week 10 lecture Flashcards
What are the drivers of climate change of the last
1000 years?
Orbital forcing
• Solar variability
• Volcanic eruptions
• Internal climate variability
• Land use / Land cover change
• Greenhouse gases
• Aerosols
• Feedbacks
How would climate change over the last 1000years be characterised?
Changes are relatively small
• High regional variability
• Focussing in on centennial, decadal and annual
variability
What archives are used for studying last 1000years?
- Tree rings
- Mountain glaciers
- Corals
- Speleothems
What is the impact of volcanic eruptions?
- *Dust and Ash** can block sunlight causing temporary cooling effect
- *Sulphur dioxide (SO2)** reflect incoming solar radiation has significant cooling effect
- *Greenhouse gas**: warming effect
What is solar varibility and what is its effect?-2
11 year sunspot cycle
small total effect around 1Wm-2
What is the Medival climate Anomaly?
Warm period in Europe and North Atlantic, temperatures 0.3-1.0 ℃ higher than 1960-1990
• Some areas were cooler than today - eastern tropical Pacific Ocean
When did the medival warm period occur?
1000 to 1300 AD (European Middle Ages), possibly earlier
When did the little ice age occur?
1450-1850
What caused the little ice age?
multiple volcanic eruptions over a 50 year period
sea ice-albedo feedback.
Solar irradiance also lower during this period.
What where the features of the little ice age?
Colder winters and shorter growing season in northern Europe led to failed crops and local famine
- Lakes, rivers and ports in Northern Europe froze
- Abandonment of settlements in Greenland
What ended the little ice age?
Likely the industrial revolution as natural cylceles would indicate it ending 50 years latter than it did?
What is the Holocene period
The current interglacial period
11,650 years BP to present
What are the drivers of climate varibility in the holocene?
- Changes in insolation
- Volcanism
- Solar irradiance
- Atmosphere – ocean interactions
- Atmosphere – vegetation interactions
What is the holocence Thermal Maximum?
The period of peak warmth during the Holocene
When did the holocence thermal maximum occur?
~9-5 kyr BP
soon after the ice sheets melted enough to reduce their chilling effect on climate,
• but before renewed cooling due to falling insolation.