Articles | Volume 25, issue 7
https://doi.org/10.5194/acp-25-4013-2025
https://doi.org/10.5194/acp-25-4013-2025
Research article
 | 
09 Apr 2025
Research article |  | 09 Apr 2025

One-year continuous observations of near-surface atmospheric water vapor stable isotopes at Matara, Sri Lanka, reveal a strong link to moisture sources and convective intensity

Yuqing Wu, Jing Gao, Aibin Zhao, Xiaowei Niu, Yigang Liu, Disna Ratnasekera, Tilak Priyadarshana Gamage, and Amarasinghe Hewage Ruwan Samantha

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This preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).
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Subject: Climate and Earth System | Research Activity: Field Measurements | Altitude Range: Troposphere | Science Focus: Chemistry (chemical composition and reactions)
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Cited articles

Aemisegger, F. and Sjolte, J.: A Climatology of Strong Large-Scale Ocean Evaporation Events. Part II: Relevance for the Deuterium Excess Signature of the Evaporation Flux, J. Climate, 31, 7313–7336, https://doi.org/10.1175/JCLI-D-17-0592.1, 2018. 
Aemisegger, F., Sturm, P., Graf, P., Sodemann, H., Pfahl, S., Knohl, A., and Wernli, H.: Measuring variations of δ18O and δ2H in atmospheric water vapour using two commercial laser-based spectrometers: an instrument characterisation study, Atmos. Meas. Tech., 5, 1491–1511, https://doi.org/10.5194/amt-5-1491-2012, 2012. 
Angert, A., Lee, J. E., and Yakir, D.: Seasonal variations in the isotopic composition of near-surface water vapour in the eastern Mediterranean, Tellus B, 60, 674–684, https://doi.org/10.1111/j.1600-0889.2008.00357.x, 2008. 
Bailey, H. L., Kaufman, D. S., Henderson, A. C. G., and Leng, M. J.: Synoptic scale controls on the δ18O in precipitation across Beringia, Geophys. Res. Lett., 42, 4608–4616, https://doi.org/10.1002/2015GL063983, 2015. 
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Monitoring of atmospheric water vapor isotopes for 1 year at Matara, Sri Lanka, revealed clear seasonal variations in δ18O and d-excess. The results showed lower amplitudes of δ18O during the southwest monsoon and higher amplitudes of δ18O during the northeast monsoon. Sea surface evaporation and regional convective activity influenced the isotopic compositions. Our results facilitate an understanding of the impacts of local meteorological conditions on tropical water vapor isotope signals.
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