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Results:

• 31. 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

• 32. Lorenzoni_Pidgeon_2006

  for people to conceptualise and to relate to their daily activities, arguably because it cannot be easily translated into the language of popular culture (Ungar, 2000; see also mental models of cli- mate change by Bostrom et al., 1994; Kempton, 1997; discussed later). Secondly, the various datasets available detailing public opinions and attitudes on climate PUBLIC VIEWS ON CLIMATE CHANGE: EUROPEAN /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 33. News

  beams into the atmosphere and measures the resulting reflection via backscattering. The instrument is used to estimate the amount of ash in the atmosphere. News 2023 2022 2021 2020 2019 2018 2017 2016 /about-imo/news/bigimg/2183

• 34. Eyjafjallajökull eruption 2010 - the role of IMO

  in April-May 2010, IMO monitored the volcanic activity through various geophysical sensors (seismic, strain, GPS), river runoff from the glacier and the behaviour of the volcanic eruption cloud (see slide show). The main tool for monitoring the volcanic cloud was a C-band weather radar located at Keflavik international airport, approximately 150 km west of the volcano (see map below). Plume height /earthquakes-and-volcanism/articles/nr/2072

• 35. The Eyjafjallajökull eruption 2010

  on activity in Eyjafjallajökull assessment from 14 April until 9 October 2010 QA on the eruption in Eyjafjallajökull, Iceland - 17 April Forecast for volcanic ash fall in Iceland - updated from 20 April until 23 May Photos from Eyjafjallajökull - 9 May An eruption in South Iceland - 23 MarchPhoto galleriesReconaissance flights with the Icelandic Coast Guard - from 24 March until 22 May Local /volcanoes/about-volcanoes/eyjafjallajokull/the-eyjafjallajokull-eruption-2010/

• 36. Flood from Skaftá

  eastern and western, are located in the western part of Vatnajökull Ice-cap. They form because of geothermal activity that melts the glacier from below and water accumulates beneath them. When the hydro static pressure is high enough for the water to lift the ice above and flow from below the cauldrons it causes a flood. Floods from the eastern-cauldron are usually larger than the floods /about-imo/news/flood-in-estern-skafta

• 37. Flood from Skaftá

  eastern and western, are located in the western part of Vatnajökull Ice-cap. They form because of geothermal activity that melts the glacier from below and water accumulates beneath them. When the hydro static pressure is high enough for the water to lift the ice above and flow from below the cauldrons it causes a flood. Floods from the eastern-cauldron are usually larger than the floods /about-imo/news/flood-in-estern-skafta/

• 38. 2010_005_

  Century control runs, as well as 21st Century forecast runs, submitted by various institutions to the Intergovernmental Panel on Climate Change (IPCC) for their Forth 11 Table 1. General circulation and regional climate models that were considered in this study. Model Version Model Name, Institute BCCR BCM 2.0 Bergen Climate Model, Bjerknes Centre for Climate Research, Bergen, Norway CCCMA CGCM 3.1 /media/ces/2010_005_.pdf

• 39. Mission

  IMO has a long-term advisory role with the Department of Civil Protection and Emergency Management of the National Commissioner of the Icelandic Police and issues public alerts about impending natural hazards. The institute participates in international weather and aviation alert systems, such as London Volcanic Ash Advisory Centre (VAAC), and the Icelandic Aviation Oceanic Area Control /about-imo/mission/

• 40. Web-pages on the Eyjafjallajökull eruption 2010

  of the accesscontrolled area around Holuhraun lava field END OF ERUPTION declaredby the Scientific Board Location map (detailed)around the new lava field Bárðarbunga earthquakes3D interactive model Thickness and volumeestimate from January 1st Comparing historic sizes of lavafields: AD 934 and 1783 Gas dispersion model Preliminary flood risk assessmentfor Jökulsá /earthquakes-and-volcanism/articles/nr/2221