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Results:

• 31. Final estimates of the emissions from the Holuhraun eruption based on ground-based measurements

  1978, the advent of satellite monitoring of volcanic eruption clouds. The Holuhraun eruption released 16 times more SO2 (sulfur dioxide, 9.6 Mt) and almost twice as much CO2 (carbon dioxide, 5.1 Mt) as one year´s worth of anthropogenic emissions within Iceland (0.06 Mt SO2 and 3 Mt CO2 in 2015). The gases from the eruption were quite poor in the halogens HCl (hydrogen chloride, 0.1 Mt /about-imo/news/final-estimates-of-the-emissions-from-the-holuhraun-eruption-based-on-ground-based-measurements-now-published

• 32. 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

• 33. GA_2009_91A_4_Andreassen

  (alb: AWS) MODELLING LONG-TERM SUMMER AND WINTER BALANCES ? The authors 2009 Journal compilation ? 2009 Swedish Society for Anthropology and Geography 241 ed temperatures relative to –20°C to account for de-cay of snow albedo at temperatures below the melt-ing point, following a study by Winther (1993). Wetested both approaches, and chose to use –5°C asthe minimum for the accumulated temperature /media/ces/GA_2009_91A_4_Andreassen.pdf

• 34. Hock_Regine_CES_2010rs

  Projections -50% -48%-73% -78% -80% +3% Storglaciären Mårmaglaciären Scandinavia Comparison with all other glacier regions Volume reduction and sea-level equivalent (SLE) until 2100 for 19 glacier regions Radic and Hock, submitted Antarctica Sub-Antarctic Islands Greenland New Zealand South America II South America I Iceland Arctic Canada West Canada and West US Alaska High Mountain Asia North /media/ces/Hock_Regine_CES_2010rs.pdf

• 35. VI_2014_005

  such as too low 2-m air temperatures, variable snow cover is completely removed from the entire model domain after completion of the first cold-start forecast.3 Based on the corrected initial data, the 6-hour cold-start forecast run is repeated, without building the model domain again ({BUILD-no}). Beginning with the end of the “no-snow cold-start” on 1 Septem- ber at 0 UTC, the model is run in surface /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 36. ESC-IASPEI-statement-LAquila-2012-1

  ) ESC Executive Committee Alexey Zavyalov, Russia Murat Nurlu, Turkey Mariano García-Fernández, Spain Stefano Parolai, Germany Pierre-Yves Bard, France Constantin Ionescu, Romania Stefano Solarino, Italy Steinunn Jakobsdottir, Iceland Peter Suhadolc, IASPEI Rémy Bossu, EMSC-CSEM Atilla Ansal, EAEE Bernard Dost, ORFEUS Rajender K. Chadha, ASC EUROPEAN SEISMOLOGICAL COMMISSION /media/vedurstofan/utgafa/hlidarefni/ESC-IASPEI-statement-LAquila-2012-1.pdf

• 37. Eriksson_2-Acceptability-of-policy

  (Stern, 2002) 4 5 (1) Concepts • Acceptability - attitude toward policy (e.g., Schade, 2003). Salient beliefs attitudes (Eagly & Chaiken, 1993). • Acceptability (before implementation) versus acceptance (after implementation) (Gärling et al. 2008) • Attitude (acceptability/acceptance) versus behaviour (Eagly & Chaiken, 1993) (2) Factors important for acceptability • Acceptability /media/loftslag/Eriksson_2-Acceptability-of-policy.pdf

• 38. News

  2006 Search Search string Contact IMO © Veðurstofa Íslands | Bústaðavegi 7- 9 | 105 Reykjavík | Phone 522 6000 | Fax: 522 6001 Recording 902 0600 | SSN 630908-0350 /about-imo/news/bigimg/2910

• 39. VI_2017_009

  we take the corresponding data from the CMIP5 project. Table 1. All GCMs and RCMs used in this study. If a model is available for any of the domains Arctic-44, EURO-44, or EURO-11, it is marked with a v, but with an x if it is unavailable. Model name Type EURO-11 EURO-44 Arctic-44 CCCma-CanESM2 GCM x v v COSMO-CLM4-8-17 RCM v v x CNRM-CERFACS-CNRM-CM5 GCM v v x IHCEC-EC-Earth GCM v v v /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 40. Group2-report

  1    Adaptive management to climate change in Horsens Fjord using scenario  development    Report by Maria, Azhar, Bjarke and Kerstin  Introduction  Horsens Fjord is an eutrophic estuary situated in east coast of Jutland, Denmark with approximately 46 km2  surface area. The Fjord is a part of bigger WFD catchments area with dominated agriculture area and small  forest, wetlands, lakes, and urban /media/loftslag/Group2-report.pdf