Snow accumulation and ablation in three forested mountain catchments
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10311996" target="_blank" >RIV/00216208:11310/15:10311996 - 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
Snow accumulation and ablation in three forested mountain catchments
Popis výsledku v původním jazyce
The study was focused on vegetation and topography effects on snow accumulation and ablation, with special interest in the role of the forest affected by the bark beetle (Ips typographus). We selected eight predictors related to winter meteorological conditions and the character of specific localities. The vegetation structure was described using parameters calculated from hemispherical photographs. The degree-day approach was used to calculate melt factors for sites with different vegetation and aspects. Multiple regression was further applied using snow water equivalent (SWE) data measured at 47 localities in winter seasons from 2010 to 2014. The SWE in forest sites was by 32% lower than in open areas. The snow ablation in large openings was on average more than two times faster compared to forest sites. Snow ablation was by 33% faster after forest defoliation (due to the bark beetle) and we expect even faster ablation in case of complete forest decline. The results indicated that to
Název v anglickém jazyce
Snow accumulation and ablation in three forested mountain catchments
Popis výsledku anglicky
The study was focused on vegetation and topography effects on snow accumulation and ablation, with special interest in the role of the forest affected by the bark beetle (Ips typographus). We selected eight predictors related to winter meteorological conditions and the character of specific localities. The vegetation structure was described using parameters calculated from hemispherical photographs. The degree-day approach was used to calculate melt factors for sites with different vegetation and aspects. Multiple regression was further applied using snow water equivalent (SWE) data measured at 47 localities in winter seasons from 2010 to 2014. The SWE in forest sites was by 32% lower than in open areas. The snow ablation in large openings was on average more than two times faster compared to forest sites. Snow ablation was by 33% faster after forest defoliation (due to the bark beetle) and we expect even faster ablation in case of complete forest decline. The results indicated that to
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DA - Hydrologie a limnologie
OECD FORD obor
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Návaznosti výsledku
Projekt
<a href="/cs/project/GA13-32133S" target="_blank" >GA13-32133S: Retenční potenciál pramenných oblastí ve vztahu k hydrologickým extrémům</a><br>
Návaznosti
S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2015
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Acta Hydrologica Slovaca
ISSN
1335-6291
e-ISSN
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Svazek periodika
16
Číslo periodika v rámci svazku
1
Stát vydavatele periodika
SK - Slovenská republika
Počet stran výsledku
9
Strana od-do
208-216
Kód UT WoS článku
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EID výsledku v databázi Scopus
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