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• 51. Articles

  Articles © NONAM Merki þriðju norrænu alþjóðlegu ráðstefnunnar um veðurfarsbreytingar og aðlögun að þeim, sem /weather/articles/bigimg/2861

• 52. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  -corrected SPOT 5 high-resolution geometric (HRG) images with 2.5 m 2.5 m spatial resolution, acquired in the autumn 2003 and (4) airborne polarimetric synthetic aperture radar images observed simultaneously to the 1998 EMISAR images and the EMISAR DEM viewed as a shaded relief image (Magnu´sson et al. 2005b). We estimate the average specific net mass balance (in m yr1 w. eq.) as bn r DV A1  N /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 53. Isskyrsla_20100120

  :00 0 00:00 00:00 0 00:00 00:00 0 00:00 00:00 0 00:00 00:00 0 Samtals########### ########### 720 Flugleið:BIRK Garðskagi fyrir jökul og norður um fyrir Vestfirði. Farið dýpra til baka, um Víkurál og Skerjadýpi. Flugskýrsla TF-SIF Dags 20.01.2010. Flug nr. 00410.025 Ísdreifar sáust á ratsjá norður af Horni, þó ekkert sem hægt er að kalla samfellt. Ísröndin var næst landi 50 sml. NV frá Straumnesi /media/hafis/skyrslur_lhg/Isskyrsla_20100120.pdf

• 54. Joining forces in weather forecasting and climate research

  of how climate change will impact our countries” says Árni.A sustainable solution Powered entirely by Icelandic hydropower and geothermal energy sources and taking advantage of the local tempered climate for keeping the supercomputer components cool, the running costs and CO2 footprint will be kept to a minimum, saving tonnes of CO2 in line with the four nations' efforts towards reaching Net /about-imo/news/joining-forces-in-weather-forecasting-and-climate-research

• 55. IPPC-2007-ar4_syr

  a near-zero pre-industrial background concentration, primarily due to human activities. {WGI 2.3, SPM; SROC SPM} There is very high confidence that the global average net effect of human activities since 1750 has been one of warm- ing, with a radiative forcing of +1.6 [+0.6 to +2.4] W/m2 (Figure 2.4). {WGI 2.3, 6.5, 2.9, SPM} The combined radiative forcing due to increases in CO2, CH4 and N2O /media/loftslag/IPPC-2007-ar4_syr.pdf

• 56. ces-oslo2010_proceedings

  anomalies of the WTs during the periods leading up to the five most severe droughts as compared to the average frequency of a given WT for the same period of the year over the entire data record. A period equal to dreg preceding the drought plus the 20 first days of the drought was used. All WTs with a net positive frequency anomaly over the five events were considered to be associated /media/ces/ces-oslo2010_proceedings.pdf

• 57. Öræfajökull : Recent research

  of the chapters can be downloaded or short summaries read.Downloadable material:Full text (pdf 23 Mb)Front matter (pdf 180 Kb)Table of contents (pdf 7.9 Kb)Chapter I. Volcanogenic floods in Iceland: An exploration of hazards and risks (pdf 1.06 Mb)Pages 7–16Emmanuel Pagneux, Sigrún Karlsdóttir, Magnús T. Gudmundsson, Matthew J. Roberts og Víðir ReynissonShort summaryChapter II. Öræfajökull Volcano /volcanoes/about-volcanoes/oraefajokull/new-research/

• 58. hafisskyrsla_18ag2011

  /s J7BD6 á ch 16, færum okkur yfir á CH-6. Green Atlantic er vélbilaður og er dráttarbáturinn Vöttur SU sknr. 2734 er með hann í tog á leið inn á Reyðarfjörð ETA seinnapartinn í dag, síðasta höfn var Vestmannaeyjar. Kl.1239 kallað í TFB vegna Akademik S. Vavilov c/s UAUO er ekki á lista yfir erlend skip, einnig er spurt um Dorado c/s YLDD. Kl.1247 kallað í Akademik S. Vavilov c/s UAUO /media/hafis/skyrslur_lhg/hafisskyrsla_18ag2011.pdf

• 59. Adalgeirsdottir-etal-tc-5-961-2011

  (DGPS) equipment in 2001. Continuous profiles, approximately 1 km apart, were measured in the accumulation zone and a dense net- work of point measurements were carried out in the abla- tion zone. Digital Elevation Models (DEMs) of the surface and bedrock were created from these data (Fig. 2; Björns- son and Pálsson, 2004). The estimated errors are at most 1–5 m (bias less than 1 m) for the surface /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 60. 16910025

  BIRK 12:01 12:04 03:26 03:33 820 00:00 00:00 0 00:00 00:00 0 00:00 00:00 0 00:00 00:00 0 00:00 00:00 0 Samtals 03:26 03:33 820 Flugleið: Flugskýrsla TF-SIF 30. nóvember 2010 Flug nr. 16910.025 Texti: Kl.0941, skipaumferð á NA- og A- landi. Kl.0948, kallað í Havfrakt OZ2056 á ch-16. Hann er að koma frá Þórshöfn í Færeyjum og er á leið til Þórshafnar á Langanesi /media/hafis/skyrslur_lhg/16910025.pdf