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Results:

• 51. norsem_michalek

  was deployed and together with the permanent NNSN stations in that area it contained 33+ stations within span 350 x 200 km. About 1250 earthquakes of M>0.0 was recorded during the project period and new map of seismicity of that area was retrieved. The main aim of the project is to reveal the stress field in that particular region and therefore determination of stable /media/norsem/norsem_michalek.pdf

• 52. Paper-Olafur-Rognvaldsson_91

  climate models is that the simulations are dependent on the lateral boundary conditions. These can constrain the model dynamics and hence affect the results (e.g. Warner et al., 1997). To minimize the constraining effects of the boundary conditions, Qian et al. (2003) suggested consecutive short term integration, overlapping in time as to minimize the effects of spin-up, instead of a single long term /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 53. CES_D2.4_task1

  NO +62:34:01 +11:23:00 628 TP 1041 KONGSBERG IV NO +59:39:47 +09:39:00 168 TP 1042 LYNGOR FYR NO +58:38:00 +09:09:01 4 T 1043 TVEITSUND NO +59:01:37 +08:31:14 252 TP 1044 LINDESNES FYR NO +57:58:59 +07:02:53 13 TP 1045 LISTA FYR NO +58:06:36 +06:34:05 14 TP 1046 SOLA /media/ces/CES_D2.4_task1.pdf

• 54. VI_2009_006_tt

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 55. The Icelandic glaciers weighed from space

  glacier down­wasting indicated by the traditional mass balance measurements that show that the volume of the glaciers has been reduced by more than 200 km³ in total since 1995, see fig. 3, as described in a new scientific publication in the journalGeophysical Journal International . Since the measurements determine changes in the total mass of the glaciers, one may say that the glaciers have /about-imo/news/the-icelandic-glaciers-weighed-from-space

• 56. 2013_001_Nawri_et_al

  values. For Part 2, data files describing the local wind statistics on the regular model grid covering Iceland are made available through an online wind atlas (follow the link from http://www.vedur.is/vedur/vedurfar/vindorka/). The files contain estimates of Weibull parameters at each grid point, for twelve wind direction sectors, five heights (10, 25, 50, 100, 200 m above ground level (mAGL /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 57. The weather in Iceland in 2050

  stocks. The acidification of the ocean may also adversely impact ocean food webs, with possible consequences on fisheries. Iceland's ice caps have been melting and will continue to do so. According to scientific estimate, they will almost disappear in the next 200 years. Many of these changes can already be seen, for instance: The tiny ice cap Ok, west of Langjökull, has changed beyond /about-imo/news/nr/2989

• 58. Instructions for weather radar pages

  the earth's surface. At a distance of 200 km from the weather radar the laser beam does not detect signals which are under 4000 m from the earth's surface. Low clouds, for example fog clouds, close to the weather radar do not appear on the image; they lie so close to the earth's surface that they are not detected. The utility of these images is most when monitoring precipitation from the south /weather/articles/nr/1221

• 59. Daily_status_report_200814

  cloud. Lightning No eruption and no eruption cloud. Noise No eruption and no eruption cloud. Meltwater No eruption. Daily measurements of water samples from Upptyppingar on Jökulsá á Fjöllum have shown a stable conductivity of 200 µS/cm since Sunday. Conditions at eruption site No eruption. Seismic tremor No sign of harmonic (volcanic) tremor detected. Earthquakes The earthquake swarm that began on 16 /media/jar/Daily_status_report_200814.pdf

• 60. Eyjafjallajokull_status_2010-04-26_IES_IMO

  observations. Radar images show continuous build-up of a tephra crater/cone in the northern ice cauldron. The diameter of the crater is 200 m and the height of the crater cone is 150 +- 20 m. Seismic tremor: Intensity comparable to the last three days of eruptive activity Earthquakes: Ml 1.7 earthquake detected ~8 km east of the eruption at 16:18 GMT GPS deformation: Horizontal displacement towards /media/jar/Eyjafjallajokull_status_2010-04-26_IES_IMO.pdf