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Results:

• 11. CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction

  of climate change on the routine and periodic maintenance of roads. Helsinki 2009. Finnish Road Administration, Central Administration. Finnra reports 8/2009, 66 p. + app. 8 p. ISSN 1459-1553, ISBN 978-952-221-172-9, TIEH 3201122-v. (in Finnish, abstract in English) [5] Salanne, i., Byring, B., Valli, R., Tikkanen, R., Peltonen, P., Haapala, J., Jylhä, K., Tolonen-Kivimäki, O., and Tuomenvirta, H /media/loftslag/CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction.pdf

• 12. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 13. 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

• 14. Adalgeirsdottir-etal-tc-5-961-2011

  961–975, 2011 966 G. Aðalgeirsdóttir et al.: 20th and 21st century evolution of Hoffellsjökull glacier Table 1. Specific winter (bw), summer (bs) and net balance (bn) for Hoffellsjökull in mw.e. a−1. A conservative error estimate is on the order of 15–20 % for both bw and bs. Glacier year bw bs bn 1935–1936 2.0 −3.4 −1.4 1936–1937 2.4 −2.1 0.3 1937–1938 1.7 −2.4 −0.6 2000–2001 2.0 −2.1 −0.1 2001 /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 15. VI_2015_006

  ....................................................................................... 10 3 September 2012 .................................................................................. 12 3 Radiation fluxes at the surface ....................................................................... 16 4 Heat fluxes at the surface .............................................................................. 21 5 Net energy /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 16. vanRoosmalen_etal-2009-WRR_2007WR006760

  with 20% and 2% for the HIRHAM experiments using HadAM3H and with 30% and 7% for the ECHAM- driven experiments for Middle Europe and Scandinavia, respectively. [18] RCM output is not available for the entire period 1961–2100 because transient RCM simulations are com- putationally very demanding. Instead two 30-year time slices are available; one representative for the climate in the period 1961–1990 /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 17. 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

• 18. Machguth_Horst_CES_2010

  experiments with different RCM’s • explore RCM biases • apply a different mass balance model data 2 RCM’s • HIRHAM4, Scenario A1B, 25 km, 1950-2100, Greenland • RCAO, Scenario A1B, 50 km, 1960-2100, Pan-Arctic 4 Weather Stations (Ta, Sin) • GC-Net Swiss Camp: 1150 m a.s.l. (1995 – 2006) • GC-Net Crawford: 2020 m a.s.l. (1995 – 2006) • Asiaq Station 437: 300 m a.s.l. (1983 – 2006) • DMI Illulisat /media/ces/Machguth_Horst_CES_2010.pdf

• 19. ces-oslo2010_proceedings

  anomalies of the WTs during the periods leading up to the five most severe droughts as compared to the average frequency of a given WT for the same period of the year over the entire data record. A period equal to dreg preceding the drought plus the 20 first days of the drought was used. All WTs with a net positive frequency anomaly over the five events were considered to be associated /media/ces/ces-oslo2010_proceedings.pdf

• 20. Reykholt-abstracts

  /media/vatnafar/joklar/Reykholt-abstracts.pdf