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98 results were found for 에이루트매수▣WWW༝S77༝KR▣濫에이루트무상증자抷에이루트분석譗에이루트실적ѷ🍷elevation/.


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  • 11. Glacier mapping – IPY

    have been working on mapping the ice with airborne laser measurement (LiDAR) since 2008. By the summer of 2012 all glaciers larger than 10 km² had been measured, and the analysis of the results will be finished before the end of 2013. Accurate elevation models based on these measurements will be available from Vatnajökull, Hofsjökull, Langjökull, Eiríksjökull, Snæfellsjökull, Mýrdalsjökull /about-imo/arctic/glacier-mapping-ipy/
  • 12. Glacier mapping – IPY

    have been working on mapping the ice with airborne laser measurement (LiDAR) since 2008. By the summer of 2012 all glaciers larger than 10 km² had been measured, and the analysis of the results will be finished before the end of 2013. Accurate elevation models based on these measurements will be available from Vatnajökull, Hofsjökull, Langjökull, Eiríksjökull, Snæfellsjökull, Mýrdalsjökull /about-imo/arctic/glacier-mapping-IPY/
  • 13. Eyjafjallajokull_status_2010-04-26_IES_IMO

    Eruption in Eyjafjallajökull Status Report: 18:00 GMT, 26 April 2010 Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland Compiled by: MJR / GNP / BO / FS Based on: IMO seismic monitoring; IES-IMO GPS monitoring; IMO river gauges; information from local police and IES geologists inspection of tephra Eruption plume: Height (a.s.l.): Mean elevation of 4.8 km /media/jar/Eyjafjallajokull_status_2010-04-26_IES_IMO.pdf
  • 14. Reykholt-abstracts

    ....................................................................................... 16 Mass balance and volume changes of Eyjafjallajökull ice cap, from 1984 to 2010, deduced by multi-temporal elevation maps Victoria H. Hamilton Morris ................................................................................................. 17 Construction and analysis of lidar mosaics of sea ice floe /media/vatnafar/joklar/Reykholt-abstracts.pdf
  • 15. Hock_Regine_CES_2010rs

    et al., 2005) Data Climate data, calibration period Monthly air temperature: ERA-40 reanalysis (0.5°×0.5°), 1958-2001 Monthly precipitation: Precipitation climatology VASClimO, 1951-2000, 0.5°×0.5° (Beck et al., 2005) Elevation-dependent mass balance data for individual glaciers Mass-balance data Data Climate data, calibration period Monthly air temperature: ERA-40 reanalysis /media/ces/Hock_Regine_CES_2010rs.pdf
  • 16. Gudmundsson-etal-2011-PR-7282-26519-1-PB

    ; Eyjafjallajo¨kull; Torfajo¨kull; Tindfjallajo¨kull. Correspondence Sverrir Gudmundsson, Institute of Earth Sciences, University of Iceland, Sturlugata 7, Askja, Reykjavı´k IS-101, Iceland. E-mail sg@raunvis.hi.is Abstract We assess the volume change and mass balance of three ice caps in southern Iceland for two periods, 19791984 to 1998 and 1998 to 2004, by comparing digital elevation models (DEMs /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
  • 17. The

    eruption site. SO2 emissions give a strong indication of magma degassing.Measurements of the elevation of the ice over Grímsvötn made by IES show that it has risen 10 m steadily since last winter. It has not been higher since October 2010. A glacial flood from under the ice cap is therefore considered to be likely during this summer or autumn. In 2004, 1934 and 1922 volcanic eruptions started /about-imo/news/the-civil-protection-scientific-advisory-board-meets-to-discuss-the-status-of-grimsvotn
  • 18. Avalanche bulletin - Eastfjords

    ; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px); */ /* Not supported in IE11 */ } .elev-bottom .mask { clip-path: url(#bottom); /* clip-path: inset(115px 0px 0% round 0px);*/ /* Not supported in IE11 */ } .elev-top .mask { clip-path: url(#top); /* clip /avalanches/forecast/east_fjords
  • 19. Avalanche bulletin - Northern Westfjords

    ; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px); */ /* Not supported in IE11 */ } .elev-bottom .mask { clip-path: url(#bottom); /* clip-path: inset(115px 0px 0% round 0px);*/ /* Not supported in IE11 */ } .elev-top .mask { clip-path: url(#top); /* clip /avalanches/forecast/northern_westfjords
  • 20. Avalanche bulletin - Southwest corner

    ; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px); */ /* Not supported in IE11 */ } .elev-bottom .mask { clip-path: url(#bottom); /* clip-path: inset(115px 0px 0% round 0px);*/ /* Not supported in IE11 */ } .elev-top .mask { clip-path: url(#top); /* clip /avalanches/forecast/southwest_corner

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