Cryosphere 3- Case-studies – ice-sheet influence on ocean currents and heat transport Flashcards

1
Q

What causes the release of heat from the North east Atlantic?

A

Gulf stream
North Atlantic drift

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2
Q

What is responsible for heat movement to higher latitudes?

A

Atmosphere

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3
Q

What is one of the main ocean drivers of the gulf stream/ North Atlantic drift?

A

Squeezing on the edge of gyre systems

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4
Q

What processes cause the movement of heat to the atmosphere from the ocean?

A

Evaporation and latent heat

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5
Q

What is another name for the movement of heat via the gulf stream and north Atlantic drift?

A

Thermohaline circulation

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6
Q

What is thermohaline circulation?

A

when currents are driven by heat (thermo) and salinity (hals)

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7
Q

Why are the surface waters of the Nordic and Labrador sea unusual?

A

they become dense enough to sink to depths below 2 km (during winter
time) sinking compensated by influx warmer equatorial water

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8
Q

What is North Atlantic drift?

A

when the gulf stream extends across the Atlantic

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9
Q

What is the average depth of the ocean and does wind interact with this?

A

4000m deep wind can only affect 1000m

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10
Q

What does wind only affecting 1000m depth of ocean mean must be the driver of deep ocean currents?

A

varying temp and salinity and how this affects their density

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11
Q

What can the movement rate of deep ocean currents be across an ocean basin?

A

decades to centuries

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12
Q

What outflow adds salinity and thus increases density further driving north Atlantic drift?

A

Mediterranean (which is warm but doesn’t sit on surface due to high salinity and thus density)

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13
Q

What is brine rejection?

A

when salt water freezes salt is expelled as brine

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14
Q

What happens when brine is rejected?

A

drains into ocean in narrow channel due to cold and saline sinks in plume which freezes water it comes into contact with

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15
Q

What was North Atlantic drift like during summer in the LGM?

A

algae records suggest warm surface water open up sea ice in Nordic sea
Deep currents for thermohaline circulation dont form

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16
Q

What was North Atlantic drift like during winter in the LGM?

A

Warm surface currents and thermohaline circulation pushed south and northward heat transport is greatly reduced from 30°N

17
Q

What will happen if their is sediment instead of rock under a glacier?

A

will deform easier allowing quicker movement
Thought quaternary ice sheet margin were prone to collapse

18
Q

How do Heinrich events/ layers form?

A

Wind from Sahara can carry fine sand but not coarse sand or gravel but icebergs are the only thing that can carry larger material

19
Q

What is a H event?

A

a dramatic collapse or increase in freshwater slowing or stopping North Atlantic drift to higher latitudes

20
Q

What was N. Atlantic circulation during a H event?

A

Lid of cold freshwater laden with interrupted ocean conveyor system
Climate affected
Air passing across ice field causes temp on land to plummet

21
Q

What are Heinrich events associated with?

A

Coldest phases of last glacial and ice berg release

22
Q

What are D/O cycles?

A

rapid warming and cooling through last glacial

23
Q

What does DO cycles stand for?

A

Dansgaard-Oeschger cycles

24
Q

What is the length of the cold warm period of D/O cycles?

A

1-2kyr

25
Q

Where can D/O cycle evidence be found?

A

First in Greenland ice cores
marine and terrestrial records
intense in North Atlantic regions

26
Q

What was the younger dryas?

A

last big climatic event of the late Quaternary before the Holocene

27
Q

When was the younger dryas?

A

return towards glacial conditions 12.9 to 11.65ka

28
Q

What was the younger dryas responsible for in the UK?

A

Loch Lomond stadial

29
Q

What was the younger dryas caused by?

A

massive flow glacial meltwater in north Atlantic which restricted overturning circulation

30
Q

Where was the largest meltwater/ iceberg discharge?

A

into Arctic via NW passage

31
Q

What was the 8.2 ka event?

A

The biggest climatic event in the Holocene in the N Atlantic region

32
Q

How was the 8.2 ka event like compared to the younger dryas?

A

less severe

33
Q

What do Greenland ice cores show the 8.2ka event was like?

A

cold (less accumulation, lower d 18 O,
windy (more salts (Cl-) and dust (Ca2+ )
dry (decreased CH 4 )

34
Q

What are tipping points?

A

points in earths climate where one change can lead to uncontrolled runaway climate change

35
Q
A