegar sem flutti svipað vatnsmagn á fyrsta eða öðrum degi eftir að hlaupið hófst við jökuljaðar. Þessi niðurstaða er /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf