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• 11. Program

  to investigate glacier geomorphic processes Rudolf Sailer, Erik Bollmann, Veronika Ebe, Anna Girstmair, Christoph Klug, Lorenzo Rieg, Maximilian Spross and Johann Stötter, Institute of Geography, University of Innsbruck, Austria. Potentials of ALS in the analysis of geomorphodynamic processes in high alpine regions Coffey 15:00–15:30 Thursday 15:30–17:30 ‒ Lidar measurements from space Beata Csatho /lidar/lidar-2013/program/

• 12. VAT_newsletter_2018_06

  mass balance in a warming climate but also due to calving (ice breaks of the front into lakes or sea) into Jökulsárlón lagoon. Calving currently causes about / of the mass loss of Breiðamerkurjökull. The large ice sheets of Antarctica and Greenland lose large amounts of ice by calving, and the rate of loss has intensied greatly in recent years.    Rapid melting of glacial ice /media/Eplicanámskeið/VAT_newsletter_2018_06.pdf

• 13. NONAM_1st_workshop_summary_v3

  ; in particular Chapter 4). 7 Seppo Saarelainen & Lasse Makkonen: Adaptation to climate change in the road management – Pre-study. Helsinki 2007. 8 The Finnish Road Administration (Finnra) (2009), The effect of climate change on the routine and periodic maintenance of roads, Finnra report 8/2009, (in Finnish, abstract in English). 9 Salanne, i., Byring, B., Valli, R., Tikkanen, R., Peltonen, P /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 14. Reykholt-abstracts

  in July 2016 on a Delta II rocket from Vandenberg Air Force Base in California. ICESat-2 will carry the Advanced Topographic Laser Altimeter System (ATLAS) and collect data to a latitudinal limit of 88 degrees. In contrast to Geoscience Laser Altimeter System (GLAS) on ICESat, ATLAS employs a 6-beam micro-pulse laser photon-counting approach. It uses a high repetition rate (10 kHz; 70 cm /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 15. VI_2014_005

  lines). Additionally, the aver- age profiles for offshore distances to the coast of up to 30 km are shown by the black lines. For temperature, the dashed lines indicate linear projection from the two lowest model levels to 2 m above ground. A comparison of monthly averages of simulated 2-m temperature with station measurements, both for SURFEX and projected values, is shown in Figure 8. On average /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 16. Moellenkampetal_etal-2010

  Acteurs et Usages (UMR G-EAU), Cemagref, 4University of Architecture, Civil Engineering and Geodesy, 5Hornsby Shire Council, 6Lisode, 7UN-Water Decade Programme on Capacity Development (UNW-DPC), United Nations University, 8School of Natural and Rural Systems Management, University of Queensland, 9College of Asia and the Pacific, The Australian National University, 10Marine and Atmospheric Research /media/loftslag/Moellenkampetal_etal-2010.pdf

• 17. Hare-2011-ParticipatoryModelling

  are labelled according to the geographical area of application. Examples such as Zürich and Hase II have already been reviewed and categorized in Hare et al. (2003) and Bots and van Daalen (2008), respectively. The entire Iskar process, of which Iskar (Phase I) is a part, has been categorized by Barreteau et al. (2010). All are included in this review to provide alternative analytical perspectives /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 18. vonKorff_etal-2010

  played a role in this first phase as the author tables on decision analysis show. In summary, the comparison resulted in the reconstruction of 10 steps on which there appears to be considerable agreement among the five guides. 1. DA 1: Assemble a team for decision analysis as part of the participation design. Its members should belong to the lead agency, e.g., the water board, but can also /media/loftslag/vonKorff_etal-2010.pdf

• 19. 2010_017

  m J M5 [C°] -3 obs. [C°] -4 nce 1 re 5. Comp 26); an int temperatu this system y gridded v picion abo -Jökulsá w similar dif han observ h elevation ces the effe months No ly only on high the tem n band wi refore be s onthly tem an Feb Ma .2 -3.1 -3. .3 -4.1 -3. .1 1.0 0.6 arison of m erpolation re is shown atic differe alues, see T ut the qual atershed; b ference wa ations for t gradient fo /media/ces/2010_017.pdf

• 20. Keskitalo_et_al-MLG_and_adaptation_FINAL

  areas: to the regional arm of the state (the county administrative boards) to coordinate adaptation; to specific governmental bodies and agencies to develop a common elevation data basis; and for the assessment of flood risk and erosion defense measures around Lake Vänern. Risks considered by the Bill include the flooding of central Gothenburg, the second largest city of Sweden (a risk /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf