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  • 51. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

    measures Downscaling and statistical correction Water system impacts Hydro-ecological models Socio-economic scenarios Socio-economic impacts Fig. 2 Structural elements in the assessment of climate change impacts and adaptation illustrating the uncertainty cascade Mitig Adapt Strateg Glob Change Tabl e 1 Ch aracterisatio n o fke y sou rce s o fun certaint y in th eun certaint y casc ad ean d thei rnatur /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf
  • 52. Kok_1-scenarios-lecture-1

    :15-11:30 Practical examples + conclusions • Exploratory scenario development – SAS approach • Group model building - Fuzzy Cognitive Maps • Normative scenario development - Backcasting Conclusions LECTURE 1 Scenario development Underlying issues and concepts Content Lecture 1: an introduction • Complex problems • Complex System analysis • Tools and methods to analyse complex systems o Methods /media/loftslag/Kok_1-scenarios-lecture-1.pdf
  • 53. Group3-Road-scenarios

     Climate data o Increase in precipitation o Change in road deterioration o Frequency of high and low temperatures o Heavy rainfall o Increase in average temperature Technical state of the roads – state of the Finnish road network: data available from Road administration Data on past events about climate related damage on roads Technical development of e.g. asphalt – more durable /media/loftslag/Group3-Road-scenarios.pdf
  • 54. TietavainenHanna_CES_2010

    the observed data sets are smaller in SW than in NE • MMM overestimates precipitation, but is closer to observations in SW than NE barb2right Better observational coverage in SW SW NE p r e c i p i t a t i o n s u m ( m m ) CES Conference, Oslo 31.5.-2.6.2010 SWNE • Precipitation trends (mm / 10 yr) in 1961-2000 according to observations and model simulations (MMM) • Including the range /media/ces/TietavainenHanna_CES_2010.pdf
  • 55. Glossary

    We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208
  • 56. Glossary

    We are hoping to find time to improve this glossary. Only a few items are available. For your relevant search, please click on one of the letters below: A Á B C D E É F G H I Í J K L M N O Ó P Q R S T U Ú V W X Y Ý Z Þ Æ Ö A A: Icelandic abbreviation of East (compass direction, easterly, eastern). ANA: Icelandic abbreviation of Eastnorthesast (compass direction). ASA: Icelandic /weather/articles/nr/1208/
  • 57. VI_2009_006_tt

    to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
  • 58. Bardarbunga-2014_September-events

    subsidence in Bárðarbunga and insignificant crustal movements north of Vatnajökull around the dyke.  Air quality in urban areas in the East of Iceland:  o High air pollution was detected yesterday in Egilsstaðir and Reyðarfjörður. Forecasts indicate that the gas cloud will blow towards the north in the next 24 hours. High concentrations of sulphuric gases can be expected in Mývatnssveit /media/jar/Bardarbunga-2014_September-events.pdf
  • 59. High resolution precipitation maps for Iceland

    maps for 1971-2000 Daily precipitation maps are available on request and further information on the making of the maps. IMO's contacts for this project are Philippe Crochet and Tómas Jóhannesson. Reference: Crochet, P., T. Jóhannesson, T. Jónsson, O. Sigurðsson, H. Björnsson, F. Pálsson and I. Barstad (2007): Estimating the spatial distribution of precipitation in Iceland using a linear model /weather/articles/nr/1625
  • 60. norsem_lindholm

    Neotectonics in Nordland; NEONOR 2 C. Lindholm, O. Olesen, I. Janutyte, S. Gradman, M. Keiding, H. Kierulf, M. Ask, J. Dehls, Y. Maystrenko, F. Riis, L. Rise and other project partners The Nordland shore region is known to be seismically active with deep local sediment basins on the continental shelf that stretches some 200 km west of the coastline. The offshore areas west of Nordland have /media/norsem/norsem_lindholm.pdf

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