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65 results were found for 立博中文版 - ladbrokes立博中文版 tf-aa.com.


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  • 21. Isskyrsla_20100116

    Reykjavík 16. janúar 2010. Til: Veðurstofu Íslands. Frá: Landhelgisgæslu Íslands. Efni: Hafískönnun 16. janúar 2010. Laugardaginn 16. janúar 2010 fór þyrla landhelgisgæslunar TF-EIR í gæslu og ískönnunarflug. Var flogið norður Húnaflóann og fyrir vestfirðina. Einn stakur ísjaki sást í Húnaflóanum á stað : 66°12,7‘N – 21°16,3‘V Komið var að ísröndinni út af Húnaflóa og henni fylgt til vesturs um /media/hafis/skyrslur_lhg/Isskyrsla_20100116_rett.pdf
  • 22. Eyjafjallajokull_status_2010-04-29_IES_IMO

    from the local police; and aerial observations from a scientific flight with the Icelandic Coastguard (observation plane TF-SIF). Eruption plume: Height (a.s.l.): Not visible above clouds at 3.6–5.1 km (12–17,000 ft), but most likely below 3.6 km (12,000 ft). Before the overflight this morning, the eruption plume was not seen on radar images from Keflavík, nor on satellite /media/jar/Eyjafjallajokull_status_2010-04-29_IES_IMO.pdf
  • 23. Eyjafjallajokull_status_2010-05-01_IES_IMO

    scientists at Gígjökull; aerial observations from two scientific overflights: TF-SIF (10:30–11:00 GMT) and Eagle Air (16:40–17:15 GMT). Eruption plume: Height (a.s.l.): TF-SIF observations at 10:30 GMT confirmed an ash plume rising to 4– 5.4 km (13–18,000 ft) near to Eyjafjallajökull. Clouds of ash at lower elevations observed drifting south-east of the eruption site. No verifiable /media/jar/Eyjafjallajokull_status_2010-05-01_IES_IMO.pdf
  • 24. Grimsvotn_status_2010-11-03_IES_IMO

    Coastguard (TF-SIF). Meltwater: Water continues to drain from Grímsvötn. At 09:30 GMT today, discharge was gauged at 2,600 m3/s on the Gígja river. Electrical conductivity has increased to 560 µS/cm. Conductively levels in the Súla river are similar, indicating that a small volume of geothermal water is draining from the western side of the Skeiðarárjökull glacier /media/vatnafar/flod/Grimsvotn_status_2010-11-03_IES_IMO.pdf
  • 25. Hard work in harsh circumstances

    to leave the relevant area. No visible changes were seen when the Icelandic Coast Guard airplane TF-SIF flew over the area this afternoon with representatives from the Civil Protection and experts from the Icelandic Met Office and the Institute of Earth Sciences. Data from radars and web-cameras is being received, showing no signs of changes at the surface. The estimate is that 150-400 meters of ice /about-imo/news/nr/2960
  • 26. The low frequency tremor 23rd August 2014

    No other corraborating signals of magma reaching the surface were observed on other monitoring systems. Observations from the Coast Guard aircraft, TF-SIF, as well as electrical conductivity measurements from IMO's hydrological monitoring network, showed no signs of activity. The scientists' conclusion was that magma did not arrive at the surface under the glacier that day; no sub-glacial eruption had /earthquakes-and-volcanism/articles/nr/2970
  • 27. Eyjafjallajokull_status_2010-05-20_IES_IMO

    to cloudy weather. Radar images from TF-SIF show no major changes in the ice cauldrons where the cinder cone is forming. The eruption is mainly explosive and almost no lava flows down Gígjökull. Seismic tremor: Volcanic tremor is fairly steady and similar to that of the last few days. Earthquakes: Two microearthquakes have been recorded in the volcano since midnight, at depths /media/jar/Eyjafjallajokull_status_2010-05-20_IES_IMO.pdf
  • 28. 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
  • 29. 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
  • 30. 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

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