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• 41. Eyjafjallajokull_status_2010-04-29_IES_IMO

  Eruption in Eyjafjallajökull Status Report: 18:00 GMT, 29 April 2010 Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland Compiled by: MJR / HB / MTG / SSJ / GS / BO 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_2010-04-29_IES_IMO.pdf

• 42. Eyjafjallajokull_status_2010-04-30_IES_IMO

  Eruption in Eyjafjallajökull Status Report: 17:00 GMT, 30 April 2010 Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland Compiled by: MJR / MTG / FS / GS / SSJ 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_2010-04-30_IES_IMO.pdf

• 43. hafisskyrsla_18ag2011

  skipið er að koma frá Scoresbysundi, Grælandi og er á leið til Vestmannaeyja, áætlar að vera þar þann 20. ágúst 2011 kl 0700 á staðartíma. Um borð eru 157 manns þar af er áhöfn 41 manns. Skipið sendi tilkynningu til LHG kl 1100 á staðaratíma í dag. Kl.1322 kallar TFB vegna Steina í Höfða sknr. 2434, TFB er með stað síðan kl. 0530, 67°05N – 018°35V. Samkvæmt göngum TF-SIF þá sást hann á /media/hafis/skyrslur_lhg/hafisskyrsla_18ag2011.pdf

• 44. Isskyrsla_06Jan_2010

  lágu frá aðal ísnum og náðum að meta þéttleikann þar. Ekki sáust neinir borgarísjakar né stakir ísjakar í þessu flugi. Aðalrönd íssins lá í gegnum eftirtalda punkta (tekið með radar). Að sjá var ísinn samfrosta 10/10 1. 66°13,7‘N – 025°35,7‘V 2. 66°24,0‘N – 024°26.0‘V 3. 66°50,1‘N – 023°44,1‘V 4. 67°03,1‘N – 023°31,0‘V 5. 67°00,7‘N – 023°11,3‘V 6. 66°58,7‘N – 022°39,7‘V 7. 66°55,8‘N – 022°23,5‘V /media/hafis/skyrslur_lhg/Isskyrsla_06Jan_2010.pdf

• 45. The weather in Iceland 2006

  fire is the largest known in Iceland, about 67 sq kilometers (6700 hectares) were burned. The squads fighting the fire managed to shield all farmhouses in the very sparsely populated area. The area will presumably recover in a few years as there is no forest there. Reykjavík Figure 2. Reykjavik from the air on January 23rd 2006. The headquarters of IMO are in the center of the picture /about-imo/news/2007

• 46. Reports and publications

  of work (PDF) Ragnar Stefánsson et al. 67 0,9 2001 PRENLAB-TWO - final report April1, 1998 - June 30, 2000 Ragnar Stefánsson et al. 2001 Foreshock activity, fault radius and silence - earthquake warnings based on microearthquakes Ragnar Slunga 2001 32nd Nordic Seminar on Detection Seismology Barði Þorkelsson et al. 2001 SMSITES - Report, November 2001 Ragnar /earthquakes-and-volcanism/reports-and-publications/

• 47. The weather in Iceland 2006

  fire is the largest known in Iceland, about 67 sq kilometers (6700 hectares) were burned. The squads fighting the fire managed to shield all farmhouses in the very sparsely populated area. The area will presumably recover in a few years as there is no forest there. Reykjavík Figure 2. Reykjavik from the air on January 23rd 2006. The headquarters of IMO are in the center of the picture /about-imo/news/2007/

• 48. The weather in Iceland 2006

  fire is the largest known in Iceland, about 67 sq kilometers (6700 hectares) were burned. The squads fighting the fire managed to shield all farmhouses in the very sparsely populated area. The area will presumably recover in a few years as there is no forest there. Reykjavík Figure 2. Reykjavik from the air on January 23rd 2006. The headquarters of IMO are in the center of the picture /about-imo/news/nr/1206

• 49. The weather in Iceland 2006

  fire is the largest known in Iceland, about 67 sq kilometers (6700 hectares) were burned. The squads fighting the fire managed to shield all farmhouses in the very sparsely populated area. The area will presumably recover in a few years as there is no forest there. Reykjavík Figure 2. Reykjavik from the air on January 23rd 2006. The headquarters of IMO are in the center of the picture /about-imo/news/nr/1206/

• 50. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  (2008), ENFJ was the most frequent type for the Ph.D. climate researchers attending the symposia, with ENFP ranking as only the fifth most frequent personality type (Fig. 2). Similarly, only 7% of symposia participants preferred the ISTJ personality type which is the most frequent personality type for a variety of scientific occupations including: biochemists, biologists, chemists, economists /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf