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  • 41. Climate Report

    ) noted that Iceland had a maritime climate that was much milder than its position on the globe might suggest. In data from 1981–2010, Iceland annual average temperatures ranged from 6°C at the south coast to 3°C at the north coast, with a substantially colder highland interior. In comparison with the latitudinal average for the same period, the coastal temperatures in Iceland are 8–10°C warmer /climatology/iceland/climate-report
  • 42. Climate Report

    ) noted that Iceland had a maritime climate that was much milder than its position on the globe might suggest. In data from 1981–2010, Iceland annual average temperatures ranged from 6°C at the south coast to 3°C at the north coast, with a substantially colder highland interior. In comparison with the latitudinal average for the same period, the coastal temperatures in Iceland are 8–10°C warmer /climatology/iceland/climate-report/
  • 43. Keranen_Jaana_CES_2010

    Energy source - Catchment area - Collection area - Wind - Biomass - etc. 2. Power Plant - Technique - Maintenance - Personnel - Organisation - etc. 902/07/2010 Tools for risk/opportunity identification very likely 2.1 - M o re rainfall: annual runo ff w ill inc rease 0 -8 % Sc en ario 2. inc reased p re cip itation 1.2 - … very likelyinc rease turbine capa city increased electrica l resis /media/ces/Keranen_Jaana_CES_2010.pdf
  • 44. 2010_017

    of radiation are added to a classic degree-day model. For infiltration, a methodology of Peschke, based on the approach of Green and Ampt, was used. To calculate the fluxes within the unsaturated soil zone, the Richards equation was used. The groundwater table was modelled in both the unsaturated zone module and the groundwater module. The coupling between both modules was done by a net /media/ces/2010_017.pdf
  • 45. VI_2021_008

    in Figure 8a are colored green, while the three to the NE plotted in Figure 8b are colored yellow. Table 2. Table of the visually picked arrival times of the Hekla 2000 eruption tremor to stations WSW of the volcano (hau, sau, kri, grv) and NE of the volcano (skr, ren, gil). Tremor velocities are with respect to the previous station. Bearing from Hekla Station Name Distance from /media/vedurstofan-utgafa-2021/VI_2021_008.pdf
  • 46. Milly_etal-2008-Stationarity-dead-Science

    6University of Washington, Seattle, WA 98195, USA. 7NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA. *Author for correspondence. E-mail: cmilly@usgs.gov. An uncertain future challenges water planners. Published by AAAS on July 12, 201 1 www.sciencemag.or g Downloaded from 1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574 POLICYFORUM combined with opera- tions /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
  • 47. Climate and Modeling Scenarios

    ” (Poster) at at ESF-COST High Level Research Conference “Extreme Environmental Events” in Cambridge, 13.-17. December 2010. Jokinen, P. Several interviews especially related to severe weather, extreme heat and climate change for radio (~10 interviews), TV (one interview) and daily press (dozens) in late July and beginning of August. Jylhä, K. Four interviews by TV channels in Septemer and December /ces/publications/nr/1680
  • 48. Climate change and hydrology: Environmental and societal effects

    national and local power companies 40% and finally Reykjavik City and others 17%. In spite of the increased importance of this resource, the network system has diminished by 30% since 2008, i.e. fewer gauging and monitoring stations are operating today. Summary The climate and hydrology of Iceland are highly variable due to natural conditions. Significant changes in these factors over the last 15 /about-imo/news/nr/2910
  • 49. Hare_1_PartINONAM

    Participatory methods and processes for adaptive management Dr Matt Hare Independent Consultant, Mexico City Adaptive and participatory water management Matt Hare, hare@gmx.de 2011 – Summer School About myself ... • Bachelor in artificial intelligence (88-92) • PhD environmental modelling in knowledge and data-poor domains (95-99) • Co-founder of Seeconsult GmbH (03-onwards /media/loftslag/Hare_1_PartINONAM.pdf
  • 50. Keskitalo_et_al-MLG_and_adaptation_FINAL

    groups, while decentralisation may further result in a larger role for city networks or voluntary local level declarations in decision-making (Rhodes 2000). Given that some processes have moved up to the international level (or in Europe, to the EU level), network governance may also allow some actors to “jump scale” (Gupta 2008, Princen 2007) by drawing on or even lobbying processes /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

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