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Earth System Dynamics An interactive open-access journal of the European Geosciences Union

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doi:10.5194/esd-2016-63
© Author(s) 2016. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
14 Dec 2016
Review status
A revision of this discussion paper was accepted for the journal Earth System Dynamics (ESD) and is expected to appear here in due course.
Presence of continental and Bay of Bengal moisture in rainfall at Kolkata, revealed through simultaneous observation from land and sea during South-West monsoon of 2004
Shaakir Shabir Dar and Prosenjit Ghosh Centre for Earth Sciences, Indian Institute of Science, Bangalore, India 560012
Abstract. The backward air mass trajectory analysis (HYSPLIT) during the summer monsoon suggests that the rain which precipitates at Kolkata is generated from a moisture parcel which originates from the Arabian Sea and moves inland over the dry Indian subcontinent or over the Bay of Bengal. We used monthly satellite and ground based measurements of the hydro-meteorological variables together with isotope data from Bangalore, Bay of Bengal and Kolkata and other locations to quantify the contribution of different moisture sources during the SW Monsoon. The vapor mass as it moves under the prevailing wind direction was subjected to isotopic modification due to addition of evaporated moisture from Bay of Bengal and rainout process. This was simulated using Craig and Gordon model and Rayleigh fractionation model respectively. The moisture generated during the process of evaporation from Bay of Bengal surface ocean gets advected towards the continent and precipitates as rainfall or snowfall over the Indo-Gangetic plain. We assumed based on our observation that the initial isotopic composition of vapor originating from the peninsular continental source is similar to our observation recorded at Bangalore station. It is found that the isotopic signature of Bangalore is completely lost albeit the significant contribution of the moisture from Bay of Bengal. To explain the isotopic composition of precipitation at Kolkata during the SW-Monsoon, it was necessary to invoke 75–80 % moisture contribution from the Bay of Bengal whereas the evaporated moisture parcel from the Peninsular India contribute 25 %–35 %.

Citation: Dar, S. S. and Ghosh, P.: Presence of continental and Bay of Bengal moisture in rainfall at Kolkata, revealed through simultaneous observation from land and sea during South-West monsoon of 2004, Earth Syst. Dynam. Discuss., doi:10.5194/esd-2016-63, in review, 2016.
Shaakir Shabir Dar and Prosenjit Ghosh
Interactive discussionStatus: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version      Supplement - Supplement
 
RC1: 'Review', Ruud van der Ent, 13 Jan 2017 Printer-friendly Version Supplement 
AC1: 'Reply to RC1', Shaakir Dar, 27 Feb 2017 Printer-friendly Version Supplement 
 
RC2: 'Reviewer comments', Anonymous Referee #2, 30 Jan 2017 Printer-friendly Version 
AC2: 'Reply to RC2', Shaakir Dar, 27 Feb 2017 Printer-friendly Version Supplement 
 
AC3: 'Tables and Figures', Shaakir Dar, 27 Feb 2017 Printer-friendly Version Supplement 
Shaakir Shabir Dar and Prosenjit Ghosh
Shaakir Shabir Dar and Prosenjit Ghosh

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