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
What does a Weak AMOC cause?
``` stadial conditions • Reduced northward heat transport leads to cooler conditions in the North Atlantic • Reduced meltwater • Surface salinity slowly increases ```
26
What is the Underlying cause of AMOC changes?
changes are related to the influx of freshwater due to ice sheet melt and calving around the North Atlantic
27
Why do we not see Dansgaard-Oeschger | events during interglacial periods?
The presence of continental ice is important | • Dansgaard-Oeschger events occur within a particular CO2 range