Isotopic composition of precipitation in Poland: a 44-year record

• Published in: Acta Geophysica
• Main Authors: Duliński, Marek, Różański, Kazimierz, Pierchała, Anna, Gorczyca, Zbigniew, Marzec, Michał
• Other Authors: Ministry of Science and Higher Education, National Science Centre
• Format: Article in Journal/Newspaper
• Language: English
• Published: Springer Science and Business Media LLC 2019
• Subjects: Geophysics; North Atlantic; North Atlantic oscillation
• Online Access: http://dx.doi.org/10.1007/s11600-019-00367-2; http://link.springer.com/content/pdf/10.1007/s11600-019-00367-2.pdf; http://link.springer.com/article/10.1007/s11600-019-00367-2/fulltext.html

Abstract Isotopic composition of precipitation ( 2 H /1 H and 18 O/ 16 O isotope ratios, tritium content) is nowadays widely used in numerous applications of environmental isotopes—most notably in hydrology, climatology and biogeochemistry. Here we present a long record (44 years) of stable isotope composition and tritium content in monthly precipitation available for the Krakow station (southern Poland). Krakow is the only site in Poland for which long-term record of the isotopic composition of monthly precipitation is available. The tritium data are discussed here in the context of generally declining levels of bomb tritium in the global atmosphere and growing influence of technogenic emissions of this isotope. Two aspects of temporal variability of stable isotope composition of precipitation collected in Krakow are discussed here: (i) seasonality and (ii) interannual changes of δ 18 O and δ 2 H signal. Whereas the seasonality of stable isotope signal is generated mainly by seasonally varying the degree of rainout of air masses bringing moisture from the source regions (subtropical Atlantic Ocean) to the centre of the European continent, the North Atlantic Oscillation seems to govern interannual changes of δ 18 O and δ 2 H on the decadal timescale. Progressing warming of the local atmosphere, in the order of 1.8 °C in the past four decades, leaves its imprint in stable isotope signal measured in Krakow precipitation; the slope of isotope–temperature relationship is in the order of 0.50‰/°C for δ 18 O and 3.5‰/°C for δ 2 H.