Ozone cell of Bangladesh



Q1. What is ozone and where is it in the atmosphere?

Ozone is a gas that is naturally present in our atmosphere. Each ozone molecule contains three atoms of oxygen

and is denoted chemically as O3. Ozone is found primarily in two regions of the atmosphere. About 10% of

atmospheric ozone is in the troposphere, the region closest to Earth (from the surface to about 10–16 kilometers

(6–10 miles)). The remaining ozone (about 90%) resides in the stratosphere between the top of the troposphere

and about 50 kilometers (31 miles) altitude. The large amount of ozone in the stratosphere is often referred to

as the “ozone layer.”

Q2. How is ozone formed in the atmosphere?

Ozone is formed throughout the atmosphere in multistep chemical processes that require sunlight. In the

stratosphere, the process begins with an oxygen molecule (O2) being broken apart by ultraviolet radiation from

the Sun. In the lower atmosphere (troposphere), ozone is formed by a different set of chemical reactions that

involve naturally occurring gases and those from pollution sources.

Q3. Why do we care about atmospheric ozone?

Ozone in the stratosphere absorbs a large part of the Sun’s biologically harmful ultraviolet radiation.

Stratospheric ozone is considered “good” ozone because of this beneficial role. In contrast, ozone formed at

Earth’s surface in excess of natural amounts is considered “bad” ozone because it is harmful to humans, plants,

and animals. Natural ozone near the surface and in the lower atmosphere plays an important beneficial role in

chemically removing pollutants from the atmosphere.

Q4. How is total ozone distributed over the globe?

The distribution of total ozone over the Earth varies with location on timescales that range from daily to

seasonal. The variations are caused by large-scale movements of stratospheric air and the chemical production

and destruction of ozone. Total ozone is generally lowest at the equator and highest in polar regions.

Q5. How is ozone measured in the atmosphere?

The amount of ozone in the atmosphere is measured by instruments on the ground and carried aloft on

balloons, aircraft, and satellites. Some instruments measure ozone locally by continuously drawing air samples

into a small detection chamber. Other instruments measure ozone remotely over long distances by using ozone’s

unique optical absorption or emission properties.

Q6. What are the principal steps in stratospheric ozone depletion caused

by human activities?

The initial step in the depletion of stratospheric ozone by human activities is the emission, at Earth’s surface,

of gases containing chlorine and bromine. Most of these gases accumulate in the lower atmosphere because

they are unreactive and do not dissolve readily in rain or snow. Natural air motions transport these accumulated

gases to the stratosphere, where they are converted to more reactive gases. Some of these gases then

participate in reactions that destroy ozone. Finally, when air returns to the lower atmosphere, these reactive

chlorine and bromine gases are removed from Earth’s atmosphere by rain and snow.

Q7. What emissions from human activities lead to ozone depletion?

Certain industrial processes and consumer products result in the emission of ozone-depleting

substances (ODSs) to the atmosphere. ODSs are manufactured halogen source gases that are

controlled worldwide by the Montreal Protocol. These gases bring chlorine and bromine atoms

to the stratosphere, where they destroy ozone in chemical reactions. Important examples

are the chlorofluorocarbons (CFCs), once used in almost all refrigeration and air conditioning

systems, and the halons, which were used in fire extinguishers. Current ODS abundances in the

atmosphere are known directly from air sample measurements.


Q8. What are the reactive halogen gases that destroy stratospheric ozone?

Emissions from human activities and natural processes represent a large source of chlorine- and brominecontaining

gases that enter the stratosphere. When exposed to ultraviolet radiation from the Sun, these halogen

source gases are converted to more reactive gases containing chlorine and bromine. Some reactive gases act as

chemical reservoirs that convert to form the most reactive gases, namely chlorine monoxide (ClO) and bromine

monoxide (BrO). The most reactive gases participate in catalytic reactions that efficiently destroy ozone. Most

volcanoes emit some reactive halogen gases that readily dissolve in water and are usually washed out of the

atmosphere before they can reach the stratosphere.

Q9. What are the chlorine and bromine reactions that destroy stratospheric ozone?

Reactive gases containing chlorine and bromine destroy stratospheric ozone in “catalytic” cycles made up of two

or more separate reactions. As a result, a single chlorine or bromine atom can destroy many thousands of ozone

molecules before it leaves the stratosphere. In this way, a small amount of reactive chlorine or bromine has a large

impact on the ozone layer. A special situation develops in polar regions in the late winter/early spring season where

large enhancements in the abundance of the most reactive gas, chlorine monoxide, leads to severe ozone depletion.

Q10. Why has an “ozone hole” appeared over Antarctica when ozone-depleting

gases are present throughout the stratosphere?

Ozone-depleting substances are present throughout the stratospheric ozone layer because they are transported

great distances by atmospheric air motions. The severe depletion of the Antarctic ozone layer known as the

ozone hole” occurs because of the special atmospheric and chemical conditions that exist there and nowhere

else on the globe. The very low winter temperatures in the Antarctic stratosphere cause polar stratospheric

clouds (PSCs) to form. Special reactions that occur on PSCs, combined with the relative isolation of polar

stratospheric air, allow chlorine and bromine reactions to produce the ozone hole in Antarctic springtime.

