Global Climate Change Flashcards
(70 cards)
What is weather
the short-term condition of the atmosphere at a given place and time. This is done by measuring changes in daily temperature, precipitation, wind speed, atmospheric pressure and cloud cover
What is climate
the long term average weather conditions for a location, calculated over long term periods of time
What is climate variability
refers to the year to year variation in monthly or seasonal conditions
What is climate change
the long term shift in area’s climatic conditions
What are three ways heat is distributed
Transmission: this is when heat energy passes through transparent materials,
Reflection: This heat energy bounces off and is reflected off a surface
Absorption: this is the heat energy that is retained by various substances
What is abledo
the reflectivity of a surface
What are three ways heat is returned to space
Terrestrial Radiation: After heat energy has been absorbed, it is transferred back to space it is transferred as longwave terrestrial radiation.
Conduction and convection: this is when the cool air warms up due to the warm land, this heats ups and expands causing it to rise causing convection currents
Evaporation and condensation: this is the heat required to turn water from a liquid to a gas, and heat remains in the air
How do the seasons effect the equator
- During the summer solstice for the southern hemisphere the heat equator exists of the Tropic of Capricorn.
- During the winter solstice the heat equator is located over the Tropic of cancer.
- There are also the spring and autumn equinox, this is when the sun’s rays pass exactly across the equator.
What is a heat equator
The heat equator refers to the point on the earth that is closest to the sun, which receives the most insolation.
What is anthropogenic climate change
human induced climate change
How does the heat equator affect climate
As the heat equator moves between the two tropics, that is why this area is generally the hottest part of the earth’s surface.
What is the angle of incidence and how does it affect climate
the angle at which insolation hits the sun, angle the angle of incidence changes it will affect how much the heat is dispersed and how much atmosphere it will have to pass through.
Where are the 4 main areas where high rainfall occurs and briefly explain why
low latitudes - because the strong heat from the sun creates evaporation
mid-latitudes - when cold air moves across which pushes the warm air up and clouds
coastal areas - more water is evaporated
windward slopes - moisture filled air forced to move up over landforms where the increasing altitude results in decreasing temperatures, the moisture condenses and rain is produced
What are 4 areas that have low levels of rainfall and briefly explain why?
- high pressure: because the warm air sinks down so there is no evaporation
- high latitude: doe to lack of evaporation because of the angle of incidence
- inland areas: due to lack of evaporation
- Leeward slopes: due to orographic rainfall there is now dry air
What are 3 areas of high temperature and briefly explain why
low latitudes: due to the angle of incidence so they receive the most sunlight (temp is slightly reduced by the clouds and rainfall)
subtropical zone: high amount of insolation and high pressure area
low albedo areas: more heat is absorbed and less is reflected increasing the temperature
What are three areas of low temperature and briefly explain why
- areas of high latitude: due to the angle of incidence there is reduced evaporation
- areas of high albedo: as increased insolation is reflected/not absorbed
- high altitude: because the atmosphere is thinner and cannot retain heat
What is the heat budget
The balance between the amount of incoming solar radiation and outgoing longwave terrestrial radiation
What is the heat budget
The balance between the amount of incoming solar radiation and outgoing longwave terrestrial radiation
How is insolation distributed
30% is reflected, 19% is absorbed by the atmosphere, 51% absorbed by the land and ocean
How does insolation differ from long wave radiation
the incoming solar radiation is much higher in energy and can therefore easily pass into the atmosphere however the terrestrial long-wave radiation cannot easily pass through or exit the atmosphere as there is less energy
How is long wave radiation distributed
70% is absorbed by the surface and atmosphere which is transferred backt o space through water vapour, conduction/convection, absorbed by greenhouse gases, some leaves through the atmospheric window.
What is the difference between insolation and long wave terrestrial radiation
it enters as short-wave radiation which has a lot of energy so it is easily able to pass through the atmosphere, terrestrial long wave radiation which has a lot less energy which makes it hard for it to pass through the atmosphere so it gets trapped.
What is the natural greenhouse effect
when gases in our atmosphere (known as greenhouse gases) retain heat and keep the planet warm, due to the terrestrial longwave radiation which is much slower to exit the atmosphere
What are the factors that affect variability in earths climate (LAPDOG)
Latitude - the distance from the equator
Altitude - height above sea level
Prevailing Winds - wind that constantly blows in a direction
Distance from the ocean - affects clouds, rainfall and wind
ocean -the movement of seawater
great barriers - the orographic rainfall effect which effects rainfall and moisture.