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  4. Temporal characteristics of stable isotopes of oxygen (18O) and hydrogen (2H) at Senai, Johor, Malaysia
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Temporal characteristics of stable isotopes of oxygen (18O) and hydrogen (2H) at Senai, Johor, Malaysia

Author(s)
Modon Valappil, Ninu Krishnan
Yusup, Yusri
Jamjareegulgarn, Punyawi
Hamza, Vijith
Date Issued
January 1, 2025
Type
Article
DOI
10.1080/10256016.2025.2492861
Abstract
The present research aimed to characterize the temporal variation in the compositions of stable isotopes ((Formula presented.) and δ18O) at Senai in Johor, Malaysia. Long-term monthly data collected from Malaysian Nuclear Agency and the International Atomic Energy Agency (IAEA)/World Meteorological Organisation (WMO), Global Network for Isotopic Precipitation (GNIP) for a period of 2013–2021 were considered. The isotopic composition was evaluated monthly, seasonally and annually by taking into account the amount of precipitation (rainfall), temperature and relative humidity. The δD and δ18O values showed enriched values in the months of January, February and March and depleted values in November and December, respectively. Considering the seasonal characteristics at Senai site, it was found that the precipitation during the northeast monsoon (NEM) showed a slight enrichment in isotopic compositions as compared to the rainfall during the southwest monsoon (SWM). The primary sources of moisture were identified through the modelling of HYSPLIT-based backward trajectories, which indicated that the Pacific Ocean, the South China Sea (NEM season) and the Indian Ocean (SWM season) play significant roles as moisture contributors. Additionally, landmasses in the western Pacific and northern continental regions also supplied moisture that influenced the composition of stable isotopes in precipitation in Senai. The findings of this study contribute to a deeper comprehension of the hydrometeorological processes at play in the study area, which affect the fluctuations of compositions of stable isotopes in precipitation within the region. Further, a more comprehensive investigation of δ18O and δD isotopes is deemed crucial as essential climate response variables. This research will enhance our understanding of the hydrological cycle and improve predictions regarding the impacts of future climate change and alterations in ecosystems.
Citation
Isotopes in Environmental and Health Studies, 61(4), 433-454, 2025
Subjects

Amount effect

GMWL

GNIP

LMWL

MMWL

precipitation

stable isotope

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