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Description
  • Heavy snowfall in the High Tatras at the end of March 2009 was the cause of several avalanche falls in the Žiarská valley of the Slovakian High Tatras Mountains. The resulting avalanche field was almost 28 ha. The event was classified as a centennial avalanche, one of the biggest in modern history in Central Europe. Snow pack was measured by accurate differential GPS technology. Snow depth and avalanche field volume were calculated using a comparison between avalanche and terrain surfaces. Considering the inaccuracies of the photogrammetric digital elevation model, most likely caused by vegetation, new terrain surveying was required after the snow pack melted in October 2009. The results confirmed that deep snow packs even in rugged terrain can be accurately surveyed by GPS technology.
  • Heavy snowfall in the High Tatras at the end of March 2009 was the cause of several avalanche falls in the Žiarská valley of the Slovakian High Tatras Mountains. The resulting avalanche field was almost 28 ha. The event was classified as a centennial avalanche, one of the biggest in modern history in Central Europe. Snow pack was measured by accurate differential GPS technology. Snow depth and avalanche field volume were calculated using a comparison between avalanche and terrain surfaces. Considering the inaccuracies of the photogrammetric digital elevation model, most likely caused by vegetation, new terrain surveying was required after the snow pack melted in October 2009. The results confirmed that deep snow packs even in rugged terrain can be accurately surveyed by GPS technology. (en)
Title
  • Using GPS for snow depth and volume measurement of centennial avalanche field in High Tatras
  • Using GPS for snow depth and volume measurement of centennial avalanche field in High Tatras (en)
skos:prefLabel
  • Using GPS for snow depth and volume measurement of centennial avalanche field in High Tatras
  • Using GPS for snow depth and volume measurement of centennial avalanche field in High Tatras (en)
skos:notation
  • RIV/62156489:43410/11:00161237!RIV11-MSM-43410___
http://linked.open...avai/predkladatel
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • Z(MSM6215648902)
http://linked.open...iv/cisloPeriodika
  • 3
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 237342
http://linked.open...ai/riv/idVysledku
  • RIV/62156489:43410/11:00161237
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • The High Tatras; Avalanche field; GNSS; Differential GPS (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CA - Kanada
http://linked.open...ontrolniKodProRIV
  • [6BAAE4264AA4]
http://linked.open...i/riv/nazevZdroje
  • Cold Regions Science and Technology
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 65 (2011)
http://linked.open...iv/tvurceVysledku
  • Klimánek, Martin
  • Janata, Přemysl
  • Mikita, Tomáš
  • Cibulka, Miloš
  • Lizuch, Milan
http://linked.open...n/vavai/riv/zamer
issn
  • 0165-232X
number of pages
http://localhost/t...ganizacniJednotka
  • 43410
is http://linked.open...avai/riv/vysledek of
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