Factors controlling stable isotopes variability in precipitation in Syria: Statistical analysis approach

Journal of earth system science

Zuhair Kattan^1¹ 

[1] Department of Geology, Atomic Energy Commission of Syria (AECS), P.O. Box 6091, Damascus, Syrian Arab Republic.^1

关键词: Hydrology;    environmental isotopes;    stable isotopes;    precipitation;    rainfall;    Syria;   

DOI  :  

学科分类：天文学(综合)

来源: Indian Academy of Sciences

【 摘 要 】

The major characteristics of the stable isotopes ($^{18}$O and $^{2}$H) and deuterium excess (d-excess or d) of rainfall samples collected from 16 stations during two periods (1989–1993 and 2003–2006) were statistically analysed to understand the factors controlling the temporal and spatial isotope variability in precipitation (P) in Syria. Rainfall waters at the mountainous regions are remarkably the most depleted in heavy stable isotopes, with also high d-excess values (d>20 per thousand). The enriched rainfall waters (lower d-excess values), mostly referring to coastal and some inland areas, are subject to the evaporation of falling raindrops. Rainfalls at the southern stations have impressively the highest d-excess values (d > 22 per thousand), likely because of intensive interactions with the Mediterranean Sea (MS) moistures. The temperature (T) effect, shown by an average $\delta^{18}$O gradient of $\approx$0.34 $\pm$ 0.03 per thousand/$^{\circ}$C, is very close to the Global Network for Isotopes in Precipitation value (0.3 per thousand/$^{\circ}$C). The altitude effect, represented by a $\delta^{18}$O gradient of −0.18 $\pm$ 0.03 per thousand/100 m, fits well with the range given for most Mediterranean countries. Relative humidity (RH) and P-amount effects are characterised by an isotopic depletion, with a notable rise in the d-excess value with P and RH increases. The seasonal effect is shown by depleted $\delta^{18}$O and $\delta^{2}$H values during December–February and enriched $\delta^{18}$O and $\delta^{2}$H values at the end of April, with frequently low d-excess values (<8 per thousand). T parameter seems to be the major factor that strongly controls the variability of the stable isotope compositions of P in Syria. The moisture from the MS and secondary evaporation conjunctly play additional roles, but of less importance than the T effect.

【 授权许可】

CC BY