About the ozone layer Essay



The ozone bed is a part of Earth ambiance that contains high degrees of ozone. The ambiance is divided into five beds: the troposphere, the stratosphere, the mesosphere, the thermosphere, and the exosphere. The troposphere is the bed closest to Earth and is where all conditions occurrences occur. The stratosphere is located straight above the troposphere, about 10-50 kilometres above the planet, and houses the ozone bed at an height of 20-30 kilometres. The mesosphere is located about 50-80 kilometres above the Earth, while the thermosphere remainders at an height of about 100-200 kilometres above the Earth surface. Finally, the boundary of the outermost bed, the exosphere, extends approximately to 960-1000 kilometres above the Earth.

The ozone found in our ambiance is formed by an interaction between O molecules ( composed of two O atoms ) and ultraviolet visible radiation. When ultraviolet visible radiation hits these O molecules, the reaction causes the molecules to interrupt apart into individual atoms of O ( UV light + O2 — & gt ; O + O ) . These individual atoms of O are really reactive, and a individual atom combines with a molecule of O to organize ozone ( O3 ) , which is composed of three atoms of O ( 2O + 2O2 — & gt ; 2O3 ) .

We will write a custom essay sample on
About the ozone layer Essay
or any similar topic only for you
Order now


The ozone bed is indispensable for human life. It is able to absorb much harmful UV radiation, forestalling incursion to the Earth surface. Ultraviolet radiation ( UV ) is defined as radiation with wavelengths between 290-320 nanometres, which are harmful to life because this radiation can come in cells and destruct the deoxyribonucleic acid ( DNA ) of many life signifiers on planet Earth. In a sense, the ozone bed can be thought of as a UV filter or our planets built in sunblock. Without the ozone bed, UV radiation would non be filtered as it reached the surface of the Earth. If this happened, malignant neoplastic disease would interrupt out and all of the life civilisations, and all species on Earth would be in hazard. Therefore, the ozone bed basically allows life, as we know it, to be.

A Dobson Unit is a measuring of how thick a specific part of the ozone bed would be if it were compressed into a individual bed at zero grades Celsius with one unit of atmospheric force per unit area moving on it ( standard temperature and force per unit area – S.t.p. ) . Therefore, one Dobson Unit ( DU ) is defined as.01 millimeter thickness at standard temperature and force per unit area. Since the ozone bed over this country would organize a 3 millimeter midst slab, the measuring of the ozone over Labrador is 300 DU.

Ozone depletion: Who is responsible?

It is of import to acknowledge the beginnings of ozone depletion before one can to the full understand the job. There are three chief subscribers to the ozone job: human activity, natural beginnings, and volcanic eruptions. Human activity is by far the most prevailing and destructive beginning of ozone depletion, while endangering volcanic eruptions are less common. Human activity, such as the release of assorted compounds incorporating Cl or Br, histories for about 75 to 85 per centum of ozone harm. Possibly the most apparent and destructive molecule of this description is chloroflourocarbon ( CFC ) . Chlorofluorocarbons were foremost used to clean electronic circuit boards, and as clip progressed, were used in aerosols and coolants, such as iceboxs and air conditioners. When Chlorofluorocarbons from these merchandises are released into the ambiance, the devastation begins. As Chlorofluorocarbons are emitted, the molecules float toward the ozone rich stratosphere. Then, when UV radiation contacts the CFC molecule, this causes one Cl atom to emancipate. This free Cl so reacts with an ozone ( O3 ) molecule to organize Cl monoxide ( ClO ) and a individual O molecule ( O2 ) . This reaction can be illustrated by the undermentioned chemical equation: Cl + O3 — & gt ; O2 + ClO. Then, a individual O atom reacts with a Cl monoxide molecule, doing the formation of an O molecule ( O2 ) and a individual Cl atom ( O + ClO — & gt ; Cl + O2 ) . This baleful Cl atom so continues the rhythm and consequences in farther devastation of the ozone bed. Measures have been taken to cut down the sum of CFC emanation, but since Chlorofluorocarbons have a life span of 20-100 old ages, antecedently emitted CFCs will make damage for old ages to come.

Natural beginnings besides contribute to the depletion of the ozone bed, but non about every bit much as human activity. Natural beginnings can be blamed for about 15 to 20 per centum of ozone harm. A common natural beginning of ozone harm is of course happening Cl. Naturally happening Cl, like the Cl released from the reaction between a CFC molecule and UV radiation, besides has damaging effects and airss danger to the Earth.

