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  • 31. IPPC-2007-ar4_syr

    (-33%) during 1970 to 2004 has been smaller than the com- bined effect of global income growth (77%) and global population growth (69%); both drivers of increasing energy-related CO2 emis- sions. The long-term trend of declining CO2 emissions per unit of en- ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM} Differences in per capita income, per capita emissions and energy /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 32. Traffc-maintenance_expenditures

    Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009 ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost operating manage- ment develop- poned-, of land grants ons European tax over- level costs ment ment comprehen- build- and com- Regional De- heads 1991- 1991- sive- and ings pensation /media/loftslag/Traffc-maintenance_expenditures.pdf
  • 33. Paper-Olafur-Rognvaldsson_91

    of Icelandic glaciers 1992–1997). Rep. OS-98082 (in Icelandic), National Energy Authority, Reykjavík. Sigurðsson, O., Thorsteinsson Th., Ágústsson S. M. and Einarsson B. 2004. Afkoma Hofsjökuls 1997–2004. (Mass balance of Hofsjökull 1997–2004.) Rep. OS-2004/029, National Energy Authority, Reykjavík. Uppala, S.M., and 45 co-authors 2005. The ERA-40 re-analysis. Q. J. R. Mete- orol. Soc., 131, 2961 /media/ces/Paper-Olafur-Rognvaldsson_91.pdf
  • 34. Outline_for_the_case_Road_maintenance_in_a_changing_climate

    o t o - a g e n d a D e f i n e a n d i n v i t e s t a k e h o l d e r s T e c h n i c a l i n p u t a n d v i s i o n s - I n t e r n a l e x p e r t s - s t a k e h o l d e r e x p e r t s F r am e p r o b l e m - t r p s e r v i c e ( q u a l i t y ) l e v e l s - t y p e s o f s c e n a r i o s A n a l y z e p r o b l e m T e c h n i c a l i n p u t f r /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
  • 35. Linnet_Ulfar_CES_2010

    °C/100y 1975-2000 • 2.35 °C/100y 2000- •Change in precipitation • Average increase 4.8% / 100 y • Range 3.3 – 7.2 % •Glaciers • Results from CES • 25% decrease in volume from 2000 to 2050 Temperature transformation Com parison of series 10000 12000 14000 16000 18000 20000 22000 1 9 5 0 1 9 5 2 1 9 5 4 1 9 5 6 1 9 5 8 1 9 6 0 1 9 6 2 1 9 6 4 1 9 6 6 1 9 6 8 1 9 7 0 1 9 7 2 1 9 7 4 1 9 7 6 1 9 7 8 1 /media/ces/Linnet_Ulfar_CES_2010.pdf
  • 36. ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN

    /lexuriserv/lexuriserv.do?uri=com:2007:0002:FIN:EN:PDF, 13 April 2009. [2] WTO, World Tourism Organization (2008): “Climate Change and Tourism - Responding to Global Challenges”, UNWTO, 9 July 2008, Madrid, Spain. Available at: http://www.unwto.org/media/news/en/press_det.php?id=1411&idioma=E, 7 March 2010. [3] Mooney, J.E. y Miller, M.L. (2009): “Climate change: Creating demand for sustainable /media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf
  • 37. VI_2015_006

    Q. J. R. Meteorol. Soc., 137, 409-422. Giesen, R. H., Andreassen, L. M., Oerlemans, J., & van den Broeke, M. R. (2014). Surface energy balance in the ablation zone of Langfjordjøkelen, an arctic, maritime glacier in northern Norway. J. Glaciol., 60(219), 57-70. Seity, Y., Brousseau, P., Malardel, S., Hello, G., Bénard, P., Bouttier, F., . . . Masson, V. (2011). The AROME-France convective-scale /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
  • 38. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

    s fro m climat e ch ang e an d cr o ss bou ndar y adaptatio n measu res . In th e Netherl and s fo r hyd rodyna m ic mod el syst em s lik e SOB EK- W AQ UA (loca lleve l) an d e.g . fo rR hi ne flo w (ba sin wi de )c o n sid er ab le u n ce rta in tie s ex ist (W ee rts et al .200 3) D ev el op m en to fi nt eg ra te d ba sin m o de l( flo od ing an d poll ution) . 2: St at ist ic al /q ua lit /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
  • 39. VI_2009_012

    Different kinds of weights were tried in the regression process in which case the least squares problem becomes the problem of minimizing { }2102 ,...),()(log∑ − i iiii rMfPGXw , with respect to the parameters of the model f. The weights wi were generally of the form ),( rMq p wi = , where p was a normalization constant and usually q(M,r) was a discrete density distribution made to correct /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
  • 40. ces-oslo2010_proceedings

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