ISOTOPES OF OXYGEN-18 AND DEUTERIUM IN PRECIPITATION IN SLOVAKIA

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F12%3A00197294" target="_blank" >RIV/68407700:21110/12:00197294 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.2478/v10098-012-0023-2" target="_blank" >http://dx.doi.org/10.2478/v10098-012-0023-2</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.2478/v10098-012-0023-2" target="_blank" >10.2478/v10098-012-0023-2</a>

Jazyk výsledku

angličtina

Název v původním jazyce

ISOTOPES OF OXYGEN-18 AND DEUTERIUM IN PRECIPITATION IN SLOVAKIA

Popis výsledku v původním jazyce

The article synthesizes available information on isotopic composition of precipitation in Slovakia (the Western Carpathians). Monthly ?18O data from eleven stations and period 1988-1997 were used to investigate correlations among the stations, altitude,air temperature and precipitation amount effects. The mean annual altitude and air temperature gradients of ?18O in precipitation were 0.21permille/100 m and 0.36permille/1°C, respectively. Maps of spatial distribution of mean annual ?18O in precipitation based on both gradients were constructed. The two maps do not significantly differ for the majority of Slovakia. ?2H data were available for only three tations. Local meteoric water line derived for the station with the longest data series (?2H = = 7.86?18O + 6.99) was close to the Global Meteoric Water line. Its parameters in periods 1991-1993 and 1991-2008 did not change. The study indicates that a more detailed monitoring of isotopic composition of precipitation in mountains should

Název v anglickém jazyce

ISOTOPES OF OXYGEN-18 AND DEUTERIUM IN PRECIPITATION IN SLOVAKIA

Popis výsledku anglicky

The article synthesizes available information on isotopic composition of precipitation in Slovakia (the Western Carpathians). Monthly ?18O data from eleven stations and period 1988-1997 were used to investigate correlations among the stations, altitude,air temperature and precipitation amount effects. The mean annual altitude and air temperature gradients of ?18O in precipitation were 0.21permille/100 m and 0.36permille/1°C, respectively. Maps of spatial distribution of mean annual ?18O in precipitation based on both gradients were constructed. The two maps do not significantly differ for the majority of Slovakia. ?2H data were available for only three tations. Local meteoric water line derived for the station with the longest data series (?2H = = 7.86?18O + 6.99) was close to the Global Meteoric Water line. Its parameters in periods 1991-1993 and 1991-2008 did not change. The study indicates that a more detailed monitoring of isotopic composition of precipitation in mountains should

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DA - Hydrologie a limnologie

OECD FORD obor

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Projekt

—

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2012

Kód důvěrnosti údajů

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

Název periodika

Journal of Hydrology and Hydromechanics

ISSN

0042-790X

e-ISSN

—

Svazek periodika

60

Číslo periodika v rámci svazku

4

Stát vydavatele periodika

SK - Slovenská republika

Počet stran výsledku

12

Strana od-do

265-276

Kód UT WoS článku

000312915300005

EID výsledku v databázi Scopus

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