Spatial Mapping of Atmospheric Precipitation Isotopes in Syria

Stable isotope ratios (δ2H and δ18O), tritium (3H). and deuterium excess (d-excess) values of atmospheric precipitation (P) at 16 stations were determined for mapping the spatial variation of oxygen and hydrogen P isotopes in Syria. The major geographical parameters (longitude east, LE; latitude...

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Main Author: Zuhair Kattan
Format: Article
Language:English
Published: Asian Association for Atmospheric Environment 2021-06-01
Series:Asian Journal of Atmospheric Environment
Subjects:
Online Access:https://doi.org/10.5572/ajae.2021.009
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spelling doaj-71acecf330ce4c57a7714f4a4919012a2021-06-30T01:10:52ZengAsian Association for Atmospheric EnvironmentAsian Journal of Atmospheric Environment1976-69122287-11602021-06-0115211510.5572/ajae.2021.009Spatial Mapping of Atmospheric Precipitation Isotopes in SyriaZuhair Kattan0Department of Geology, Atomic Energy Commission of Syria (AECS), Damascus, SyriaStable isotope ratios (δ2H and δ18O), tritium (3H). and deuterium excess (d-excess) values of atmospheric precipitation (P) at 16 stations were determined for mapping the spatial variation of oxygen and hydrogen P isotopes in Syria. The major geographical parameters (longitude east, LE; latitude north, LN; altitude, H; and inland distance from the coast, DFC) were used to find out the best fitting models for the spatial mapping of atmospheric P isotopes in Syria. The highest correlation coefficients (r>0.73) were found for the relationships δ18O-H and δ2H-H. The impacts of LE and LN factors were rather moderate (0.3<r<0.6). However, a high correlation coefficient (r>0.7) was found for the relationship d-excess-LN. The increase of d-excess value from 23‰ to 24‰ in southern Syria is due to the Mediterranean Sea (MS) moisture, likely as a high percentage (>65%) of prevailed winds usually comes over the MS. The concentrations of 3H in P samples (4-14 TU) during the period 1989-1993 were higher than those (3-10 TU) for the period 2004-2006, indicating thus a return back toward the levels of typical 3H production in nature. The high correlation coefficients (r>0.59) that were found for the relationships 3H-DFC and 3H-LE, suggest a continuous exchange between the low tritium moisture from the MS and the higher tritium moisture from the inland areas. Produced gridded isotopic values are quite satisfactory for covering certain areas in Syria and the neighboring Arab countries.https://doi.org/10.5572/ajae.2021.009precipitationenvironmental isotopesmodelingspatial variation
collection DOAJ
language English
format Article
sources DOAJ
author Zuhair Kattan
spellingShingle Zuhair Kattan
Spatial Mapping of Atmospheric Precipitation Isotopes in Syria
Asian Journal of Atmospheric Environment
precipitation
environmental isotopes
modeling
spatial variation
author_facet Zuhair Kattan
author_sort Zuhair Kattan
title Spatial Mapping of Atmospheric Precipitation Isotopes in Syria
title_short Spatial Mapping of Atmospheric Precipitation Isotopes in Syria
title_full Spatial Mapping of Atmospheric Precipitation Isotopes in Syria
title_fullStr Spatial Mapping of Atmospheric Precipitation Isotopes in Syria
title_full_unstemmed Spatial Mapping of Atmospheric Precipitation Isotopes in Syria
title_sort spatial mapping of atmospheric precipitation isotopes in syria
publisher Asian Association for Atmospheric Environment
series Asian Journal of Atmospheric Environment
issn 1976-6912
2287-1160
publishDate 2021-06-01
description Stable isotope ratios (δ2H and δ18O), tritium (3H). and deuterium excess (d-excess) values of atmospheric precipitation (P) at 16 stations were determined for mapping the spatial variation of oxygen and hydrogen P isotopes in Syria. The major geographical parameters (longitude east, LE; latitude north, LN; altitude, H; and inland distance from the coast, DFC) were used to find out the best fitting models for the spatial mapping of atmospheric P isotopes in Syria. The highest correlation coefficients (r>0.73) were found for the relationships δ18O-H and δ2H-H. The impacts of LE and LN factors were rather moderate (0.3<r<0.6). However, a high correlation coefficient (r>0.7) was found for the relationship d-excess-LN. The increase of d-excess value from 23‰ to 24‰ in southern Syria is due to the Mediterranean Sea (MS) moisture, likely as a high percentage (>65%) of prevailed winds usually comes over the MS. The concentrations of 3H in P samples (4-14 TU) during the period 1989-1993 were higher than those (3-10 TU) for the period 2004-2006, indicating thus a return back toward the levels of typical 3H production in nature. The high correlation coefficients (r>0.59) that were found for the relationships 3H-DFC and 3H-LE, suggest a continuous exchange between the low tritium moisture from the MS and the higher tritium moisture from the inland areas. Produced gridded isotopic values are quite satisfactory for covering certain areas in Syria and the neighboring Arab countries.
topic precipitation
environmental isotopes
modeling
spatial variation
url https://doi.org/10.5572/ajae.2021.009
work_keys_str_mv AT zuhairkattan spatialmappingofatmosphericprecipitationisotopesinsyria
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