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Long-Term Isotope Records of Precipitation in Zagreb, Croatia (CROSBI ID 68004)

Prilog u knjizi | izvorni znanstveni rad | međunarodna recenzija

Krajcar Bronić, Ines ; Barešić, Jadranka ; Borković, Damir ; Sironić, Andreja ; Lovrenčić Mikelić, Ivanka ; Vreča, Polona Long-Term Isotope Records of Precipitation in Zagreb, Croatia // Use of Water Stable Isotopes in Hydrological Processes / Vreča, Polona ; Kern, Zoltan (ur.). Basel: MDPI Books, 2020. str. 187-214 doi: 10.3390/w12010226

Podaci o odgovornosti

Krajcar Bronić, Ines ; Barešić, Jadranka ; Borković, Damir ; Sironić, Andreja ; Lovrenčić Mikelić, Ivanka ; Vreča, Polona

engleski

Long-Term Isotope Records of Precipitation in Zagreb, Croatia

The isotope composition of precipitation has been monitored in monthly precipitation at Zagreb, Croatia, since 1976. Here, we present a statistical analysis of available long-term isotope data (3H activity concentration, delta2H, delta18O, and deuterium excess) and compare them to basic meteorological data. The aim was to see whether isotope composition reflected observed climate changes in Zagreb: a significant increase in the annual air temperature and larger variations in the precipitation amount. Annual mean delta18O and delta2H values showed an increase of 0.017%o and 0.14%o per year, respectively, with larger differences in monthly mean values in the first half of the year than in the second half. Mean annual d-excess remained constant over the whole long-term period, with a tendency for monthly mean d-excess values to decrease in the first half of the year and increase in the second half due to the influence of air masses originating from the eastern Mediterranean. Changes in the stable isotope composition of precipitation thus resembled changes in the temperature, the circulation pattern of air masses, and the precipitation regime. A local meteoric water line was obtained using different regression methods, which did not result in significant differences between nonweighted and precipitation-weighted slope and intercept values. Deviations from the Global Meteoric Water Line GMWL (lower slopes and intercepts) were observed in two recent periods and could be explained by changes in climate parameters. The temperature gradient of delta18O was 0.33%o/oC. The tritium activity concentrations in precipitation showed slight decreases during the last two decades, and the mean A in the most recent period, 2012–2018, was 7.6 +- 0.8 Tritium Units (TU).

precipitation ; Zagreb ; Croatia ; stable isotope ratios ; 2H/1H and 18O/16O ; deuterium excess ; local meteoric water line ; delta18O–temperature relation ; tritium

rad u knjizi "Use of Water Stable Isotopes in Hydrological Processes" je reprint rada iz časopisa Water, Water 2020, 12, 226; doi:10.3390/w12010226

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Podaci o prilogu

187-214.

objavljeno

10.3390/w12010226

Podaci o knjizi

Use of Water Stable Isotopes in Hydrological Processes

Vreča, Polona ; Kern, Zoltan

Basel: MDPI Books

2020.

978-3-03943-266-0

Trošak objave rada u otvorenom pristupu

Povezanost rada

Fizika, Interdisciplinarne prirodne znanosti, Kemija

Poveznice