Ozone thinning has changed ocean circulation, scientists report

January 31, 2013

According to a Johns Hopkins earth scientist, the hole in the Antarctic ozone layer has caused changes in the way that waters in those southern oceans mix – a situation that has the potential to alter the amount of CO2 in the atmosphere and eventually could have an impact on global climate change.

In a paper published in this week's issue of the journal Science, Darryn W. Waugh and his team show that subtropical intermediate waters in the southern oceans have become "younger" as the upwelling, circumpolar waters have gotten "older" – changes that are consistent with the fact that have strengthened as the ozone layer has thinned.

"This may sound entirely academic, but believe me, it's not," said Waugh, of the Morton K. Blaustein Department of Earth and Planetary Sciences at Johns Hopkins' Krieger School of Arts and Sciences. "This matters because the southern oceans play an important role in the uptake of heat and carbon dioxide, so any changes in southern ocean circulation have the potential to change the global climate."

Waugh's team used measurements taken from the early 1990s to the mid-to-late 2000s of the amount of a known as "chlorofluorocarbon-12," or CFC-12, in the southern oceans. CFC-12 was first produced commercially in the 1930s and its concentration in the atmosphere increased rapidly until the 1990s when it was phased out by the on substances that deplete the . (Prior to the Montreal Protocol, CFC-12 was used in products such as aerosol hairsprays and refrigerants and in air conditioning systems.)

From those ocean measurements, Waugh's team was able to infer changes in how rapidly surface waters have mixed into the depths of the southern oceans. Because they knew that concentrations of CFCs at the increased in tandem with those in the atmosphere, they were able to surmise that the higher the concentration of CFC-12 deeper in the ocean, the more recently those waters were at the surface.

The inferred age changes – "younger in the subtropics, "older" nearer the South Pole—are consistent with the observed intensification of surface westerly winds, which have occurred primarily because of the Antarctic ozone hole, suggesting that stratospheric ozone depletion is the primary cause of the changes in ocean ventilation. As stratospheric ozone recovers over the next 50 years, the changes in ventilation may slow or reverse. The impact of continued increases in greenhouse gases in the atmosphere will also need to be considered, however. The combined impact of the two factors on the southern oceans' ventilation and uptake of heat and carbon is an open question.

Explore further: Global warming may delay recovery of stratospheric ozone

More information: "Recent Changes in the Ventilation of the Southern Oceans," by D.W. Waugh et al., Science, 2013.

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The Alchemist
1 / 5 (4) Jan 31, 2013
Wow, darn clever, huh?
ValeriaT
1.3 / 5 (4) Jan 31, 2013
so any changes in southern ocean circulation have the potential to change the global climate
Why not, but after then the (speed of) absorption of CFCs with oceanic watter will affect the thickness of ozone layer - not vice-versa. For me it's difficult to believe that rather insignificant portion of UV energy in solar spectrum could change the way, in which oceans are circulating, as the article title implies (or it's just a result of my poor understanding of English grammar?). The reversed causality arrow seems way more probable for me.
The Alchemist
1 / 5 (3) Feb 01, 2013
They were using concentrations to measure the displacement. It's not cause/effect.
Grallen
3 / 5 (1) Feb 01, 2013
This article didn't demonstrate the link. they just used a chemical to determine if the oceans were turning over slower...

The original article may have covered it, but this one should have as well...

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