Long-term atmospheric changes Flashcards

1
Q

Carbon dioxide

A
  • Carbon dioxide is an important ‘Greenhouse’ gas in Quaternary glaciations
  • CO2 plays a role in the synchronisation of Northern and Southern Hemisphere glaciations
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2
Q

Why does atmospheric CO2 decline during a glaciation?

(1) Chemical weathering

A

– Greater land area in glacial conditions
– Solution of rocks by carbonic acid locks up CO2
– Possibly 50 – 100 ppmv drop in CO2 concentration
attributable to chemical weathering

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3
Q

Why does atmospheric CO2 decline during a glaciation?

(2) Changes in oceans

A

– (a) Temperature change
– (b) Productivity of the oceans
» Light
» Nutrients

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4
Q

Changes in glacial oceans

(a) Temperature

A

• Oceans hold x60 more CO2 than atmosphere
• They control CO2 exchange with the
atmosphere
• Glacial oceans store even more CO2
• ….because CO2 is more soluble in colder water

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5
Q

Changes in glacial oceans

(b) Productivity

A
  • CO2 is used by plankton
  • Plankton dies and rains to ocean bottom continually
  • Plankton numbers increase in the glacial oceans drawing extra CO2 from the atmosphere
  • What causes plankton productivity to increase?
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6
Q

Ocean productivity

Abundance of plankton is
usually limited by availability of :

(1) Light

A
(1) Light
In a glacial period northern sea
ice pushes plankton belts to S
where sun is stronger
increasing productivity
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7
Q

Ocean productivity

Abundance of plankton is
usually limited by availability of :

(2) Nutrients

A

• Iron is usually in very limited supply in oceans
• It is an important nutrient
• The supply of iron increases in glacial
oceans

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8
Q

The effect of extra dust in the glacial atmosphere

A

• Dust not only generates greater productivity in the
oceans it also leads to:-
- Greater cloudiness = greater albedo
- consequent estimated cooling of 1oC

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9
Q

Dust in the atmosphere

A

• Dust is a source of condensation
nuclei
• The nuclei are important for cloud development
(if air humidity allows this)

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10
Q

Water vapour in the atmosphere

A
  • Normally super abundant in interglacial phases
  • Very effective greenhouse gas
  • Exchange with the oceans is very important
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11
Q

Level of water vapour greatly reduced because:

A

– cold air holds less vapour
– restricted evaporation from cold oceans
– sea ice formation prevents evaporation

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12
Q

The importance of water vapour in glaciation

A

• Ocean still quite warm during glacial build-up
• Only later does moisture starvation affect growth of ice
sheets
• Reduced water vapour is not likely to be an initiator of global cooling

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13
Q

The Holocene began

A

11,700 calendar years ago

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14
Q

The Ipswichian Interglacial occurred in Oxygen Isotope Stage

A

5e

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15
Q

The Quaternary is

A

2.6 million years old

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16
Q

In the late Quaternary ice ages have occurred with a pacing of approximately

A

100,000 years

17
Q

The eccentricity of the earth’s orbit is

A

the circularity of the orbit

18
Q

Ocean current upwelling predominantly occurs

A

In the Indian and North Pacific Oceans

19
Q

Orbital variations consist of:-

A
  • Eccentricity - c. 100 k yrs (circularity)
  • Obliquity - c. 42 k yrs (tilt of axis)
  • Precession - c. 21 k yrs (‘wobble of axis)
20
Q

Eccentricity is the weakest effect yet the ice

ages occur every

A

100,000 years

21
Q

At present the northern hemisphere mid winter occurs

A

at perihelion

22
Q

Perihelion is the point in the orbit when the Earth is

A

closest to the sun

23
Q

The positions of the seasons on the Earth’s orbit will be reversed after

A

10,500 years

24
Q

Summer solstice =

A

Hemisphere tilted directly

towards sun…produces longest day of year

25
Q

Equinox =

A

direction of axis side on to sun

26
Q

Aphelion =

A

Earth at most distant part of elliptical orbit

27
Q

Perihelion =

A

Earth closest to sun

28
Q

Increased algal blooms occur in the world’s oceans during glacial stages because

A

increased levels of iron enter the oceans, supplying a key nutrient

29
Q

In the last 800,000 years, CO2 typically peaks

A

at the start of an interglacial

30
Q

Eustatic sea level relates to

A

Global sea level change