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30 Cards in this Set

  • Front
  • Back

The atmosphere (air)

Mixture of gases which envelope the earth

Low latitudes

Warm air


Sun is closer to equator More insulation


0-30°

High latitudes

Cold air


At the poles

Latitude

Measures distance from north or south of equator

Cool air sinks

High pressure

Warm air rises

Low pressure

Cyclone

Warm air rises - clouds - rainfall - low pressure - 30-60° latitude

Anticyclone

Cold air sinks - clear Skye - dry weather - high pressure

Polar cell

Air cools and sinks - belt of high pressure - cold dry climate - 90° latitude

Ferrel cell (pt.1)

Cold polar air mixes with warmer air - rises - belt of low pressure - 60° latitude

Ferrel cell (pt.2)

Air Cools and sinks - belt of high pressure - as it sinks,warmer drier

Hadley cell

30-0° latitude - warm air rises - belt of low pressure - as air rises it cools - cloud form - precipitation

Warmer climate

Interglacial phase

Cooler climate

Glacial phase

Ice cores

Made of Layers(1year snowfall) Trapped bubbles CO2 - drill through core to measure CO2

Pliectocene

Last major cold perid

When did Pleistocene start and end

Started 2.6mil years ago


Ended 10,000 years ago

Current warm phase

Holocene

Holocene and Pleistocene

Quaternary period

Quaternary period

The period of geothermal time we are living in

Warmest 10 year period on record

2013-2022

Seasonal shifts

Effect nesting and migrational patterns of wildlife

3 greenhouse gases

Nitrous oxide


Methane


Carbon dioxide

What is an ice core

Layers of ice built up over time


1 layer = 1 year

How are ice cores used to measure climate change

CO2 trapped in bubbles


Measure the CO2 in each bubble

Atmospheric gas concentration

CO2 measured in ice cores

Atmospheric gas concentration

CO2 measured in ice cores

3 examples of natural climate change evidence

Ice core


Tree rings


Historical sources

What would happen without natural greenhouse effect

The planet would be to cold for humans to survive

How do greenhouse gases heat up the planet

Some long radiation is reflected of greenhouse gases back to earth - heating the earth up