Finally, volcanic eruptions are a little subscriber to ozone harm, accounting for one to five per centum. During big volcanic eruptions, Cl, as a constituent of hydrochloric acid ( HCl ) , is released straight into the stratosphere, along with sulfur dioxide. In this instance, S dioxide is more harmful than Cl because it is converted into sulphuric acid aerosols. These aerosols accelerate damaging chemical reactions, which cause Cl to destruct ozone.

Rocket Launches May Need Regulation to Prevent Ozone Depletion

As the projectile launch market grows, so will ozone-destroying projectile emanations, if left unregulated, projectile launches by the twelvemonth 2050 could ensue in more ozone devastation than was of all time realized by Chlorofluorocarbons.

Since some proposed infinite attempts would necessitate frequent launches of big projectiles over drawn-out periods. In the policy universe uncertainness frequently leads to unneeded ordinance, this could be avoided with a more robust apprehension of how projectiles affect the ozone bed.

Current planetary projectile launches deplete the ozone bed by no more than a few hundredths of 1 per centum yearly. But as the infinite industry grows and other ozone-depleting chemicals decline in the Earth ‘s stratosphere, the issue of ozone depletion from projectile launches is expected to travel to the head.

Today, merely a smattering of NASA infinite bird launches let go of more ozone-depleting substances in the stratosphere than the full one-year usage of CFC-based medical inhalators used to handle asthma and other diseases in the United States and which are now banned.

Highly reactive trace-gas molecules known as groups dominate stratospheric ozone devastation, and a individual group in the stratosphere can destruct up to 10,000 ozone molecules before being deactivated and removed from the stratosphere. Microscopic atoms, including carbon black and aluminium oxide atoms emitted by projectile engines, provide chemically active surface countries that increase the rate such groups “ leak ” from their reservoirs and contribute to ozone devastation.

Every type of projectile engine causes some ozone loss, and projectile burning merchandises are the lone human beginnings of ozone-destroying compounds injected straight into the center and upper stratosphere where the ozone bed resides.

Although U.S. scientific discipline bureaus spent 1000000s of dollars to measure the ozone loss potency from a conjectural fleet of 500 supersonic aircraft — a fleet that ne’er materialized — much less research has been done to understand the possible scope of effects the bing planetary fleet of projectiles might hold on the ozone bed.

Since 1987 Chlorofluorocarbons have been banned from usage in aerosol tins, deep-freeze refrigerants and air conditioners. Many scientists expect the stratospheric ozone bed — which absorbs more than 90 per centum of harmful UV radiation that can harm worlds and ecosystems — to return to degrees that existed prior to the usage of ozone-depleting chemicals by the twelvemonth 2040.

Rockets around the universe usage a assortment of propellents, including solids, liquids and loanblends. Ross said while small is presently known about how they compare to each other with regard to the ozone loss they cause, new surveies are needed to supply the parametric quantities required to steer possible ordinance of both commercial and authorities projectile launches in the hereafter.

To cut down the hazard that unpredictable and more rigorous ozone ordinances would be a hinderance to infinite entree by mensurating and patterning precisely how different projectile types affect the ozone bed.

Volcanic Aerosol Clouds and Gases Lead To Ozone Destruction

The volcanic gases released during eruptions accelerate reactions that lead to ozone devastation. The research workers found that even comparatively little volcanic eruptions can destruct ozone and create localised ‘holes ‘ in the stratosphere.

Previously, scientists had concentrated on the climatic effects of the bantam atoms of volcanic sulfate created from the sulfur dioxide gas emitted during an eruption. For the first clip, analyzing informations from a 2000 eruption of the Hekla vent, Iceland, the research workers discovered that volcanic gases may besides take to the formation of ice and azotic acid atoms. This is a critical determination as these atoms ‘switch on ‘ volcanic chorus girl gases, speed uping reactions that lead to ozone devastation.

Volcanic eruptions which penetrate the stratosphere can take to the formation of the type of clouds that promote reactions with volcanic Cl gases – gases that destroy stratospheric ozone and lead to the formation of ‘mini-ozone holes.

The ozone hole: Why over Antarctica?

When the subject of the ozone bed arises, many people instantly think of the hole over Antarctica, but few know why the hole is really at that place. In 1985, British scientists discovered this hole. A particular status exists in Antarctica that accelerates the depletion of the ozone bed. Every Arctic winter, a polar whirl signifiers over Antarctica. A polar whirl is a twirling mass of really cold, dead air surrounded by strong westerly air current. Since there is an absence of Sun during Arctic winters, the air becomes improbably cold and the formation of ice clouds occurs. When the Sun returns in the spring, the light reflecting on the N oxide filled ice atoms activates the formation of Cl. This surplus of ozone destructing Cl quickly accelerates the depletion of the ozone bed. Finally, when the polar whirl breaks up, the rapid disintegration lessenings. It is apparent that the effects of the polar whirl are dramatic.For about two month every southern spring, the entire ozone diminutions by approximately 60 % over most of Antarctica. In the nucleus of the ozone hole, more than 75 % of the ozone is lost and at some heights, the ozone virtually disappeared in October, 1999. The mean size of the ozone hole is larger than most continents, including South America, Europe, Australia, and Antarctica, and the maximal size of the ozone hole in 1996 was larger than North America. Finally, one must observe that the hole over Antarctica is genuinely a hole merely in the Antarctic spring, when the depletion is highly terrible due to the whirl.

