Accuracy of Manual Snow Sampling, Depending on the Sampler's Cross-Section-A Comparative Study
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F23%3A97484" target="_blank" >RIV/60460709:41330/23:97484 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.3390/geosciences13070205" target="_blank" >http://dx.doi.org/10.3390/geosciences13070205</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.3390/geosciences13070205" target="_blank" >10.3390/geosciences13070205</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Accuracy of Manual Snow Sampling, Depending on the Sampler's Cross-Section-A Comparative Study
Popis výsledku v původním jazyce
Snow sampling, either by inserting a tube through the entire snowpack or by taking samples from the vertical profile, is widely applied to measure the snow depth, density, and snow water equivalent (SWE). A comparative study of snow-sampling methods was carried out on 24 March 2022 in Sodankyla, Finland. Six groups from five countries (Estonia, Finland, Greenland, Iceland, and Sweden) participated, using 12 different snow samplers, including 9 bulk tube samplers and 3 density cutters. The cross-sectional area of the SWE samplers varied from 11 to 100 cm(2), while tube length varied from 30 cm to 100 cm. The cross-sectional area of the density profile cutters varied from 100 cm(2) to 200 cm(2) and the vertical sampling step varied from 5 cm to 10 cm. The samples were taken from snow pits in 55-65-centimeter-deep snow cover in a flat area with sparse pine trees, with the pits at a maximum distance of 10 m from each other. Each tube sampling series consisted of 3-10 vertical columns to ensure statistical validation. The snowpack was relatively soft, with two moderately hard crust layers. The density recorded in the tube sample measurements varied from 218 to 265 kgm(-3). The measurement results of SWE, however, varied depending on the sampling equipment used, ranging from 148 to 180 kgm(-2), with two outliers of 77 and 106 kgm(-2), both with 11 cm(2) samplers.
Název v anglickém jazyce
Accuracy of Manual Snow Sampling, Depending on the Sampler's Cross-Section-A Comparative Study
Popis výsledku anglicky
Snow sampling, either by inserting a tube through the entire snowpack or by taking samples from the vertical profile, is widely applied to measure the snow depth, density, and snow water equivalent (SWE). A comparative study of snow-sampling methods was carried out on 24 March 2022 in Sodankyla, Finland. Six groups from five countries (Estonia, Finland, Greenland, Iceland, and Sweden) participated, using 12 different snow samplers, including 9 bulk tube samplers and 3 density cutters. The cross-sectional area of the SWE samplers varied from 11 to 100 cm(2), while tube length varied from 30 cm to 100 cm. The cross-sectional area of the density profile cutters varied from 100 cm(2) to 200 cm(2) and the vertical sampling step varied from 5 cm to 10 cm. The samples were taken from snow pits in 55-65-centimeter-deep snow cover in a flat area with sparse pine trees, with the pits at a maximum distance of 10 m from each other. Each tube sampling series consisted of 3-10 vertical columns to ensure statistical validation. The snowpack was relatively soft, with two moderately hard crust layers. The density recorded in the tube sample measurements varied from 218 to 265 kgm(-3). The measurement results of SWE, however, varied depending on the sampling equipment used, ranging from 148 to 180 kgm(-2), with two outliers of 77 and 106 kgm(-2), both with 11 cm(2) samplers.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10511 - Environmental sciences (social aspects to be 5.7)
Návaznosti výsledku
Projekt
—
Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2023
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Geosciences (Schwitzerland)
ISSN
2076-3263
e-ISSN
2076-3263
Svazek periodika
13
Číslo periodika v rámci svazku
7
Stát vydavatele periodika
CH - Švýcarská konfederace
Počet stran výsledku
10
Strana od-do
1-10
Kód UT WoS článku
001035952700001
EID výsledku v databázi Scopus
2-s2.0-85166315277