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ACP | Articles | Volume 18, issue 12
Atmos. Chem. Phys., 18, 8789–8805, 2018
https://doi.org/10.5194/acp-18-8789-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Atmos. Chem. Phys., 18, 8789–8805, 2018
https://doi.org/10.5194/acp-18-8789-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 22 Jun 2018

Research article | 22 Jun 2018

Isotopic composition of daily precipitation along the southern foothills of the Himalayas: impact of marine and continental sources of atmospheric moisture

Ghulam Jeelani et al.

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Cited articles

Agnihotri, C. L. and Singh, M. S.: Satellite study of western disturbances, Mausam, 33, 249–254, 1982. 
Allan, R. P. and Soden, B. J.: Atmospheric warming and the amplification of precipitation extremes, Science, 321, 1481–1484, 2008. 
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Araguás-Araguás, L., Froehlich, K., and Rozanski, K.: Stable isotope composition of precipitation over Southeast Asia, J. Geophys. Res., 103, 28721–28742, 1998. 
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Analysis of stable isotope composition of daily precipitation collected along the southern foothills of the Himalayas was used to gain deeper insight into the mechanisms controlling isotopic composition of precipitation. The results suggested that the decrease in isotopic composition in the course of ISM evolution stems from large-scale recycling of moisture-driven monsoonal circulation. High d-excess of rainfall is attributed to moisture of continental origin released into the atmosphere.
Analysis of stable isotope composition of daily precipitation collected along the southern...
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