Q11. How severe is the depletion of the Antarctic ozone layer?

Severe depletion of the Antarctic ozone layer was first reported in the mid-1980s. Antarctic ozone depletion

is seasonal, occurring primarily in late winter and early spring (August to November). Peak depletion occurs in

early October when ozone is often completely destroyed over a range of altitudes, thereby reducing total ozone

by as much as two-thirds at some locations. This severe depletion creates the “ozone hole” apparent in images

of Antarctic total ozone made using satellite observations. In most years the maximum area of the ozone hole

far exceeds the size of the Antarctic continent.

Q12. Is there depletion of the Arctic ozone layer?

Yes, significant depletion of the Arctic ozone layer now occurs in most years in the late winter/early spring period

(January to March). However, the maximum depletion is less severe than that observed in the Antarctic and is

more variable from year to year. A large and recurrent “ozone hole,” as found in the Antarctic stratosphere,

does not occur in the Arctic.

Q13. How large is the depletion of the global ozone layer?

Depletion of the global ozone layer began gradually in the 1980s and reached a maximum of about 5% in

the early 1990s. The depletion has lessened since then and now is about 3.5% averaged over the globe. The

average depletion exceeds the natural year-to-year variations of global total ozone. The ozone loss is very small

near the equator and increases with latitude toward the poles. The larger polar depletion is attributed to the late

winter/early spring ozone destruction that occurs there each year.

Q14. Do changes in the Sun and volcanic eruptions affect the ozone layer?

Yes, factors such as changes in solar radiation, as well as the formation of stratospheric particles after volcanic

eruptions, do influence the ozone layer. However, neither factor can explain the average decreases observed in

global total ozone over the last three decades. If large volcanic eruptions occur in the coming decades, ozone

depletion will increase for several years afterwards.


Q15. Are there regulations on the production of ozone-depleting gases?

Yes, the production and consumption of ozone-depleting substances are controlled under a 1987 international

agreement known as the “Montreal Protocol on Substances that Deplete the Ozone Layer” and by its

subsequent Amendments and Adjustments. The Protocol, now ratified by all 197 United Nations members,

establishes legally binding controls on national production and consumption of ozone-depleting substances

(ODSs). Production and consumption of all principal ODSs by developed and developing nations will be almost

completely phased out before the middle of the 21st century.

Q16. Has the Montreal Protocol been successful in reducing ozone-depleting gases in

the atmosphere?

Yes, as a result of the Montreal Protocol, the overall abundance of ozone-depleting substances (ODSs) in the

atmosphere has been decreasing for about a decade. If the nations of the world continue to comply with the

provisions of the Montreal Protocol, the decrease will continue throughout the 21st century. Those gases that

are still increasing in the atmosphere, such as halon-1301 and HCFC-22, will begin to decrease in the coming

decades if compliance with the Protocol continues. Only after midcentury will the effective abundance of ODSs

fall to values that were present before the Antarctic ozone hole was observed in the early 1980s.

Q17. Does depletion of the ozone layer increase ground-level ultraviolet radiation?

Yes, ultraviolet radiation at Earth’s surface increases as the amount of overhead total ozone decreases, because

ozone absorbs ultraviolet radiation from the Sun. Measurements by ground-based instruments and estimates

made using satellite data provide evidence that surface ultraviolet radiation has increased in large geographic

regions in response to ozone depletion.

Q18. Is depletion of the ozone layer the principal cause of climate change?

No, ozone depletion itself is not the principal cause of climate change. Changes in ozone and climate are directly

linked because ozone absorbs solar radiation and is also a greenhouse gas. Stratospheric ozone depletion and

increases in global tropospheric ozone that have occurred in recent decades have opposing contributions to climate

change. The ozone depletion contribution, while leading to surface cooling, is small compared with the contribution

from all other greenhouse gas increases, which leads to surface warming. The total forcing from these other

greenhouse gases is the principal cause of observed and projected climate change. Ozone depletion and climate

change are indirectly linked because both ozone depleting substances and their substitutes are greenhouse gases.

Q19. Have reductions of ozone-depleting substances under the Montreal Protocol

also protected Earth’s climate?

Yes. All ozone-depleting substances are also greenhouse gases that contribute to climate forcing when they

accumulate in the atmosphere. Montreal Protocol controls have led to a substantial reduction in the emissions of

ozone-depleting substances (ODSs) over the last two decades. These reductions have provided the added benefit

of reducing the human contribution to climate change while protecting the ozone layer. Without Montreal Protocol

controls, the climate forcing contribution from annual ODS emissions could now be 10-fold larger than its present

value, which would be a significant fraction of the climate forcing from current carbon dioxide (CO2) emissions.

Q20. How is ozone expected to change in the coming decades?

Substantial recovery of the ozone layer from the effects of ozone-depleting substances (ODSs)

is expected near the middle of the 21st century, assuming global compliance with the Montreal

Protocol. Recovery will occur as ODSs and reactive halogen gases in the stratosphere decrease in

the coming decades. In addition to responding to ODSs, future ozone amounts will increasingly

be influenced by expected changes in climate. The resulting changes in stratospheric ozone

will depend strongly on the geographic region. During the long recovery period, large volcanic

eruptions could temporarily reduce global ozone amounts for several years.