60 results were found for Fethiye Otel Fiyatları 0534 512 68 98 Tlos Butik Otel.

Results:

• 11. norsem_mantyniemi

  Macroseismology in Finland from the 1730s to the 2000s: From an obligation of the learned elite to citizen science Päivi Mäntyniemi Institute of Seismology, Department of Geosciences and Geography, P.O. Box 68, FI-00014 University of Helsinki, Finland, e-mail: paivi.mantyniemi@helsinki.fi The presentation is based on a snapshot of macroseismology in Finland from the 1730s to the 2000s that has /media/norsem/norsem_mantyniemi.pdf

• 12. ces-oslo2010_proceedings

  ...................................................................... 66 Roald, L.A., Beldring, S. and Engen-Skaugen, T. Long term variability and projection of shifts in the streamflow at selected catchments in Norwegian rivers induced by climate change .................................................................................................................................... 68 Wilson, D., Roald, L.A., Lawrence, D /media/ces/ces-oslo2010_proceedings.pdf

• 13. vanRoosmalen_etal-2009-WRR_2007WR006760

  occurring during winter from 86% in the present climate to 98% in the year 2100. High evapotranspiration during summer was mainly attributed to forests because forests were able to utilize most of the increase in soil moisture storage that came from winter recharge. For future studies Woldeamlak et al. [2007] suggested use of transient models to study seasonal varia- tions of the groundwater /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 14. 2010_003rs

  10. Rake distribution for mapped faults/clusters in box J, Hella. ........................ 97 Figure B.11. Rake distribution for mapped faults/clusters in box K, Hraungerði. ............. 97 Figure B.12. Rake distribution for mapped faults/clusters in box L, Skeið. ........................ 98 Figure B.13. Rake distribution for mapped faults/clusters in box M, Land. ....................... 98 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 15. Eriksson_2-Acceptability-of-policy

  % (2%), own reduction 18% (21%), effectiveness 17% (47%), fairness 35% (27%), acceptability 51% (49%). .42 (.43) .11 (.17) .14 (24) .58 (.50) .40 (.44) .10 (.14) .16 (.26) .17 (.16) .42 (68) .50 (48) .19 (.26) .48 (.31) .27 (.31) .17 (.14) .37 (34) Acceptability of raised tax on fuel Freedom Effectiveness Own reduction Fairness Problem awareness Personal norm Pro-env orientation Willingness /media/loftslag/Eriksson_2-Acceptability-of-policy.pdf

• 16. CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction

  2010: Climate Change and Freight Transport. Publications of the Ministry of Transport and Communications 15/2010. 98 pp. (in Finnish, abstract in English) [6] Perrels. Adriaan, Himanen, Veli, Lee-Gosselin Martin (2008), Building Blocks for Sustainable Transport – Obstacles, Trends, Solutions, Emerald publishers. /media/loftslag/CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction.pdf

• 17. 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

• 18. Eriksson_Garvill_Nordlund_2006

  were more opposed to this TDM measure compared to the increase with two SEK/liter (F ð1; 902Þ ¼ 4:98, po0:05, partial Z2 ¼ 0:005). Significant differences were found between all the examined evaluations of the three TDM measures. Increased tax on fuel was expected to infringe on freedom to choose travel mode to a larger extent compared to the information campaign. Improved public transport /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 19. VI_2020_011_en

  the Eldfell eruption ........................................................................................................................ 68 Tables Table 1: Properties of selected Vestmannaeyjar lava flows. ................................................... 18 Table 2: Characterization of the three different eruption size scenarios ................................. 24 Table 3 /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 20. 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