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• 21. Eyjafjallajokull_status_2010-05-03_IES_IMO

  Eruption in Eyjafjallajökull Status Report: 16:00 GMT, 03 May 2010 Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland Compiled by: Sigurlaug Hjaltadóttir, Freysteinn Sigmundsson, Björn Oddsson, Sigrún Hreinsdóttir, Þórdís Högnadóttir. Based on: IMO seismic monitoring; IES-IMO GPS monitoring; IMO hydrological data; web cameras of the eruption site from /media/jar/Eyjafjallajokull_status_2010-05-03_IES_IMO.pdf

• 22. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  296 Public Choice (2010) 143: 293–301 2 The commons The literature on the commons, or what is more technically defined as common-pool re- sources (CPRs), should be viewed initially from its place in the larger literature on dilem- mas of collective action. Since the foundational work of H. Scott Gordon (1954) on the com- mons, and Mancur Olson (1965) on collective action more broadly, the behavioral /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 23. Eyjafjallajokull_status_2010-04-28_IES_IMO

  Eruption in Eyjafjallajökull Status Report: 19:00 GMT, 28 April 2010 Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland Compiled by: MJR / SSJ / MTG / FS / SRG / GS / KH Based on: IMO seismic monitoring; IES-IMO GPS monitoring; IMO river gauges; web cameras of the eruption site from Vodafone, Mila, and Múlakot; IMO weather radar measurements; information /media/jar/Eyjafjallajokull_status_2010-04-28_IES_IMO.pdf

• 24. Grimsvotn_status_2011-05-22_IES_IMO

  to 10 kilometers. Heading: Most of the ash cloud heads to the south. Lower and scattered clouds head southwest and travel over the eastern part of the South Iceland Lowlands. The plume forms a 60 km long circular cloud around the eruption site with its lower boundary at a height of about 5 km. Out from this cloud, a scattered cloud lies to the north reaching about 450 km north /media/jar/Grimsvotn_status_2011-05-22_IES_IMO.pdf

• 25. Eyjaf_status_2010-05-04_IES_IMO

  of the eruption site from Vodafone, Milan and Mulakot; IMO weather radar measurements, NOAA satellite image; information from an eye witness at Fljótshlíð (MJR), information from the Icelandic Coast Guard flight. Eruption plume: Height (a.s.l.): Plume observed at 5.8-6 km height (19-20,000 ft) estimated from the Icelandic Coast Guard (ICG) flight at 10:40 and 15:30 GMT /media/jar/Eyjaf_status_2010-05-04_IES_IMO.pdf

• 26. Eyjafjallajokull_status_2010-05-01_IES_IMO

  Eruption in Eyjafjallajökull Status Report: 18:00 GMT, 01 May 2010 Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland Compiled by: MJR / HB / FS / SSJ / BO Based on: IMO seismic monitoring; IES-IMO GPS monitoring; IMO hydrological data; web cameras of the eruption site from Vodafone, Mila, and Múlakot; IMO weather radar measurements; information from /media/jar/Eyjafjallajokull_status_2010-05-01_IES_IMO.pdf

• 27. Grimsvotn_status_2011-05-23_IES_IMO

  At altitudes of 8 km and higher, part of the plume heads to the west. Colour: Brown- or grayish and sometimes black close to the eruption site. Tephra fallout: The amount of fallout is great from Vík in the west to the east of Öræfajökull. The amount of ash fall is the greatest close to the village Kirkjubæjarklaustur. Ash has been detected in several areas throughout the country, except /media/jar/Grimsvotn_status_2011-05-23_IES_IMO.pdf

• 28. norsem_sahar

  Soil structure impact on site effects and modeling spatial strong-motion variability across Icelandic strong-motion arrays Sahar Rahpeyma and Benedikt Halldorsson PhD Student (SR) and Director of Research (BH), Earthquake Engineering Research Centre, and Research Professor (BH), Faculty of Civil and Environmental Engineering, School of Engineering and Natural Sciences, University of Iceland /media/norsem/norsem_sahar.pdf

• 29. 2010-05-02_En-IES_IMO

  Eruption in Eyjafjallajökull Status Report: 21:00 GMT, 02 May 2010 Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland Compiled by: MJR / MTG / FS / BO / SSJ / SH Based on: IMO seismic monitoring; IES-IMO GPS monitoring; IMO hydrological data; web cameras of the eruption site from Vodafone, Mila, and Múlakot; IMO weather radar measurements; information from /media/jar/2010-05-02_En-IES_IMO.pdf

• 30. Reykholt-abstracts

  driving melt pond formation and evolution at the ice surface. Changes in the surface morphology of snow- then melt pond-covered ice were measured quantitatively with a terrestrial laser scanner (lidar) and, in combination with physical measurements taken along a geostatistical transect adjacent to the laser scanning site, were used to calculate mass and meltwater balance at the ice surface. We /media/vatnafar/joklar/Reykholt-abstracts.pdf