How much ozone is left




















Some hydrochlorofluorocarbons HCFCs , transitional substitutes that are less damaging but still harmful to ozone, are still in use. Developing countries need funding from the Montreal Protocol's Multilateral Fund to eliminate the most widely used of these, the refrigerant R The next generation of coolants, hydrofluorocarbons HFCs , do not deplete ozone, but they are powerful greenhouse gases that trap heat, contributing to climate change.

Though HFCs represent a small fraction of emissions compared with carbon dioxide and other greenhouse gases , their planet-warming effect prompted an addition to the Montreal Protocol, the Kigali Amendment , in The amendment, which came into force in January , aims to slash the use of HFCs by more than 80 percent over the next three decades. In the meantime, companies and scientists are working on climate-friendly alternatives, including new coolants and technologies that reduce or eliminate dependence on chemicals.

All rights reserved. Climate Ozone Depletion The ozone layer helps to protect life from harmful ultraviolet radiation. Find out what caused the ozone hole, and how the Montreal Protocol sought to put an end to ozone depletion. Ozone threats and 'the hole' In , Mario Molina and Sherwood Rowland , two chemists at the University of California, Irvine, published an article in Nature detailing threats to the ozone layer from chlorofluorocarbon CFC gases.

Share Tweet Email. Read This Next Wild parakeets have taken a liking to London. Animals Wild Cities Wild parakeets have taken a liking to London Love them or hate them, there's no denying their growing numbers have added an explosion of color to the city's streets.

India bets its energy future on solar—in ways both small and big. Environment Planet Possible India bets its energy future on solar—in ways both small and big Grassroots efforts are bringing solar panels to rural villages without electricity, while massive solar arrays are being built across the country. Epic floods leave South Sudanese to face disease and starvation. Also, from direct measurements over Antarctica, a column ozone level of less than Dobson Units is a result of the ozone loss from chlorine and bromine compounds.

The graphs above show the progress of the ozone hole for The gray shading indicates the highest and lowest values measured since The red numbers are the maximum or minimum values. The stratospheric temperature and the amount of sunlight reaching the south polar region control the depth and size of the Antarctic ozone hole.

The data for the ozone hole area , the minimum ozone , and the minimum stratospheric temperature are available. Also available is a table of values showing the maximum ozone hole area and the minimum ozone values for each year.

Click on the image to get a table of values. The graphs above show the variations of ozone from year to year. What does ardent mean? What kind of literature is a picaresque novel? What does culpable mean? What's a cenotaph? What does gallimaufry mean in The Girl with the Dragon Tattoo? My vocabulary is pretty good, but that one has me stumped! What does it mean to genuflect? Someone told me I was looking wistful. What is wistful? In David Copperfield, what does superannuated mean?

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I'm in a literary dispute over this! What did W. Du Bois mean when he wrote of second-sight? It is these unique conditions through the winter and early spring that result in high ozone destruction over Antarctica. As discussed earlier in this entry , stratospheric ozone plays a fundamental role in protecting surface lifeforms from exposure to harmful levels of UV-B radiation. In the figure we show the average percentage change in UV irradiation reach the surface in relative to levels in Shown are the changes across wavelengths from to nanometres, which is the region where DNA damage from UV irradiation has its largest health impacts.

Here we see that the largest increases in UV irradiation have been at high latitudes — particularly in the South Hemisphere. At nm, for example, irradiance at high Southern latitudes increased by more than 25 percent over this period. At the Northern poles, this was much less at between 5 to 10 percent. Ozone layer protection from UV-B irradiation is critical to the health of many lifeforms, including human health. Ozone depletion and the subsequent increase in UV-B irradiation, as discussed above , can increase negative health impacts such as skin cancer , and other implications such as sunburn and skin ageing.

Using combined ozone, UV and dose-response models, numerous studies have attempted to quantify the potential increase in skin cancer cases as a result of ozone depletion. Such studies also attempt to quantify the number of skin cancer cases avoided as a result of international action through the Montreal Protocol to reduce ODS consumption. Dijk et al. The study estimates that by , two million cases worldwide will be avoided per year as a result of ODS reduction from the Montreal Protocol and its later revisions.

