Using GPS for snow depth and volume measurement of centennial avalanche field in High Tatras
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43410%2F11%3A00161237" target="_blank" >RIV/62156489:43410/11:00161237 - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Using GPS for snow depth and volume measurement of centennial avalanche field in High Tatras
Popis výsledku v původním jazyce
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.
Název v anglickém jazyce
Using GPS for snow depth and volume measurement of centennial avalanche field in High Tatras
Popis výsledku anglicky
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.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
EH - Ekologie – společenstva
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
Z - Vyzkumny zamer (s odkazem do CEZ)
Ostatní
Rok uplatnění
2011
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Cold Regions Science and Technology
ISSN
0165-232X
e-ISSN
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Svazek periodika
65 (2011)
Číslo periodika v rámci svazku
3
Stát vydavatele periodika
CA - Kanada
Počet stran výsledku
9
Strana od-do
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Kód UT WoS článku
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EID výsledku v databázi Scopus
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