Linking ocean physics / biology / chemistry Flashcards

1
Q

What can be used to trace water masses in the deep ocean?

A

Phosphate concentration (As decomposition enriches the deep ocean with nutrients.)

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2
Q

Put these ocean masses in order from surface to depth - NADW, Antarctic Intermediate water, Mediterranean outflow, Antarctic Bottom Water.

A

Mediterranean outflow > Antarctic Intermediate Water > North Atlantic Deep Water > Antarctic Bottom Water.

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3
Q

What increases with age of water and why?

A

The nutrient concentration - as it becomes more enriched by decomposition.

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4
Q

What can nutrient concentration tell you about the North Pacific compared to the South?

A

It is older and filled with deep waters.

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5
Q

Globally, both surface and deep concentrations of nitrate and phosphate are very similar. What do they reflect?

A

Surface concentrations reflect upwelling (so higher concentration in equatorial / coastal regions and high latitude winter mixing zones).
Deep water concentrations reflect the movement of deep water masses (Therefore high in the North Pacific, South Atlantic and Indian oceans - and lower in the South Pacific, North Atlantic and Southern ocean).

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6
Q

Given our knowledge of the oxygen cycle compared to other nutrients, what is its distribution in the ocean?

A

Opposite to phosphate - and decreases with age of water masses.

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7
Q

At what concentration is an oxygen minimum zone declared? Where are these prevalent?

A

[O2] < 50µmol O2 per litre. Found in the equatorial east pacific and indian oceans.

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8
Q

Why do concentrations of nitrogen and phosphorus vary together in a 16-proportion in the ocean? (N:P = 16:1)

A

Because decomposition, and photosynthesis at the surface, both occur in Redfield proportions, and dominate both the nitrogen and phosphorus cycles in the ocean.

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9
Q

Why do some observations of nitrogen and phosphate concentration plotted against each other, not follow the slope/redfield ratio of 16?

A

These coincide with low oxygen areas as when decomposition occurs in anaerobic conditions, denitrification occurs, as bacteria start to use NO3- instead. Therefore the observations show low levels of nitrogen.

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10
Q

What process is active in oxygen minimum zones?

A

Denitrification

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11
Q

What is the condition for a phosphorus limitation?

A

[NO3-] > 16x[PO43-]

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12
Q

What limitation is experienced by most of the ocean, if only marginally? What is the condition for this?

A

Nitrogen limitation, where [NO3-] < 16x[PO43-]

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13
Q

Why is the N:P ratio of phytoplankton almost identical to the one of seawater?

A

Conicidence? - they are not exactly equal, seawater is 1:15 not 1:16
Adaptation of phytoplankton - changed their elemental ratio to match the environment.
Regulation by phytoplankton - Redfield argued that they control seawater concentration.

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14
Q

Why does the redfield ratio not characterise nitrogen fixers / what does?

A

They are independent of common nitrogen forms, their growth is slower as N2 triple bond is energy demanding, they live in nitrogen-limited and nutrient poor environments.

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15
Q

How do nitrogen fixers control the chemical composition of the ocean?

A
  • A net biological uptake of PO43- occurs in the absence of NO3-
  • Nitrogen fixers work to draw N2 gas into the ocean and increase [NO3-] until = 16x[PO43-] at which point nitrogen fixers die off.
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16
Q

What do cells take in via their membrane in the ocean, and how does the SA:V affect this?

A
  • Take in DIC, DIN, PO3-. The higher the SA relative to Volume, the better the uptake.
17
Q

SA:V can be calculated as equal to what? This means that smaller organisms do better in what type of environment?

A

3/r. As this shows SA:V is inversely proportional to cell size, smaller organisms do better in oligotrophic, low nutrient environments.

18
Q

How does the SA:V explain the distribution of prochlorococcus and synedochus in the oceans?

A

As they are the smallest phytoplankton, therefore having the largest SA:V ratio, they are found in the nutrient limited waters (of between 30 degrees N/S).

19
Q

What is proximate limiting and ultimate limiting?

A

Proximate limiting = short term, local

Ultimate limiting = long term

20
Q

Why is there high anthropogenic CO2 concentration along the NW Atlantic and E American coasts?

A

Due to the newly formed NADW current

21
Q

Where is surface C02 highest and why?

A

The subtropical Atlantic, as Revelle factor is lowest here - warmer, less alkaline.

22
Q

State the three key reasons why the North Atlantic has high vertical penetration?

A
  • Ventilation of the main thermocline
  • Deepwater formation
  • Flow patterns of lower thermohaline circulation (involves flow of waters from the southern hemisphere, modification and convection of these waters, and outflow in a thick deep layer)
23
Q

Why is air/sea gas exchange inhibited in S. Atlantic?

A

Short residence time of surface waters, as well as dilution of deep and bottom waters by subsurface mixing.

24
Q

What is CO2 air/sea flux a function of?

A

pCO2 difference and transfer velocity (the diffusivity of gas in water and effect of physical processes -turbulence - within the boundary layer).

25
Q

What is the transfer velocity rate determined by?

A

The difference in DIC across the top and bottom of the water boundary layer. Rate of diffusion increases with temperature.

26
Q

Which ocean is the most saline?

A

The North Atlantic.