One of the first studies to attempt to quantify excess skin cancer cases, despite being published in the s correlates well with results from recent studies. The primary role of the Vienna Convention, Montreal Protocol and its subsequent revisions was to protect depletion of the stratospheric ozone layer. However, the ambition to reduce and eventually eliminate the use of ozone-depleting substances ODS has also produced co-benefits for greenhouse gas reduction.

With a GWP up to 10, times higher than carbon dioxide CO 2 , these gases can have a notable impact on total greenhouse gas emissions, even in very small concentrations. The reduction in ODS, in particular CFCs has therefore had a significant impact on greenhouse gas reduction in recent years.

In fact, several sources estimate that the climate benefits of the Montreal Protocol have been five to six times that of the Kyoto Protocol.

In the chart we visualize the impact of the reduction in ODS emissions for climate change in terms of greenhouse gas emissions in carbon dioxide equivalents , and radiative forcing measured in watts per square metre.

Blue trends map the estimated impact had the Montreal Protocol not been adopted: it is based on the assumption of a 2 to 3 percent dashed and solid line increase in annual production of halogen substances. The blue area therefore represents the estimated quantity of GHG or radiative forcing averted as a result of the Montreal Protocol. GHG emissions from ODSs in could have reached approximately 10 billion tonnes of CO 2 -equivalents which would have been five times the annual target of the Kyoto Protocol for the period.

If increasing trends of ODSs had continued through to , the WMO project that total GHG emissions from halogen gases could have approximated 20 billion tonnes of CO 2 -equivalents relative to 36 billion tonnes of CO 2 in — this would have been an increase of more than 50 percent to global GHG emissions.

This means HFC emissions have increased notably in recent years. However, HFCs have a large global-warming potential as shown in the table in the Data Definitions section ; and could begin to cancel out climate benefits made by the rapid reduction of CFCs and HCFCs in recent decades. If we are to preserve the climate benefits of the Montreal Protocol, further emissions and potential substitutes for CFC products will be important in the coming years. ODP tonnes attempt to standardise and correct for the differences in the potential ozone destruction across different substances.

In the table in the section below , we provide a list of substances and their respective ODP values; ODP values provide a measure of the relative destruction potential of one tonne of that substance relative to chlorofluorocarbon CFC CFC is therefore given a value of 1.

The sum of all of halogen gases in ODP tonnes provides a total measure of ozone-depleting substance emissions.

Emissions of ozone-depleting substances can be natural or man-made. Small, relatively consistent levels of ozone-depleting substances are emitted through natural processes. Most discussion in relation to ODS emissions therefore focuses on man-made emissions which can be controlled. The use of halogen gases in products such as refrigerants, solvents and foams has been persistent since the early 20th century.

These gases still reside in some products which are liable to leakage over time. Concentrations of ozone-depleting substances in the atmosphere are determined by the stock of substances, in addition to the balance of inputs and outputs over time.

The lifetime of gases in the atmosphere play an important role in understanding how their concentrations change over time. Even once emissions of ODS cease; why does the concentration of these substances not return to zero?

For many substances, this timeframe is on the scale of decades up to a century. As a result, even if emissions were halted, depleting substances which were previously emitted would continue to persist in the stratosphere. It will therefore take many decades for full recovery as substances are removed. In the table we list the range of ozone-depleting substances ODS with their corresponding ozone depleting potential ODP per tonne measured relative to CFC which is equal to 1 ; their global warming potential GWP and atmospheric lifetime in years.

The Montreal Protocol and later amendments was adopted in — since then all countries have signed on to the agreement, allowing for the dramatic decline in global ozone-depleting emissions. Ozone layer thickness declined, and the Antarctic ozone hole grew substantially from the s through to the early s. Through the first decade this trend largely stabilized and we now see initial signs of recovery.

It will take decades for the ozone layer to recover.



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