With the recent climate agreement in Paris, many countries are looking at improved energy efficiency as a way to reduce greenhouse gas (GHG) emissions to contribute to the agreed climate goal of keeping global warming below two degrees Celsius.
Innovative air-conditioning (A/C) technology, just launched by a Thai A/C manufacturer in cooperation with the Government of Thailand and the Federation of Thai Industries, will not only save consumers and the country energy, it will eliminate emissions of ozone depleting, high global warming refrigerants with little to no additional costs. At scale, this technology can play an important role in global climate mitigation efforts.
Today (September 16) is International Ozone Day. This day offers the international community the opportunity to laud the achievements of the Montreal Protocol on Substances that Deplete the Ozone Layer. Since 1987, the Protocol has worked to reduce the production and consumption of ozone-depleting substances (ODS), man-made industrial chemicals that damage the earth’s ozone layer.
Yet, as has become clear over the past few years, International Ozone Day is about more than just successful ozone layer protection. Given that many substances that deplete the ozone layer also have global warming potential (GWP), the transition to the use of substances with lower or no GWP has contributed important climate co-benefits over the years. As a result, the Protocol’s agenda has increasingly focused on cross-cutting themes linked with climate mitigation and energy efficiency. From both ozone and climate perspectives, the Protocol is widely recognized as a success.
The World Bank–China Montreal Protocol partnership is a testament to this success. Over the past two decades, it has phased-out more than 219,000 tons of ozone depleting substances from sectors as varied as refrigeration, air-conditioning, foam manufacturing, aerosol production, and fire extinguishing. Since these substances have GWP, the phase-out also avoided the equivalent of 885 million tons of carbon dioxide (CO2) or having the effect of taking 184 million cars off the roads.
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Last month, China was granted US$95 million to reduce its production of hydro-chlorofluorocarbons (HCFCs), substances that are used primarily for cooling, refrigeration, and the manufacture of foam products. The funding comes from the Multilateral Fund (MLF) of the Montreal Protocol, because HCFCs deplete the ozone layer and are controlled under the Protocol. With access to these funds, between now and 2015 China will reduce its production of HCFCs by 10%, or 47,000 metric tons from 2010 levels, allowing it to meet the first reduction targets set by the Protocol.
This alone is worth celebrating because China is the world's largest producer of HCFCs. Nearly 50% of its production is consumed by other developing countries, all of whom also face HCFC consumption reduction targets under the Protocol. Herein lies one secret to the Protocol’s success: its ability to regulate both production and consumption worldwide simultaneously, putting into practice an economist’s dream to tackle both supply and demand in tandem. By addressing the supply side of the problem through support to China’s production phase-out, the demand side - in China and in developing countries around the world - can build a sustainable HCFC consumption phase-out response. The ozone layer, and human and environmental health, will all be the better for it.
The world’s leaders set a high bar when they adopted the Montreal Protocol, which has helped protect the Earth’s protective ozone layer for the last 25 years. Even with its ambitious goals, the treaty won universally ratification – 197 parties have agreed to legally binding reduction targets to phase out ozone-depleting gases, and they have stuck to them.
The result: we, as a global community, have almost completely phased out the use of 97 substances that were depleting the ozone layer.
It’s a success worth celebrating, but we can’t rest on our laurels. We phased out CFCs, once used for cooling most refrigerators on the planet, but some of their replacement gases have become a climate change problem we still have to contend with.
The CFCs story showed that the world can move at speed and scale to reduce environmental threats. Scientists realized that CFCs were depleting the ozone layer in 1974. The ozone hole over Antarctica became common knowledge in the 1980s and helped drive global action which led to the Montreal Protocol being adopted in 1987.
At the C40 Summit in Sao Paolo last week, former President Clinton urged participating cities and the World Bank to make a dramatic reduction in methane and black carbon. He said it would help the earth buy some time on climate change. He has reasons to be worried: In Cancun last year, parties agreed to stabilize average global temperatures at a level not exceeding 2 degree C above pre-industrial levels. This looks difficult as 0.8 degree C warming has already taken place and GHG emissions continue to grow.
Developed countries collectively reduced greenhouse gas (GHG) emissions by a mere 6.1% from 1990-2008. Compared to the fast track for warming, humanity is on the slow train to reducing carbon dioxide (CO2) emission reductions.
President Clinton’s statement follows two recent reports that point to emerging scientific awareness that a climate change strategy focusing exclusively on carbon dioxide (CO2) is neither the quickest nor the most effective way to achieve long-term climate stabilization. These reports focus on non-CO2 emissions that stay in the atmosphere for a shorter period of time than CO2. As a result, reducing emissions of these non-CO2 gases will result in a slowing of temperature rise over the first half of the 21st century, buying time both to adapt and to transition away from carbon.
The first report, produced by UNEP and WMO, assesses black carbon and tropospheric ozone. Black carbon—basically soot—is produced by incomplete combustion of carbon fuels, particularly diesel, wood, and coal. It is a dark suspended particle or aerosol, technically not a GHG. It is frequently emitted together with light-colored aerosols (sulfates and organic carbon) which cool the climate. The latest research indicates that, on balance, the warming effect of black carbon overpowers the cooling effect of its companions. It stays in the atmosphere for only a few weeks before falling to earth. Its warming contribution comes from its black color, making it absorb heat while in the air. If it falls onto mountain or polar snow, it accelerates glacial melt.