A 9-year record of stable isotope ratios of precipitation in Eastern Hungary: Implications on isotope hydrology and regional palaeoclimatology

• Published in: Journal of hydrology (Amsterdam) Vol. 400; no. 1; pp. 144 - 153
• Main Authors: Vodila, G., Palcsu, L., Futó, I., Szántó, Zs
• Format: Journal Article
• Language: English
• Published: Kidlington Elsevier B.V 30.03.2011; Elsevier
• Subjects: Deuterium; Deuterium excess; Earth sciences; Earth, ocean, space; Evaporation; Exact sciences and technology; Hungary; Hydrology; Hydrology. Hydrogeology; Isotopes; Monitoring; Precipitation; Sampling; Secondary evaporation; Stable isotopes; Stations; Temperature correlation; Hungary; Central Europe; Europe; Secondary evaporation; Precipitation; Temperature correlation; Deuterium excess; Hungary; Stable isotopes; stable isotopes; isotope ratios; sampling; hydrogen; slopes; extremities; precipitation; correlation; deuterium; raindrops; temperature; evaporation; oxygen
• DOI: 10.1016/j.jhydrol.2011.01.030
• ISSN: 0022-1694

► Results of 9 years of systematic precipitation sampling and isotope analysis. ► Extrapolation of the data of the surrounding stations to Debrecen is misleading. ► LMWL for the study site was found to be δ 2H = (6.55 ± 0.22) δ 18O–7.74 ± 1.97. ► Deuterium excess shows the effects of secondary evaporation better than δ 18O values. ► The δ 18O–T function has similar slope than that of other continental stations. The stable isotopic composition of hydrogen and oxygen of precipitation from Debrecen, Eastern Hungary was analysed in event-based samples collected from the beginning of 2001 to the end of 2009. During the monitoring period, the δ 18O values varied between −22.3‰ and 6.64‰ and the δ 2H values between −176.8‰ and 10.7‰. The LMWL for the monthly based data is close to the GMWL, but shows the effect of secondary evaporation of falling raindrops with lower intercept and slope. LMWL of each year shows highly different parameters due to differences in precipitation amount and summer temperatures, especially in the extreme years of 2002 and 2003. On the basis of our data, deuterium excess is considered to be the best parameter to reveal the extremities of dry and warm periods. Deuterium excess also proved to be a useful tool to show the different formation histories of certain precipitation events. Good correlation of δ 18O with temperature was obtained for the samples. The slope of the δ 18O–T functions for the whole sampling period was 0.32 ± 0.03‰/°C for the monthly samples, however, a slope of 0.37 ± 0.03‰/°C was obtained if monthly mean temperatures were replaced with the monthly mean temperatures of the rainy days. Considering the temperature dependency of the δ 18O values in the past, it can be concluded that Δ δ 18O/ΔT relationship using monthly mean temperatures of the rainy days might be a better approach than monthly mean temperatures.