EQ 1 Flashcards
Icehouse Climate
A global ice age
When large ice sheets present on earth
During this time the climate fluctuates between cooler glaciates, when ice advances, and interglacial, ice retreat
Greenhouse Climate
Occurs when there are no continental glaciers on the planet, as a result of warming processes such as height levels of greenhouse gases in the atmosphere
Current geological era
Cenozoic
Current period
Quaternary Ice Age
Quaternary Ice age
Started approximately 2.6 million years age and extends up to and including the present day
Divided into two epochs:
- Pleistocene
- Holocene
Holocene
began 10,000 years ago and continues today
Pleistocene
Wasn’t just a single ice age. Over the 2 million or so years during which it lasted, temperatures fluctuated enough to allow a number of ice advances and retreats
The extent to the ice advance during each glacial was different
There are fluctuations within each major glacial. These relatively short-lived pulses of ice advance are known as stadial, and warmer periods of retreat known as interstadials
end of the Pleistocene epoch
The last glacial advance is known as the Loch Lomond Stadial, which occurred between 12,000 and 10,000 years ago
Cryosphere
water is permanently frozen and stored as snow or ice
Why is the cryosphere important
Drinking water
Glaciers are visible and sensitive barometers of climate change because they constantly grow/advance and shrink/retreat in response of changes in temperature and precipitation
Vital role in Earth’s climate. Snow and ice reflect heat from the sun - called the albedo effect which help regulate temperature on Earth
Stadial/Interstadial
Relatively short-lived pulses of ice advance are known as stadial, and warmer periods of retreat known as interstadials.
Describe the cause of the Loch Lomond Stadial
Ice sheets began retreating about 18,00 years ago, with rapid deglaciation by 15,000 years ago (late glacial interstadial) with similar temperatures as today leading to widespread distribution of deciduous woodlands across Europe. However, around 12,000 years ago the temperatures plunged downwards and by 11,500 years ago glacial conditions occurred with temperatures 6-7*C lower
Time line order
Era, period, epoch