Ozone layer recovery in recent years

The Indegenous
The Indegenous

The ozone barrier has been found to be quickly diminishing in the late 20th century as a result of the emission of some man-made chemicals, such as chlorofluorocarbons (CFCs), which are used in foam production, solvents, cooling and air conditioning, and other products. Because of their extreme stability, CFCs can linger in the atmosphere for many years. When they get to the atmosphere, UV light causes them to disintegrate, releasing chlorine atoms that can then damage ozone molecules.

The ozone layer which is an area of elevated ozone concentration in the stratosphere, located between 15 and 35 kilometres above the Earth's surface functions as an invisible barrier, shielding us from the sun's damaging ultraviolet (UV) rays. The ozone layer, in particular, protects us from UV-B rays, which produce sunburn. Long-term UV-B radiation endangers human health and harms most animals, plants, and microbes, so the ozone layer safeguards all species on Earth. Ozone is constantly being created and depleted. In addition to UV-B, the sun also produces UV-C ultraviolet radiation. UV-C radiation is entirely absorbed by oxygen molecules in the stratosphere and never reaches the Earth's surface. UV-C separates oxygen molecules into oxygen atoms. These solitary oxygen atoms then combine with other oxygen molecules to form ozone. As a result of these processes, the quantity of ozone in the stratosphere increases.

However, ozone is not the only gas present in the atmosphere. Other nitrogen and hydrogen-containing gases exist in the stratosphere and engage in reaction cycles that destroy ozone and transform it back into oxygen. As a result, these processes reduce the quantity of ozone in the stratosphere.

The natural mechanisms of ozone creation and destruction sustain a constant ozone concentration in the stratosphere when left alone. Unfortunately, we, as people, interfere with this normal process.

Global efforts to tackle this issue

To address this issue, the international community signed the Montreal Agreement on Substances that Deplete the Ozone Barrier in 1987. This treaty controlled the manufacture and consumption of these hazardous chemicals and established a structure for international collaboration to safeguard the ozone layer.

As a consequence of this treaty and later revisions, CFC output has decreased, and the ozone layer is beginning to recover. According to the UN, the Antarctic ozone hole has been steadily shrinking since 2000 and is anticipated to be fully repaired by 2070. Northern Hemisphere and mid-latitude ozone levels are also expected to return to 1980 values by the 2030s.

It has been crucial to create the Montreal Protocol and to keep monitoring it and adhering to the rules set in order to ensure the ozone layer's recovery and protect the world from harmful UV radiation. The international community must also maintain its caution and keep ozone-depleting substances under control in order to protect the ozone barrier for future generations.

As a consequence of the Montreal Protocol and later revisions, CFC output has decreased, and the ozone layer has begun to recover some instances of ozone depletion are: 

  1. Since 2000, the Antarctic ozone hole has gradually shrunk and is anticipated to be fully healed by 2070.
  2. Northern Hemisphere and mid-latitude ozone levels are expected to return to 1980 values by the 2030s.

A United Nations study in 2023 brought these figures into sharper relief. It discovered that if nations continued to adhere to the Montreal Protocol and its follow-on agreements, ozone concentrations would mainly revert to pre-1980 levels by 2040, with the Arctic hitting pre-1980 levels by 2045 and the Antarctic following suit by 2066.

To guarantee the continued healing of the ozone layer and to safeguard the Earth from harmful UV radiation, it is critical to continue tracking the ozone layer and adhering to the Montreal Protocol rules. The international community, for example, must remain watchful and continue to control new and developing ozone-depleting chemicals, such as hydrofluorocarbons (HFCs), which are used as refrigerants in air conditioning and cooling systems.

Montreal Protocol:

The Montreal Protocol on Substances that Deplete the Ozone Layer is an international environmental agreement that governs the manufacture and usage of nearly 100 man-made chemicals known as ozone-depleting substances (ODS). It was approved on September 16, 1987, and remains one of the few accords to have received universal approval to this day. The Protocol gradually reduces the usage and output of various ODS, with varying timetables for established and developing nations (Article 5 countries).

It includes provisions on Control Measures, Control Level Calculation, Control of Trade with Non-Parties, Special Situations of Developing Countries, Data Reporting, Non-compliance, and Technical Assistance. Annexes A, B, C, E, and F enumerate the compounds governed by the treaty (HFCs). The Meeting of the Parties governs the treaty, with professional assistance given by an Open-ended Working Group and assistance from the Ozone Secretariat.

The treaty is made to develop over time in response to new scientific, technological, and commercial advancements, and it is constantly amended and altered