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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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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1721353938206195712 |