The research team found that the principal source of iodine oxide can be explained by emissions of hypoiodous acid (HOI) – a gas not yet considered as being released from the ocean – along with a contribution from molecular iodine (I2).
Since the 1970s when methyl iodide (CH3I) was discovered as ubiquitous in the ocean, the presence of iodine in the atmosphere has been understood to arise mainly from emissions of organic compounds from phytoplankton -- microscopic marine plants.
This new research builds on an earlier study, which showed that reactive iodine, along with bromine, in the atmosphere is responsible for the destruction of vast amounts of ozone – around 50 percent more than predicted by the world’s most advanced climate models – in the lower atmosphere over the tropical Atlantic Ocean.
The scientists quantified gaseous emissions of inorganic iodine following the reaction of iodide with ozone in a series of laboratory experiments.
They showed that the reaction of iodide with ozone leads to the formation of both molecular iodine and hypoiodous acid.
Using laboratory models, they show that the reaction of ozone with iodide on the sea surface could account for around 75 percent of observed iodine oxide levels over the tropical Atlantic Ocean.
The study is published in the journal Nature Geoscience.
Washington: Scientists at the Universities of York and Leeds have claimed that the majority of ozone-depleting iodine oxide observed over the remote ocean comes from a previously unknown marine source.
First Published: Monday, January 14, 2013, 12:49