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70 results were found for 联系TG电报(duo788)超级签名 ios企业签-超级签-苹果TF签.pba.


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  • 31. TF-FMS_20141204_skyrsla

    niðurstöður: Flogið var frá Reykjavíkurflugvelli með TF-FMS og var flugtak kl. 14. Tilgangurinn var að fljúga línur yfir Bárðarbungu og hið nýja Nornahraun sem og að fylgjast með hegðun gosmakkar og gasdreifingu. Suðvestanátt var ríkjandi frá yfirborði og upp úr, fremur hæg en um 25 hnútar yfir Bárðarbungu. Þegar mökkurinn sást fyrst frá Bárðarbungu leit hann út fyrir /media/jar/TF-FMS_20141204_skyrsla.pdf
  • 32. Factsheet-Bardarbunga-140904

    although this interpretation has currently not been confirmed by other observations.  There are no signs of a subglacial eruption under Dyngjujökull. No obvious changes such as increased water flow or cauldrons on the glacier surface were observed from scientists on board TF-SIF yesterday. Water meters in Jökulsá á Fjöllum do not show any unusual changes in discharge and electric /media/jar/Factsheet-Bardarbunga-140904.pdf
  • 33. HaBj_PlumePictures_w_explanations-20140901

    Photos of the eruption plume taken on September 1st 2014 Halldór Björnsson, Icelandic Meteorological Office. TF-SIF an airplane from the Icelandic Coast Guard flew over the volcano and nearby areas in the north of Vatnajökull on September 1st from kl. 13:45 to 16:30. Despite relatively cloudy conditions, the visibility was acceptable, especially at low altitude. This document discusses several /media/jar/myndsafn/HaBj_PlumePictures_w_explanations-20140901.pdf
  • 34. Bárðarbunga and Holuhraun - overview

    What is Bárðarbunga? - including a chapter from the Catalogue of Icelandic Volanoes (in progress) The FutureVolc project and the eruption on National Geographic A glimpse into the field Hard work in harsh circumstances A reconnaissance flight with TF-SIF Seismic activity still great Updated summary from Bárðarbunga Summary of activity in Bárðarbunga Seismic activity /earthquakes-and-volcanism/articles/nr/2947
  • 35. The Bárdarbunga/Holuhraun eruption 2014-2015

    from the lavaWarning banners removed2014The segmented dyke intrusion explainedWhat is Bárðarbunga? - including a chapter from the Catalogue of Icelandic Volanoes (in progress) The FutureVolc project and the eruption on National GeographicA glimpse into the fieldHard work in harsh circumstancesA reconnaissance flight with TF-SIFSeismic activity still greatUpdated summary from BárðarbungaSummary /volcanoes/about-volcanoes/bardarbunga/the-bardarbungaholuhraun-eruption/
  • 36. Bárðarbunga and Holuhraun - overview

    What is Bárðarbunga? - including a chapter from the Catalogue of Icelandic Volanoes (in progress) The FutureVolc project and the eruption on National Geographic A glimpse into the field Hard work in harsh circumstances A reconnaissance flight with TF-SIF Seismic activity still great Updated summary from Bárðarbunga Summary of activity in Bárðarbunga Seismic activity /earthquakes-and-volcanism/articles/nr/2947/
  • 37. Grímsvötn 2010

    Office and the Institute of the Earth Sciences, University of Iceland, 4 November 2010 at 17:00. Aerial view The following photographs were taken 3rd November during scientific flight with the Icelandic Coast Guard (TF-SIF): Matthew J. Roberts and Egill Axelsson, Icelandic Meteorological Office. Skeiðarárjökull Aerial view of debris-laden floodwater flowing along the terminus /hydrology/articles/nr/2040
  • 38. Grímsvötn 2010

    Office and the Institute of the Earth Sciences, University of Iceland, 4 November 2010 at 17:00. Aerial view The following photographs were taken 3rd November during scientific flight with the Icelandic Coast Guard (TF-SIF): Matthew J. Roberts and Egill Axelsson, Icelandic Meteorological Office. Skeiðarárjökull Aerial view of debris-laden floodwater flowing along the terminus /earthquakes-and-volcanism/articles/nr/2040
  • 39. Factsheet_Bardarbunga_20150130

    January 21st blue line). The graph is based primarily on measurements from surveillance flights by the ISAVIA plane TF-FMS. There is quite some uncertainty in individual measurements but there is a definite trend showing diminishing lava flow rates. The red and pink lines show the increase of the volume of the subsidence of the Bardarbunga caldera, these values are derived with similar methods /media/jar/Factsheet_Bardarbunga_20150130.pdf
  • 40. Isskyrsla_20100407

    Ísskýsla 7.apríl Flug 03410.025 Miðvikudaginn 7 apríl var farið í ískönnunarflug á TF-SIF úti fyrir vestfjörðum. Kl.1115 var komið að ísröndini sem lá til NA um eftirtalda staði: 1. N65°50'- W028°05' 2. N65°44' -W027°49 ' 3. N65°56'- W027°08' 4. N66°12' -W026°21' 5. N66°31'- W025°57' 6. N66°43'- W025°49' 7. N66°40'- W025°24' 8. N67°05'- W024°32' 9. N67°14' -W023°56' 10.N67°19'- W023°32' 11.N67°40 /media/hafis/skyrslur_lhg/Isskyrsla_20100407.pdf

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