Hydrosphere 2 session 1 Flashcards

1
Q

What factors are there to note with the keeling curve?

A

exponential increase since 1960s
not straight in annual variations

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2
Q

When did measurements for the keeling curve in Mauna Loa begin?

A

March 1958

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3
Q

What was the carbon mystery

A

60% C emission went into atmo but where was other 40%

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4
Q

Where has carbon released by humans gone?

A

majority atmo
then almost even split between:
Land (highly variable)
Sea

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5
Q

What is the atmosphere like as a reservoir?

A

relatively small and subject to large fluxes
like “middle man” showing changes in land or sea

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6
Q

Where is ocean uptake of Carbon highest?

A

North Atlantic near arctic

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7
Q

Why is carbon uptake by the ocean so great near the arctic?

A

Cold area with colder water being able to store more gas
Formation of deep water (sinking) so more pulled in

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8
Q

What is the chemical change for the oceans as they absorb more carbon?

A

reduce pH- acidification

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9
Q

What law is there for Air-sea gas?

A

Henrys law

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10
Q

What does henrys law mean?

A

pCO2= partial pressure co2
K0= constant changes with temp or salinity
[co2]= co2 in aqueous

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11
Q

How does water temp affect gas solubility?

A

warmer less soluble
Colder more soluble

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12
Q

How much more co2 can ocean store than atmo?

A

50 times more

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13
Q

What is happening to oceans ability to absorb CO2?

A

weakening as temp increase

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14
Q

How does henrys law explain thermal pollution?

A

solubility of oxygen decreases rapidly as temp increases (harmful to biota- oxygen minimum zones)

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15
Q

What does future CO2 uptake into oceans depend on?

A

CO2 concentration in the surface ocean

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16
Q

how long does it take to fully sequester an emission of carbon?

A

hundreds of thousands of years

17
Q

What will be most affected by ocean acidification?

A

organisms with CaCO3 exoskeleton as wont form in low pH

18
Q

What are the 2 most important variables for using past co2 events as analogues for the future?

A

Mass
Rate

19
Q

Why do we care about the mass of CO2 emissions?

A

Determines how much climate change

20
Q

Why do we care about the rate of carbon emission?

A

Determines whether life can keep pace via adaptation/migration
Determines whether emissions outpace natural Earth recovery mechanisms

21
Q

What are the big 5 mass extinction events?

A

End Ordovician
Late Devonian
End-Permian (‘Great Dying’)
End-Triassic
End-Cretaceous (RIP non-avian dinos)

22
Q

What mass extinction events are more frequent/ applicable to modern emissions?

A

Large Igneous provinces

23
Q

How can large igneous provinces release carbon?

A

Might be trapped in the magma and then released due to not crystallising
Province might come into contact with carbon rich rock and burn (coal)

24
Q
A