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Results:

• 21. TietavainenHanna_CES_2010

  -2100 p r e c i p i t a t i o n s u m ( m m ) • Relative increase largest in May • NE: Absolute increase largest in May-June barb2right the difference between the driest and wettest summer months will decrease • SW: Absolute increase largest in July barb2right increasing the inter-monhtly differences in precipitation • Smallest increase in August in both areas SW NE CES Conference, Oslo 31.5 /media/ces/TietavainenHanna_CES_2010.pdf

• 22. Hare_1_Part2

  is important to the person about a management issue a71 the important concepts in that system a71 and their relationships to one another (causal, structural etc.) a108 can identify beliefs about how the system works, as well as its problems and their solutions cognitive mapping Knowledge Elicitation 1. Individual SH cognitive maps (Hodgson‘s hexagon modelling) 2. Scientists‘ agent-based /media/loftslag/Hare_1_Part2.pdf

• 23. ces-oslo2010_proceedings

  change over the North Atlantic and in some simulations also for Iceland. In all areas, including the North Atlantic and Iceland, a clear climate change signal compared to the spread between the simulations is seen. The standard deviation calculated from 17 of the simulations are less than 1°C in all areas apart from Iceland where it reaches between 1 and 2°C and in parts of the Barents Sea where /media/ces/ces-oslo2010_proceedings.pdf

• 24. IPPC-2007-ar4_syr

  Approximate CO2-eq concentrations corresponding to the computed radiative forcing due to anthropogenic GHGs and aerosols in 2100 (see p. 823 of the WGI TAR) for the SRES B1, AIT, B2, A1B, A2 and A1FI illustrative marker scenarios are about 600, 700, 800, 850, 1250 and 1550ppm, respectively. d) Temperature changes are expressed as the difference from the period 1980-1999. To express the change relative /media/loftslag/IPPC-2007-ar4_syr.pdf

• 25. The weather in Iceland 2007

  warmest recorded, but in the Northeast and East it was among the 15 warmest. Multi-station temperature measurements go back to the early 1870s. In Reykjavik only May had slightly below normal temperatures (1961-1990) and in 7 of the months the temperature was more than 1.5°C above the normal. April and July were particularly warm and April registered the highest temperature ever measured in April /about-imo/news/2008/nr/1205

• 26. The weather in Iceland 2007

  warmest recorded, but in the Northeast and East it was among the 15 warmest. Multi-station temperature measurements go back to the early 1870s. In Reykjavik only May had slightly below normal temperatures (1961-1990) and in 7 of the months the temperature was more than 1.5°C above the normal. April and July were particularly warm and April registered the highest temperature ever measured in April /about-imo/news/nr/1205

• 27. Abstract_Impacts_of_Climate_Change_on_Stormwater_Systems_in_Reykjavik

  Impacts of Climate Change on Stormwater Systems in Reykjavík Ásta Ósk Hlöðversdóttir1*, Philippe Crochet2, Jónas Elíasson1, Hrund Ó. Andradóttir1 and Brynjólfur Björnsson3 1 University of Iceland, 2 Icelandic Meteorological Office, 3 Mannvit Engineering *Corresponding author. Email address: aoh3@hi.is Due to climate change, precipitation is projected to increase in Northern Europe (Bates /media/loftslag/Abstract_Impacts_of_Climate_Change_on_Stormwater_Systems_in_Reykjavik.pdf

• 28. norsem_atakan_ip

  episodes, geological information and modelling. In addition, transnational access to multi-scale laboratories and geo-energy test-beds for low-carbon energy will be provided. In total more than 450 DDSS elements will be integrated into Integrated Core Services (ICS), a platform that will ensure their interoperability and access to these services by the scientific community as well as other /media/norsem/norsem_atakan_ip.pdf

• 29. Keskitalo_et_al-MLG_and_adaptation_FINAL

  Department of Geography and Economic History, Umeå University, Umeå 90187, Sweden. Tel. +46-90-786 50 80. Fax. +46-90-786 63 59 Abstract A coherent application of a multi-level framework that takes interactions between levels and how these are shaped by the political system into account is a prerequisite for understanding the development and implementation of climate change adaptation policies /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 30. VI_2020_004

  vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Sara Barsotti, Veðurstofa Íslands Sigrún Karlsdóttir, Veðursstofa Íslands Anna María Ágústsdóttir, Landgræðslan Björn Oddsson, Almannavarnadeild Ríkislögreglustjóra Íris Marelsdóttir, Embætti landlæknis Þorvaldur Þórðarson, Jarðvísindastofnun H áskólans Þórólfur Guðnason, Embætti landlæknis Bogi B. Björnsson, Veðurstofa Íslands /media/vedurstofan-utgafa-2020/VI_2020_004.pdf