Week 8 LGM Flashcards

1
Q

When did the LGM occur?

A

23,000 – 19,000 BP, centred on ~21,000 ka BP

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2
Q

What is the LGM?

A

defined as ‘peak’ glacial conditions when ice sheets were largest and global temperatures were at a minimum.

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3
Q

When did the last glacial period occur?

A

115,000 – 11,500 years BP.

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4
Q

What does the LGM mrak?

A

the culmination of a nearly 100 kyr long glacial

period, during which ice-sheets had continued to build up.

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5
Q

What were the conditions during the LGM

A

icy, dry, cold, windy and sparsely vegetated

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6
Q

What was the insolation at mx ice sheets?

A

summer insolation had risen closer

to modern levels

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7
Q

what helped force LGM

A

Lower CO2
insolation
presence of ice sheets

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8
Q

What where global sea level during LGM?

A

110-125 m lower than today

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9
Q

How much of the world was covered by ice sheets today and in the LGM?

A

10% today

25% LGM

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10
Q

Which ice sheet was the largest in NH?

A

The North American ice sheet (Laurentide and Cordilleran) was the largest accounting for 55%
of the extra ice volume.

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11
Q

What did the presence of large ice sheets impact?

A

sea level, atmospheric circulation and

vegetation

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12
Q

What are loess fields?

A

large amounts of dust deposited from a glacier

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13
Q

What did the presence of ice sheets do?

A

generated large

amounts of dust leading to the formation of loess fields

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14
Q

Why do ice sheets cause more dust?

A

Ice sheets grind across the landscape, scraping and
dislodging soils, producing large amounts of debris
(boulders to fine clay).

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15
Q

Where did dust in Antarctica come from?

A

predominantly from Patagonia.

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16
Q

Where did dust in Antarctica come from?

A

eastern Asia

17
Q

How much dust is in glacials what causes these dust levels?

A

10 x more dust
result of a more turbulent atmosphere
greater production of debris
a drier climate.

18
Q

What was the global temperature in the LGM?

A

Global temperatures were 3-8 °C cooler than today

19
Q

Where was cooling greatest in the LGM?

A

polar regions
Greenland was 21-25 °C cooler than the present.
•Antarctica was 7-10 °C cooler than the present.

20
Q

How was Sea surface temperature affected?

A

North Atlantic was at least 8°C cooler

Other regions may actually have been warmer

21
Q

How did atmospheric circulation change during LGM?

A

meaning sites in the north had reduced precipitation,

and those further south had enhanced precipitation

22
Q

How can we tell what happened with vegetation in the LGM?

A

using pollen preserved in lake sediments

reflect the average composition of vegetation

23
Q

What was the total biomass in the LGM?

A

Total biomass on Earth was 25% less than

today

24
Q

How much cooler where tropic oceans during LGM?

A

4-6°C cooler than present

mountain regions were 4-6°C cooler than present