The hole above Antarctica has clearly proven to be damaging. Plankton, organisms that live on C, visible radiation, and foods such as N, are near the underside of the nutrient concatenation, and are accustomed to low degrees of UV. In December of 1994, on the island of Bacharcaise off Antarctica, increased degrees of UV radiation decreased the figure of photoplankton dramatically. Photoplankton are the chief beginning of nutrient for krill, which in bend are the chief beginning of nutrient for assorted birds and giants in the South-polar part.

At this clip, due to the reduced figure of photoplankton, the krill degree was so low that it could non back up the penguin population. Thus, some penguins were forced to go up to two 100 stat mis in hunt of nutrient, but most returned with none. Furthermore, when summer came, merely about ten of the 1800 hatched penguin biddies survived. This calamity illustrates the fact that even submerged animals are non protected from harmful UV beams, and is a perfect illustration of the full nutrient concatenation being affected due to an addition in the UV radiation as a consequence of the thinning ozone bed.


Internationalefforts to try to restrict the production and release of Chlorofluorocarbons began one time the function of Chlorofluorocarbons in ozone devastation was established. In 1987 the United Nations Montreal Protocol was agreed and came into consequence in January 1989. The states that signed up to the protocol purpose to phase out the usage of Chlorofluorocarbons globally. The chief Chlorofluorocarbons ceased to be produced by the signers in 1995, and the European Union ceased utilizing them in 1998, except for a really little sum in limited and indispensable utilizations such as medical sprays. Although the Montreal Protocol has been successful, it should be noted that without the subsequent amendments, recovery of the ozone hole would hold been impossible.

Thehydro-chlorofluorocarbons ( HCFCs ) were developed to replace CFCs. These gases can still damage ozone if they reach the stratosphere, but they are less likely to since their excess H atom allows them to be destroyed in the lower beds of the ambiance. These gases are besides controlled under the Montreal Protocol and were phased out after 2004. The gases that replaced both the Chlorofluorocarbons and Hydrochlorofluorocarbons are hydro-fluorocarbons ( HFCs ) , which do non incorporate any Cl atoms and so hold no ozone consuming consequence. Unfortunately, many of them are powerful nursery gases and could lend to planetary heating if emitted in big measures.

SincetheCFCshaveatmospheric life-times of approximately 50 to 100 old ages, and take 5 to 10 old ages to make the upper atmosphere where they are broken down, the atmosphere reacts easy to the cuts made in emanations of these gases. Stratospheric ozone should get down to increase as the sum of Cl and Br lessenings. However, ozone is affected by alterations in other gases, such as methane, temperature alterations due to climate alteration, and besides indirectly by atoms from volcanic eruptions.

Compoundscontainingbromine, such as methyl bromide ( chiefly of natural beginning ) and the brominated CFCs ( halons: used chiefly as fire retardents ) , are besides ozone-depleting chemicals. While the entire sum of Cl in the lower ambiance peaked in 1994, and is now easy worsening, the entire sum of Br is still increasing. An appraisal by the World Meteorological Organization in 1998 estimated that planetary and South-polar ozone degrees would return to pre-1980 degrees by 2050, and in 2003 grounds suggested that the rate at which ozone is vanishing had so slowed down markedly, although estimations as to when ozone can return to a proper balance have now been revised to the latter half of the twenty-first century. However, many factors influence ozone, and future degrees are non wholly predictable.


The most obvious, and possibly most of import connexion between society and the ozone bed is the fact that scientific research suggests depletion of the ozone bed straight and indirectly endangers the wellness of the population. Research has focused on connexions between the consuming ozone bed and tegument malignant neoplastic disease, immuno-suppression, cataracts, and snow-blindness.

Ozone depletion and tegument malignant neoplastic disease: What is the connexion?

