Term 2 - Climate Change Flashcards
Troposhpere
The first layer of the earths atmosphere Contains weather Densest layer Warmer at surface and decreases with alititude Bordered by tropopause 7-20km high
Stratosphere
Second layer of earths atmosphere Contains the ozone layer which absorbs UV radiation causes temp to rise Around 10-50km up less dense (less water vapour) Temp increases with altitude
Mesophere
Drop in temp marks the beginning of mesosphere
Meteors burn here
80km high
gases are less dense
temp decreases as altitude increases
gases in this layer absorb little UV radiation
Thermosphere
Extends to almost 600km high temperature increases with altitude absorbs UV radiation through gases Particles are very hot but they are so few that it woud feel cold unless you touched one Space shuttles orbit here
Exosphere
Outer layer Extends for 1000s of km satellites orbit here no defined edge molecules gradually escape to outer space barrier between space and earth
what are the most common atmospheric gases?
Nitrogen and Oxygen
Explain how altittude effects air density
As the air pressure decreases with altitude, the density of the air decreases. The air particles are not so close together as tightly as they go further from the earths surface. at earth they are pulled down dense bc of gravity
What is good and bad ozone?
Stratosphere ozone is good - its natural and protects the earth from the sun by absorbing the UV radiation
Tropospheric ozone is bad - it is pollution (not natural)
what causes ozone depletion?
Caused by ChloroFluroCarbon pollution
Radiation from the sun causes the CFCs to break down and release a chlorine atom which react with the ozone
What causes an increase in the earths avergae temp?
increase of greenhouse gases
Name the 5 greenhouse gases
Carbon dioxide, sulfur dioxide, ozone, CFCs, water vapour
Effects of greenhouse gas pollution
global warming, increased severity of weather, ice metls, floodijng, rising sea levels, drought etc
Explain the global heat budget
different parts of the earths atmosphere and surface reflect different amounts of incoming solar radiation (insolation). it is a balance of how much the earth should receive, reflect and absorb. if not balanced, the earth becomes hotter or colder.
How is the solar radiation reflected?
20% reflected by dark soil
10% reflected by ocean
85%-90% reflected by snow and ice - when the ice melts, the lower the albedo (amoun that can be reflected)
ways to read climate change
rings on trees and coral, air trapped in ice, carbon in air, argo floats in ocean, how much ice is melting