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


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  • 1. VI_2020_005

    ). Since the tide gauges measure the ocean elevation relative to a point on land, vertical land motion needs to be taken into account when estimating sea surface changes (Hamlington and Thompson, 2016; Quante and Colijn, 2016). The land motion can be caused by natural processes, such as glacial isostatic adjustments or tectonics, and/or anthropogenic processes, for instance land subsidence due /media/vedurstofan-utgafa-2020/VI_2020_005.pdf
  • 2. Protective measures

    to the "Adaptation of the Swiss Guidelines for supporting structures for Icelandic conditions (IMO Rep. 99013)" (IMO Memo TóJ-2003-05, author T. Jóhannesson) (pdf 0.03 Mb) Remarks on the design of avalanche braking mounds based on experiments in 3, 6, 9 and 34 m long chutes (IMO Int. Rep. 03024, 2003, authors T. Jóhannesson and Kr. M. Hákonardóttir) (pdf 0.8 Mb) Field observations and laboratory /avalanches/imo/protective/
  • 3. glacier_mass_balance_poster

    2LEGOS, Toulouse, France 3National Space Institute, Technical University of Denmark, Lyngby, Denmark Abstract. We assess the mean mass balance of three ice caps in South Iceland, for two periods, 1980 to 1998 and 1998 to 2004, by comparing digital elevation models (DEMs) covering the entire glaciers; Eyjafjallajökull (81 km2), Tindfjallajökull (15 km2) and Torfajökull (14 km2). The DEMs were /media/ces/glacier_mass_balance_poster.pdf
  • 4. Crochet_Philippe_CES_2010

    characteristics » Annual maximum » Snow cover duration • Daily snowmelt rates » Annual maxima • Daily glacial melt rates » Annual maxima » Duration of melting period 25% warmest years 25% coldest years 1971-2000 - Direct runoff rivers - Spring-fed rivers - Glacial rivers (5) - Lakes 11 River basins Size: 42 km2 – 5687 km2 Mean elevation: 163 m – 863 m Data • Discharge measurements (daily) (1929 /media/ces/Crochet_Philippe_CES_2010.pdf
  • 5. ces-glacier-scaling-memo2009-01

    balance perturbations in climate change runs are typically on the order of 1 ma 1 so that over a period of a few or several decades, the ice surface may be lowered by several tens of metres. A lowering of that magnitude will start to affect the air temperature over the glacier and leads to an intensification of surface melting through the mass- balance–elevation feedback. Based on the preceding /media/ces/ces-glacier-scaling-memo2009-01.pdf
  • 6. Hazard zoning

    takes place on two vents along the fissure, the northernmost part of the rampart and from the central part of the rampart. These two sources merge into one plume. Downwind, dense volcanic gases separate and descend. Further downwind a second plume, rich in water vapour, reaches higher elevation than the first plume /pollution-and-radiation/volcanic-gas/hazard-zoning/bigimg/3042
  • 7. News

    2010, as seen at 12:00 GMT at an elevation of 3-3.6 km (10-12,000 ft). Light coloured, low-lying clouds of steam were observed over the eruption site, together with occasional bursts of grey to black-coloured cloud, which rise to up to half of the total height of the eruption plume. Above this level, the plume was lighter in colour with a capping of white cloud (not visible here /about-imo/news/bigimg/1891
  • 8. Articles

    the lake, reaching up to 20–30 m elevation above the water level and even higher in places. Search Search string /avalanches/articles/bigimg/2929
  • 9. Glacier mapping – IPY

    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, Eyjafjallajökull, Drangajökull, Tungnafellsjökull and several other smaller glaciers. A total of 11,000 km² glaciers have been mapped in this effort, but the total measured area exceeds 15,000 /about-imo/arctic/glacier-mapping-ipy/
  • 10. Glacier mapping – IPY

    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, Eyjafjallajökull, Drangajökull, Tungnafellsjökull and several other smaller glaciers. A total of 11,000 km² glaciers have been mapped in this effort, but the total measured area exceeds 15,000 /about-imo/arctic/glacier-mapping-IPY/

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