Topic 6 - Atmospheric systems and society Flashcards
What is the composition of atmosphere broken down as (in %) - oxygen, nitrogen, other gases?
Nitrogen - 78%
Oxygen - 21%
Other (carbon dioxide, argon, water vapour, ozone) - 1%
Stratosphere height
10-50km high
Troposphere height
Less then 10km
Greenhouse effect
Natural phenomenon maintaining temperatures for living systems. Gases in the atmosphere reduce heat loss by radiation back into space. Trap heat energy and re-radiate it, some back to space and some back to earth
Ozone Depleting Substances (ODS)
Include CFCs are used in aerosols, gas blown plastics, pesticides, flame retardants and refrigerants
UV radiation impact on humans
-VE Reaching earth surface damages human living tissue, increasing incidents of cataracts, mutation during cell division, skin cancer, suppression of immune system
+VE Stimulates production of Vitamin D, can be used to treat psoriasis and vitiligo (skin diseases), industrial uses in lasers, used as a steriliser as it kills pathogenic bacteria
UV radiation impact on biological productivity
Damage to photosynthetic organisms, especially phytoplankton
UNEP - United Nations Environment Programme
Played a key role in providing information and creating and evaluating international agreements for the protection of stratospheric ozone
Montreal Protocol
1987 + yearly updates including Kigali Amendment 2016. International agreement, 197 countries agreed, including USA, China, Russia.
Reduction of use of ODS.
Multilateral fund set up to support nations in their transition away from ODS such as CFC
Staggered time frame to support poorer nations and their transition
Ozone layer
Dynamic layer at 20-40km high where ozone is continuously made from oxygen atoms and is continuously converted back to oxygen. During both processes UV radiation is absorbed (good thing)
Primary pollutants
From combustion of fossil fuels, include carbon monoxide, carbon dioxide, black carbon / soot, unburned hydrocarbons, nitrogen oxides and sulfur oxides
Secondary pollutants
Formed when primary pollutants react with other chemicals already in the atmosphere
Tropospheric ozone
Example of secondary pollutant formed when oxygen molecules react with oxygen atoms that are released from nitrogen dioxide in the presence of sunlight
Smog
Complex mixture of primary and secondary pollutants
Thermal inversions
Occur due to a lack of air movement when a layer of dense, cool air is trapped beneath a layer of less dense warm air. Causes concentration of air pollutants to build up near the ground rather than being dispersed