week 10 lecture Flashcards

1
Q

What are the drivers of climate change of the last
1000 years?

A

Orbital forcing
• Solar variability
• Volcanic eruptions
• Internal climate variability
• Land use / Land cover change
• Greenhouse gases
• Aerosols
• Feedbacks

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2
Q

How would climate change over the last 1000years be characterised?

A

Changes are relatively small
• High regional variability
• Focussing in on centennial, decadal and annual
variability

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3
Q

What archives are used for studying last 1000years?

A
  • Tree rings
  • Mountain glaciers
  • Corals
  • Speleothems
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4
Q

What is the impact of volcanic eruptions?

A
  • *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
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5
Q

What is solar varibility and what is its effect?-2

A

11 year sunspot cycle

small total effect around 1Wm-2

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6
Q

What is the Medival climate Anomaly?

A

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

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7
Q

When did the medival warm period occur?

A

1000 to 1300 AD (European Middle Ages), possibly earlier

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8
Q

When did the little ice age occur?

A

1450-1850

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9
Q

What caused the little ice age?

A

multiple volcanic eruptions over a 50 year period

sea ice-albedo feedback.

Solar irradiance also lower during this period.

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10
Q

What where the features of the little ice age?

A

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
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11
Q

What ended the little ice age?

A

Likely the industrial revolution as natural cylceles would indicate it ending 50 years latter than it did?

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12
Q

What is the Holocene period

A

The current interglacial period

11,650 years BP to present

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13
Q

What are the drivers of climate varibility in the holocene?

A
  • Changes in insolation
  • Volcanism
  • Solar irradiance
  • Atmosphere – ocean interactions
  • Atmosphere – vegetation interactions
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14
Q

What is the holocence Thermal Maximum?

A

The period of peak warmth during the Holocene

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15
Q

When did the holocence thermal maximum occur?

A

~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.

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16
Q

Is the timing of the holocene thermal maximum constant?

A

No: timing of maximum warmth varies regionally, depending on when nearby ice melted

17
Q

What is the 8.2 ka Event?

A

A period of abrupt cooling of North Atlantic and northern hemisphere

is Largest climate excursion during Holocene

18
Q

How long did the 8.2Ka Event last for?

A

Occurred 8.2 ka BP, lasting for ~160 years

19
Q

What where the conditions of the 8.2 Ka event?

A

Cold, dry and dusty

Decrease in temperature (of 3.3± 1.1 °C) and snow accumulation in Greenland

Increase in dust and forest fire frequency

Decrease in methane

20
Q

What caused the 8.2Ka event?

A
  • Outburst of final drainage proglacial lake Agassiz and Ojibway ~ 8.45 ka BP
  • Lakes drained into Labrador sea in space of 0.5 – 5 years, having a cooling effect.
  • Likely slowing of the Atlantic Meridional Overturning Circulation (AMOC)
21
Q

What event is the 8.2 ka simlur too and why?

A

Somewhat similar to the Younger Dryas due to Similar mechanism, but shorter lived and smaller in magnitude

22
Q

What has Northern hemishpere summer insolation been doing throughout the holocene?

A

Northern hemisphere summer insolation has been slowly decreasing throughout the Holocene, since a peak ~10 kyr BP

23
Q

How much higher was the summer insolation during the 10kyr peak?

A

10 kyr BP NH summer insolation was ~8% higher than today

24
Q

When does the Northern hemishpere experiance summer?

A

at the aphelion

25
Q

What where monssons like 9000 years ago relative to today?

A

Stronger across northern tropical

Green Sahara period

26
Q

How does the holocence compare to past interglacials?

A

Both MIS 5e and MIS 11c were globally warmer than the Holocene