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Results:

• 31. VI_2014_005

  and direction, as well as air temperature, from the IMO operational surface station net- work. Most anemometers are installed at 10 m above ground level (mAGL). However, at some stations, surface winds are measured at different heights, h, varying between 4.0 and 18.3 m. 3This is done using a GRIB-API command on Parameter 141 (snow depth) in the earliest boundary data file: grib_set -f -d 0.0 -w /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 32. Bárðarbunga 2014 - August events

  line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude. During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately. 18 August 2014 20:45 - An overview of the first three days Since the onset of the earthquake swarm at Bárðarbunga on Saturday /earthquakes-and-volcanism/articles/nr/3000/

• 33. NONAM_1st_workshop_summary_v3

  /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 34. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  in the data used in making the decision and the factors are interlinked, all of which makes the problem highly complex. The part of the net defined by variables and links is relatively easily communicated to stakeholders (Henriksen et al., 2007b). However the tal Management 88 (2008) 1025–1036 quantitative part, with the conditional probability tables (CPTs), the numbers, is the step where /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 35. Kok_et_al._TFSC_published_2011

  development: Experiences from the SCENES project Kasper Kok a,
  , Mathijs van Vliet a, Ilona Bärlund c, Anna Dubel b, Jan Sendzimir b a Wageningen University, P.O. Box 47, 6700 AA Wageningen, Netherlands b International Institute for Applied Systems Analysis, Schlossplaz 1, A-2361 Laxenburg, Austria c Helmholtz Centre for Environmental Research (UFZ), Brückstrasse 3a, 39114 Magdeburg, Germany a r t i c /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 36. Kok_and_Veldkamp_editorial_ES-2011-4160

  Copyright © 2011 by the author(s). Published here under license by the Resilience Alliance. Kok, K., and T. (A.) Veldkamp. 2011. Scale and governance: conceptual considerations and practical implications. Ecology and Society 16(2): 23. [online] URL: http://www.ecologyandsociety.org/vol16/iss2/ art23/ Guest Editorial, part of a Special Feature on Scale and Governance Scale and Governance /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 37. Kok_JGEC658_2009

  scenario development, with an example from Brazil Kasper Kok * Land Dynamics, Department of Environmental Sciences, Wageningen University, P.O. Box 47, 6700 AA Wageningen, The Netherlands 1. Introduction The world is undergoing rapid changes while globalising constantly, which gives the consideration of the future new urgency and importance. Scenario development has emerged as a key method when taking /media/loftslag/Kok_JGEC658_2009.pdf

• 38. Adaptive management in relation to climate change

  Adriaan Perrels, Finnish Meteorological Institute, FMI Sigrún Karlsdóttir, Icelandic Meteorological Office, IMO Frederik Uldal, International Research School of Water Resources (FIVA) Lecturers Kasper Kok, Wageningen University, The Netherlands Louise Eriksson, Umeå University, Sweden Matt Hare, Seecon, Germany Jens Christian Refsgaard, Geological Survey of Denmark and Greenland, GEUS Hans /nonam/phd-summerschool/

• 39. VI_2022_006_extreme

  that, the detrended timeseries would have had a net difference of zero if the negative values had not been set back to zero. This shows that over the 39 years of data, there was a slight precipitation increase for this grid-point. This trend has been removed, resulting in a detrended, almost flat dataset. 29 Figure 14. Regression lines for hourly precipitation timeseries of grid-point [100, 100] from /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 40. VI_Arsskyrsla_2018_vef

  grundvelli myndatöku með flygildum og leysimælitæki (TLS) hefur verið notað við kortlagningu flóðfara og við mat á útbreiðslu og umfangi hlaupa. Þétt net jarðskjálftamæla, sem staðsettir eru á jökulskerjum eða grafnir í jökul, hefur gefið góða raun við ákvörðun á dýpi jarðskjálfta undir jöklum. Kvikuhreyfingar hafa þannig verið kortlagðar og myndun gosrása staðfest af meiri nákvæmni en áður. Þó /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf