Spatial and temporal variability of stable water isotopes in snow related hydrological processes

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F13%3A00213837" target="_blank" >RIV/68407700:21110/13:00213837 - isvavai.cz</a>

Result on the web

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DOI - Digital Object Identifier

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Result language

angličtina

Original language name

Spatial and temporal variability of stable water isotopes in snow related hydrological processes

Original language description

We monitored variability of ?18O and ?2H in the snow-related part of a hydrological cycle (snowfall, snow cover, snowmelt, soil water, groundwater and streams) in mountain catchments of northern Slovakia in winters 2011 and 2012. Unexpected negative altitude gradients of ?180 and ?2H were found for almost all snowfalls. The isotopic composition of snow cover during a snow-poor winter was spatially more variable than during a snow-rich winter. Light snow water was visible in the soils (at depths of 51-71cm) at least until the middle of June. Isotopic signals of snowmelt water significantly depended on the device used to collect the water samples. The isotopic composition of streams of different orders during snowmelt periods pointed out the different regimes of the snowmelt in the main river valley and in the mountains.

Czech name

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Czech description

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Type

J_x - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

CEP classification

DA - Hydrology and limnology

OECD FORD branch

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Project

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Continuities

Z - Vyzkumny zamer (s odkazem do CEZ)

Publication year

2013

Confidentiality

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Name of the periodical

Die Bodenkultur

ISSN

0006-5471

e-ISSN

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Volume of the periodical

64

Issue of the periodical within the volume

3-4

Country of publishing house

AT - AUSTRIA

Number of pages

7

Pages from-to

39-45

UT code for WoS article

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EID of the result in the Scopus database

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