AI Article Synopsis

  • Tar ball deposition along the West Coast of India, especially in Goa and Gujarat during the southwest monsoon, raises concerns among local stakeholders.
  • Previous studies identified tanker wash as the source of tar balls in 2010 and Bombay High oil fields as the source for those found in subsequent years.
  • The current study used a trajectory model to trace tar balls deposited in May 2013 and 2014, confirming their origins from the oil fields and showing that wind and ocean conditions significantly impact their residence time and deposition patterns.

Article Abstract

Tar ball (TB) deposition along the West Coast of India (WCI) is a common phenomenon during the southwest monsoon season, particularly along the coast of Goa and Gujarat, and it is a major concern to the stake holders. Our earlier studies showed that the source oil for the TBs deposited on the Goa coast in August 2010 is the tanker wash, and the source for subsequent TBs deposited on the Gujarat coast during July 2012 and June 2013 and Goa coast in May 2013 is from Bombay High (BH) oil fields. In the present study, the TBs that were deposited during May 2013 and May 2014 on the Goa coast were backtracked through a trajectory model, primarily to simulate their pathways and identify the reason for the occurrence of TBs only in May, and eventually to identify the origin and the source. The backtracking results re-confirmed that the TBs deposited in 2010 were originated from the tanker routes and that of both 2013 and 2014 TBs from the BH oil fields. The climatology of wind and surface circulation showed that the TBs deposited on the Goa coast during May/June only are from the oil fields and those during August from the tanker route. The results of backtracking simulations showed that the residence time of the oil residues/TBs is approximately 22days for August 2010 TBs, ≈30days for May 2013 TBs and 65days for May 2014 TBs. The residence time (in water) of TBs that deposit (on the coast) in the month of May could be as much as 7months, and could be around one month if deposit in August, primarily because of winds and hydrodynamic conditions of the Arabian Sea.

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Source
http://dx.doi.org/10.1016/j.scitotenv.2016.06.101DOI Listing

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