In the first
post, we mentioned that the ozone layer is able to absorb most of the sun's harmful ultraviolet rays. This
kind of harmful ultraviolet rays is called UV-B, as shown in
figure 1. It also presents how the ozone layer protects the earth by absorbing
UV-B.
This section will talk about how the ozone hole threats environment from different aspects. Firstly, the depletion
of ozone will reduce the
ability of the ozone layer to absorb UV-B, thus
damaging the plants, such as reducing crop production and plant leaves as well as photosynthesis,
making crops more susceptible to weeds, etc.
Furthermore, there are many indirect effects, including changing plant form, altering growth cycle of plant,
modifying plant metabolism. These can have more profound effects on the
environment because it may break the balance of biogeochemical cycles by
influential herbivores.
Secondly, the ozone layer is closely linked to human
health. UV can promote the synthesis of vitamin D on the skin, which plays a
beneficial role in the formation of bone. However, excessive irradiation with
ultraviolet B (λ = 280 to 320 nm) in ultraviolet light (λ = 200 to 400 nm) can
cause diseases such as skin cancer and eye diseases. It is estimated that a 1%
decrease in stratospheric ozone (an increase in UVB of 2%) will increase the
incidence of skin cancer by 4% to 6%. By now, about 100,000 people die of skin
cancer each year around the world, and those who die of skin cancer increase by
about 5,000 every year. In light-skinned people exposed to the sun for a long
time, more than 50% of the skin diseases are sun-induced, that means light-skinned
people are more susceptible to various sun-induced skin cancers than other
ethnic groups. In addition, ultraviolet light can cause premature aging of the
skin.
The ozone hole can also
change the atmosphere and ocean circulations. It may significantly impact the changes in the climate system and weather within the
Southern Hemisphere, especially in the summer (December to February). Darryn W. Waugh and his team show that subtropical
intermediate waters in the southern oceans have become fresher, because surface
winds have strengthened as the ozone layer has been thin. Antarctic ozone hole
has changed the mix in the southern oceans, a situation that could change the
amount of carbon dioxide in the atmosphere and could eventually have an impact
on global climate change.
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