Week 7 part 2 Flashcards

1
Q

What does Millennial scale mean?

A

lasting for a few thousand years
• Some changes happened within decades
> Relevant to a human life span

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2
Q

Where do Dansgaard-Oeschger Events occur?

A

Greenland

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3
Q

Where do Heinrich Events occur?

A

North Atlantic Marine sediment

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4
Q

Where do Antarctica Isotopic Maxima Events occur?

A

Antarctica

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5
Q

What happens in a Dansgaard-Oeschger Event?

A

sharp spikes in d18O indicate temperature changes

of up to 15C

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6
Q

How many Dansgaard-Oeschger Events over the last glacial period?

A

Over 25 events during the lastglacial period

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7
Q

What is a Interstadial?

A

warmer period in otherwise cold glacial climate

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8
Q

Waht is a Stadial?

A

coldest glacial conditions

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9
Q

What is the pattern of Dansgaard-Oeschger Events?

A
saw-tooth shaped pattern
Abrupt warming of up to 15C
Warmer ‘interstadial’ persists for 100’s to 1000’s years
Gradual cooling
random in time and duration
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10
Q

What are the characteristics of Greenland ice?

A

Long and continuous

  • High resolution – sub-decadal to annual resolution
  • Multiproxy
  • Excellent replication between different ice cores
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11
Q

What are the large ice berg discharge

events known as?

A

Heinrich Events

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12
Q

How many Heinrich Events have there been?

A

6

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13
Q

How are henich events recorded?

A

as layers of coarse-grained sediments derived

from the land.

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14
Q

What are heinrich events evidence for?

A

Evidence of an increase in iceberg discharge and a

southward extension of cold polar waters

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15
Q

How long do heinrich events last?

A

Events last between 200 and 2000 years

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16
Q

what is the Relationship between Heinrich and

Dansgaard-Oeschger Events

A

Heinrich Events occurred during coldest intervals
in Dansgaard-Oeschger Events
but not every Dansgaard-Oeschger Events

17
Q

how often where Heinrich events?

A

every 10,000 years

18
Q

What is Dansgaard-Oeschger and Heinrich Events footprint

A

near global
temperature and precipitation changes in North America and Europe
monsoon variations

19
Q

What where the vegetation changes in Europe during Dansgaard-Oeschger and Heinrich Events?

A
  • Repeated expansion and contraction of temperate forests

- Changes occurring over centuries

20
Q

When did the Asia summer Monsoon strengthen?

A

Asian Summer Monsoon strengthened during warming events (interstadials) in Greenland

21
Q

How are Antarctic millennial scale changes different from those in greenland?

A

smaller in size , warmings are less abrupt
Warming in Antarctica lags cooling in Greenland by ~200 years
warming in Antarctica occurred when Greenland had reached peak cold temperatures
Bipolar seesaw pattern

22
Q

Why are Antarctica and Greenland out of phase?

A

due to AMOC

23
Q

What are Antarctic millennial scale called?

A

Antarctica Isotopic Maxima (AIM)

24
Q

What does a Strong AMOC cause?

A
interstadial conditions
• Enhanced northward heat transport
• Ice sheets around North Atlantic start to
melt
• Surface salinity slowly reduces
25
Q

What does a Weak AMOC cause?

A
stadial conditions
• Reduced northward heat transport leads
to cooler conditions in the North Atlantic
• Reduced meltwater 
• Surface salinity slowly increases
26
Q

What is the Underlying cause of AMOC changes?

A

changes are related to the influx of freshwater
due to ice sheet melt and calving around the North
Atlantic

27
Q

Why do we not see Dansgaard-Oeschger

events during interglacial periods?

A

The presence of continental ice is important

• Dansgaard-Oeschger events occur within a particular CO2 range