Ozone may be heating the planet more than scientists realise

Ozone may be heating the planet more than scientists realise
Ozone may be heating the planet more than scientists realise

Ozone may be weakening one of Earth's most important cooling mechanisms and heating our planet even more than we realise, a new study warns. 

An international team of researchers discovered changes in ozone levels in two layers of Earth's atmosphere. 

In the troposphere (the lowest layer of Earth's atmosphere), ozone has increased, which is bad news because it acts as greenhouse gas, trapping outgoing longwave radiation, and thereby heating the Earth. 

Meanwhile, ozone levels in the stratosphere (the next layer up from the troposphere) have decreased, which is also bad news, according to the team. 

Both of these changes have weakened a natural cooling mechanism of the Southern Ocean, and in turn contributed to warming of the planet.  

Acting like a shield, ozone absorbs UV light from the sun. Its absence means more of this high-energy radiation reaches the Earth, where it can harm living cells. The ozone layer is depleted by chemical reactions, driven by solar energy, that involve the by-products of human-made chemicals that linger in the atmosphere. Pictured: ozone levels vary with altitude

Acting like a shield, ozone absorbs UV light from the sun. Its absence means more of this high-energy radiation reaches the Earth, where it can harm living cells. The ozone layer is depleted by chemical reactions, driven by solar energy, that involve the by-products of human-made chemicals that linger in the atmosphere. Pictured: ozone levels vary with altitude

False-colour view of total ozone over the Antarctic pole, March 28. The purple and blue colors are where there is the least ozone, and the yellows and reds are where there is more ozone

False-colour view of total ozone over the Antarctic pole, March 28. The purple and blue colors are where there is the least ozone, and the yellows and reds are where there is more ozone

LAYERS OF THE ATMOSPHERE

Troposphere is where humans live and weather exists, the lowest layer stretching up to about six miles. 

Stratosphere extends up to about 40 miles and contains much of the ozone in the atmosphere.

Mesosphere sits just above the stratosphere where temperature decreases with height, reaching -130F.

Thermosphere is where temperatures begin to increase with height, caused by the absorption of UV and X-rays.

Exosphere starts at 310 miles and contains oxygen and hydrogen atoms, but in very low numbers.

Magnetosphere features charged particles along magnetic field lines in two bands at 1,800 and 10,000 miles above the surface.

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The Southern Ocean contributes to ocean circulation, transporting heat from the equator to the poles, causing the planet to cool overall. 

'The ocean absorbs excess heat from Earth's system, acting to balance the excess heat from rising global temperatures,' study author Dr Michaela Hegglin, an associate professor at the University of Reading, told MailOnline. 

'As the Earth's surface warms up due to increasing greenhouse gases, water in the ocean soaks up energy (heat) and distributes it more evenly across the planet.'

Ozone (O3) – which causes a smoggy haze that can damage the lungs – is a molecule comprised of three oxygen atoms that occurs naturally in small amounts. 

It is created by chemical reactions between oxides of nitrogen (NOx) and volatile organic compounds (VOC), found in exhaust fumes, in the presence of sunlight. 

It's already well known that at ground level, ozone can cause health problems for vulnerable people who suffer from lung diseases such as asthma. 

However, further up in the Earth's atmosphere – in the stratosphere, between 31 miles and 52 miles above the ground – ozone is beneficial to us. 

In the stratosphere is the ozone layer, a thin region that absorbs almost all of the sun's harmful ultraviolet light. 

Smog is primarily made up of ground level ozone combined with other gases and particle pollution. Picture, smog over New York

Smog is primarily made up of ground level ozone combined with other gases and particle pollution. Picture, smog over New York 

WHAT IS THE OZONE LAYER?

Ozone is a molecule comprised of three oxygen atoms that occurs naturally in small amounts. 

In the stratosphere, roughly seven to 25 miles above Earth's surface, the ozone layer acts like sunscreen, shielding the planet from potentially harmful ultraviolet radiation.

It is produced in tropical latitudes and distributed around the globe. 

Closer to the ground, ozone can also be created by photochemical reactions between the sun and pollution from vehicle emissions and other sources, forming harmful smog.

In the 1970s, it was recognised that chemicals called chlorofluorocarbons used in refrigeration and aerosols were destroying ozone in the stratosphere.  

In 1987, the Montreal Protocol was agreed, which led to the phase-out of CFCs and, recently, the first signs of recovery of the Antarctic ozone layer. 

At lower latitudes, the upper stratosphere is also showing clear signs of recovery, suggesting the

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