Unit 6 Flashcards
The atmosphere is
A dynamic system essential to life on earth that have undergone changes throughout geological time
The atmosphere is composed of
nitrogen and oxygen with smaller amounts of carbon dioxide, argon water vapor and other gases
Troposphere
Closest layer to the earth’s surface and includes where we live. 10 km above sea level
Greenhouse effect
The ‘greenhouse effect’ is an atmospheric heating phenomenon in which the Earth experiences rise in temperature because certain gases (water vapor, carbon dioxide, nitrous oxide, and methane) in the atmosphere allow incoming sunlight to pass through but trap heat radiated from the earth’s surface.
Stratosphere
10 to 50km. Absorbs ultra violet radiation from the run.
Mesosphere
50 to 80km. Without the presence of ozone or other particulates to absorb UV radiation, the temperature declines with height. Coldesr part
Thermosphere
80km to between 500km and 1000km.
What is the albedo effect and its role managing the earths temperature
Albedo is a measure of the reflectivity of a surface. The albedo effect when applied to the Earth is a measure of how much of the Sun’s energy is reflected back into space. More water vapour in the atmosphere means more cloud formation. More clouds lead to increased albedo of the earth.
it changes how much solar energy is reflected by the Earth as opposed to how much is absorbed. This changes how Earth’s energy budget balances and thus changes Earth’s heat balance.
What is stratospheric ozone
a key component of the atmospheric system because it protects living systems from the negative effects of ultraviolet radiation from the sun
Dynamic equilibirum in stratospheric ozone
some ultraviolet radiation from the sun is abrobed by the stratospeheric ozone causing ozone molecule to break apart. Under normal conditions the ozone molecule with reform. This ozone destruction and reformation showcases dynamic equilibrium.
Consequences of UV radiation on plants/on animals
Damages human living tissues, increase cataracts, mutation during cell division, skin cancer etc
on plants
damages biological productivity especially plankton that fors at basis of aquatic food wevs
Threats to stratospheric ozone
Collectivley called (Ozone depleting substances) (ODS). Often contain clorine or bromine.
Chloroflurocarbons (CFS) are the main grouos of ODS. These are mainly used in coolants in refrigeratiors and air conditioning systems, propellants in aerosol cans, cleaning agents for electrical parts, blowing agents in plastic foam.
Changes in stratospheric ozone levels
Over time variation. Long term and seasonal changes have been recorded.
Since 1970s there has been a reduction in oone levels around the world.
Ozone levels are their lowest at summer in the Antartic regions. Sunlight releases chlorine and other chemicals that cause ozone destruction.
Management of stratospheric ozone
International agreement: Montreal Protocol signed by 197 nations.
Reduction of ozone depleting substances. Make laws and regulations to decrease the consumption and production of halogened organic gases like CFS.
Challenges for dealing with Ozone depleting substances
- Long span of ODS. They have an effect for a long time after production and use have stopped.
- ODS present in discarded equipment and these may leak into the environment
- lack of alternatives. cheaper alternatievs to ODS may not be available
- Ilegal trade. Might be driven by higher cost of alternatves. Less effective replacements
- Lack of policing and enforcemnent