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Results:

• 41. QA on the eruption in Eyjafjallajökull 2010

  health, for example the respiratory system. The fluorine content is approximately 850 mg/kg according to chemical analysis carried out by the Institute of Earth Sciences, University of Iceland, on a sample taken 19 April. An earlier sample since 14 April only measured 25-35 mg/kg of fluorine because the water vapour from melting ice rinsed the ash. When the eruption progressed, water became less /earthquakes-and-volcanism/articles/nr/1880

• 42. ice-chart_colour-code-standard

  - this is different from “No Information” which indicates that nothing at all is known about the area. 5) No specific colour is assigned to areas of “No Information”; such areas should be clearly indicated on ice charts - text annotation may be used where appropriate; an assigned colour within the code should not be used to indicate “No Information”. 6) Colour codes do not preclude use of black /media/hafis/frodleikur/ice-chart_colour-code-standard.pdf

• 43. Statistical Analysis

  and Chemistry of the Earth, Special Issue: COST Action (Accepted for publication). Jónsdóttir, J. F., Uvo, C. B. & Clarke, R. T. (2008). Filling gaps in measured discharge series with model-generated series. Technical Notes. Journal of Hydrological Engineering, 13, 9, 905-909. Jónsdóttir, J. F., Uvo, C. B. & Clarke, R. T. (2008). Trend analysis in Icelandic discharge, temperature and precipitation series /ces/publications/nr/1943

• 44. Fagradalsfjall eruption unusual in many ways compared to other eruptions

  deformation and seismicity preceding the eruption that began 19 March 2021. a) Model of deformation 24 February – 19 March, showing horizontal displacements as arrows and vertical displacements with a colour scale. The red line shows the location of the dyke and the broken black line shows the central axis of the plate boundary b) Hourly earthquake rate (blue) and cumulative number of earthquakes /about-imo/news/fagradalsfjall-eruption-unusual-in-many-ways-compared-to-other-eruptions

• 45. Fagradalsfjall eruption unusual in many ways compared to other eruptions

  deformation and seismicity preceding the eruption that began 19 March 2021. a) Model of deformation 24 February – 19 March, showing horizontal displacements as arrows and vertical displacements with a colour scale. The red line shows the location of the dyke and the broken black line shows the central axis of the plate boundary b) Hourly earthquake rate (blue) and cumulative number of earthquakes /about-imo/news/fagradalsfjall-eruption-unusual-in-many-ways-compared-to-other-eruptions/

• 46. Glacier change sessions at this year's Arctic Circle

  from other parts of the archipelago. (Photo; Fr. Marek Michalski). A new accurate high-resolution digital elevation model of Iceland A special workshop on the use of the above-mentioned ArcticDEM and upcoming new data to monitor glacier changes was organized by IMO during the Arctic Circle Assembly, with participation from universities and surveying institutes in Austria, Canada, Denmark /about-imo/news/glacier-change-sessions-at-this-year-s-arctic-circle-assembly

• 47. Awards and press

  our users to the comprehensive web of the Icelandic Road and Coastal Administration, road.is. Appraisal during Bárðarbunga and Holuhraun 2014 - 2015 From Belmont, MA, USA: "Congratulations and thank you for superb coverage and public release of information about the Bárðarbunga eruption 2014 - 2015. I have been on the staff of Harvard SEAS for decades, retired now. I have visited /about-imo/the-web/awards_and_press/

• 48. Hock_Regine_CES_2010rs

  Projections -50% -48%-73% -78% -80% +3% Storglaciären Mårmaglaciären Scandinavia Comparison with all other glacier regions Volume reduction and sea-level equivalent (SLE) until 2100 for 19 glacier regions Radic and Hock, submitted Antarctica Sub-Antarctic Islands Greenland New Zealand South America II South America I Iceland Arctic Canada West Canada and West US Alaska High Mountain Asia North /media/ces/Hock_Regine_CES_2010rs.pdf

• 49. Nikulin_Grigory_CES_2010

  driven by different global climate models Nikulin et al., Tellus A 2010, accepted Models Regional climate model RCA3 (Rossby Centre, SMHI, Sweden) Europe, resolution: 50 km Forcing global models (A1B) ECHAM5-r3 (MPI, Germany) HadCM3-ref (MOHC, UK) BCM (NERSC, Norway) CCSM3 (NCAR, USA) CNRM (CNRM, France) IPSL (IPSL, France) Reference simulation driven by ERA40 Reanalysis Observations gridded E /media/ces/Nikulin_Grigory_CES_2010.pdf

• 50. Group-1_Scenarios-for-AWM

  t / c o s t ratio H i g h L o w S c enar i o 1 S c ena r io 2 Present time 20302020 Socio E c onomic D e v elopme n t Figure 1. Scenario building for AWM in Horsens Fjord To estimate of the adaptation strategy (Table 2) we will use back-casting approach. The assessments of the productivity of this approach are based on main big strategies which need to have an attention. One of them /media/loftslag/Group-1_Scenarios-for-AWM.pdf