Exposure to UV radiation increases the hazard of skin malignant neoplastic disease and causes harm to the Deoxyribonucleic acid in the tegument cells. Deoxyribonucleic acid is highly sensitive to UV radiation, particularly UV-B radiation. UV radiation is located in the optical radiation part of the electromagnetic spectrum, while UV-B radiation is a subdivision of the UV spectrum and consists of a wavelength of 280 to 315 nanometres. Therefore, DNA is particularly sensitive to radiation with a wavelength between 280 and 315 nanometres.

When UV radiation hits the tegument, it can do the cell to lock up and scramble or delete DNA information. This action causes confusion in the Deoxyribonucleic acid, and the organic structure loses control of the growing and division of the cell. If the conditions are right, the cell may go cancerous. It is of import to observe that non all affected cells turn into skin malignant neoplastic disease, for many can mend themselves. However, continual exposure to UV radiation increases the hazard of skin malignant neoplastic disease due to cumulative harm of the Deoxyribonucleic acid.

Skin malignant neoplastic disease can be divided into two classs: melanoma and non-melanoma. The melanoma signifier of skin malignant neoplastic disease is the more unsafe of the two. This type of malignant neoplastic disease has the ability to distribute rapidly throughout the organic structure and occupy other cells. On the other manus, non-melanoma tegument malignant neoplastic disease is non to be taken lightly either, but is a less serious signifier of the disease. Non-melanoma tegument malignant neoplastic diseases are non normally life threatening, and remotion is comparatively everyday. However, intervention does include radiation therapy or surgery. The concern of many is that tan may take to increased hazard of geting skin malignant neoplastic disease. Some signifiers of malignant neoplastic disease are associated with tan, while other signifiers are non. Melanoma skin malignant neoplastic disease is a signifier that tans may play a prima function in. Jan new wave der Leun, a Dutch scientist, explains that, light hitting the outer bed of the tegument, the cuticle, triggers the production of some substances which diffuse into the corium below. The corium is filled with blood vass, and the chemical substances cause them to distend, doing the tegument ruddy and warm to the touch.

The bottom line is that UV beam exposure increases the hazard of skin malignant neoplastic disease. However, contention lies around the inquiry of whether or non the depletion of the ozone bed will take to more tans, and in bend, more skin malignant neoplastic disease. Some scientists suggest that the tegument will bit by bit accommodate to higher UV-B degrees as the ozone bit by bit depletes. The opposition to this theory would province that the cutting of the ozone bed would take to more human UV-B exposure. This increased UV-B exposure would, in bend, increase the harm to the Deoxyribonucleic acid doing it hard for the cell to rectify the harm before it divides. This harm accumulates over clip and increases the opportunities that a cell will turn cancerous. In add-on, since UV-B radiation amendss the immune system, it is much more likely that a cell will turn cancerous.In carnal surveies, immunosuppressive effects caused by UV-B have so been shown to play an of import function in the result of both melanoma and non-melanoma tegument malignant neoplastic diseases. Furthermore, states that for the non-melanoma tegument malignant neoplastic diseases, the grounds is obliging and there are estimations that each per centum lessening in the stratospheric ozone will take to a two per centum addition in the incidence of these malignant neoplastic diseases. Therefore, if the ozone depletes by 10 per centum over a certain clip period, 250,000 more people would be affected by these malignant neoplastic diseases each twelvemonth.

Due to controversy in the scientific community, it is hard to clearly province whether or non ozone depletion will take to an increased hazard of tegument malignant neoplastic diseases, but scientists agree on the fact that UV-B radiation plays a big function in the formation of malignant neoplastic disease. Therefore, it may really good be that as the UV filter we call the ozone bed thins, the increased sum of UV-B radiation posed on human tegument may lend to an increased sum of tegument malignant neoplastic disease. Yet, one can merely weigh all the grounds and speculate, for scientific discipline has yet to supply a cut and dry reply for society to establish its judgements on.


Regardless of the inside informations of the statements, it is obvious that the depletion of the ozone bed is a serious job that poses many effects to society. Although scientific contention exists, the possibility seems high that the depletion of the ozone bed will turn out damaging if action is non taken. For illustration, research shows the strong possibility of a figure of wellness hazards associated with increased UV-B exposure as a direct consequence of the thinning ozone bed. These wellness hazards include skin malignant neoplastic disease, immuno-suppression, cataracts, and snow sightlessness.

Furthermore, the possibility that increased UV-B radiation consequences in lower harvest outputs should supply a wakeup call to those who feel the thinning ozone bed is non a job. For if we are non able to engender UV-B immune workss, the universes nutrient supply would go dramatically reduced, ensuing in higher degrees of dearth and malnutrition.

Surveies from Antarctica tell society that increased UV radiation can straight impact the nutrient concatenation. Remember the lessening in nutrient supply as a consequence of decreased degrees of photoplankton in Antarctica. This may look like an stray, non-significant, and remote job ; nevertheless, this incident illustrates the dangers of reduced nutrient supply and change of the nutrient concatenation as a consequence of the thinning ozone bed. Even though the photoplankton were located at the underside of the nutrient concatenation, the whole concatenation was affected. In the hereafter, jobs like this could potentially impact the planetary nutrient web and consequence in an overall lessening in nutrient supply. Therefore, recognize that the dangers posed by ozone depletion are existent now, and will be in the hereafter, if action is non taken.

Take Action: Teamwork does the fast one

Although the Earth will be able to mend itself if the CFC degree continues to remain as it is, the depletion of the ozone bed is still a job that society should be concerned with. In order for Earth to mend the harm worlds have posed on the ozone bed, society must take an active function. There are many undertakings persons can affect themselves in to assist battle the job of ozone depletion. First of all, one can merely look into merchandise labels for ozone friendly position. Many companies have gone to great lengths to take Chlorofluorocarbons from their merchandises. These merchandises do non make every bit much harm to the ozone bed, and therefore, are denoted as ozone friendly. A collaborative attempt by society non utilizing merchandises with Chlorofluorocarbons is a major measure toward the healing of the ozone bed.

Unfortunately, many merchandises still used in society are damaging to the ozone bed. For illustration, CFCs marketed under the trade name Freon are used in contraptions with refrigerants such as iceboxs and air conditioners. When persons must dispose of merchandises with refrigerants in them, certain actions must be taken in order to forestall the Chlorofluorocarbons from get awaying from the fain merchandise. For illustration, when an bureau, such as a waste haling company, comes to pick up the unwanted contraption, cheque to do certain refrigerant-recovery equipment is used by the bureau. This equipment allows for the disposal of refrigerants without harm to the ozone bed.

Society can besides assist the job of ozone depletion through instruction, every bit good as through assorted contributions. If persons contribute clip or money to environmental bureaus focused on mending the ozone bed, the bureaus will be able to form activities advancing the apprehension of the ozone job. If society is educated through these agencies, more single attempts will be taken to do ozone smart determinations such as utilizing ozone friendly merchandises.

Although thinning ozone may non straight affect the coevals turning up today, future coevalss depend on the actions taken now. Therefore, it is of import for society to acknowledge that the thinning ozone bed is a job and to take action in order to guarantee the safety and endurance of future coevalss.


It is really much clear from the above treatments that there is an pressing demand of the hr to recognize the importance of the really critical ozone bed which is merely like a God gift to human civilization.

It acts as a protection shield which prevents the unsafe and harmful UV rays come ining the Earth surface. It occupation is to filtrate those harmful atoms present in the beams that can take to terrible devastation of world, wealth and belongings.

The impact of ozone depletion can be seen on the world`s economic system today it has decelerate down the advancement of non merely any peculiar state instead it is a planetary phenomenon which is impeding development.

Harmonizing to studies conducted it has been seen that twelvemonth 1998 observed soap. diminution in sum of ozone depletion.


The ozone bed is indispensable for protecting society from harmful UV radiation by moving as a filter. However, this protective bed has been thinning due to three chief beginnings: human activity, natural beginnings, and vents. Human activity is responsible for the most harm to the ozone bed, therefore, society should acknowledge that much can be done to forestall ozone bed harm.

In 1985, in a part over Antarctica, the annually polar whirl had caused the ozone bed to consume so greatly, that it could be classified as a hole. In 1996, this hole was big plenty to cover Antarctica.

The depletion of the ozone bed does non come without jobs. Scientific research has suggested the chance that increased UV-B radiation as a consequence of the thinning ozone bed leads to increased instances of tegument malignant neoplastic disease, immuno-suppression, cataracts, and snow-blindness due to radiation harm of the DNA. Additionally, experiments have shown a correlativity between increased UV radiation and harvest harm due to UV radiation damaging the workss DNA. Some scientists, nevertheless, feel that this will non be a job in the hereafter due to the possibility of engendering UV immune harvests and workss.

Many national authoritiess and bureaus recognized the job of ozone depletion, and hence, united in 1987 to subscribe the Montreal Protocol. This understanding was implemented to diminish CFC degrees in order to assist protect the thinning ozone bed.

Clearly, ozone depletion is a unsafe job due to possible disease eruptions and dearth as a consequence of increased UV-B radiation. However, society can jointly try to battle this job by comparatively simple agencies such as instruction and the pattern of ozone smart behaviour. For if society Acts of the Apostless now, future coevalss will be handed a safe and healthy planet.


Hi there, would you like to get such a paper? How about receiving a customized one? Check it out