Lecture 19: Southern Ocean, formation of the ACC Flashcards

(14 cards)

1
Q

What is the physical definition of the Southern Ocean?

A

Everything south of the Antarctic Convergence or within and south of the Antarctic Circumpolar Current (ACC).

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2
Q

What is the political definition of the Southern Ocean?

A

The region between 60°S and the coast of Antarctica.

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3
Q

What is the Antarctic Circumpolar Current (ACC)?

A

A massive, wind-driven geostrophic current encircling Antarctica, connecting all major ocean basins.

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4
Q

What drives the Antarctic Circumpolar Current?

A

Strong circumpolar westerly winds.

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5
Q

What are the two major gyres south of the ACC?

A

The Ross Sea Gyre and the Weddell Gyre.

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6
Q

How does Ekman transport influence vertical water movement in the Southern Ocean?

A

It causes divergence that drives deep-water upwelling along sloping isopycnal surfaces.

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7
Q

What is upwelling and where does it occur in the Southern Ocean?

A

Upwelling is the rise of deep waters to the surface, driven by wind-induced divergence, especially under the westerlies.

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8
Q

What are isopycnals?

A

Surfaces of equal potential density.

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9
Q

What is baroclinity?

A

The condition where isopycnals and isobars are not aligned, leading to vertical mixing and instability.

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10
Q

What causes diapycnal mixing?

A

Instability from baroclinic conditions, which moves water across isopycnal layers.

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11
Q

What is the role of the Southern Ocean in the global climate system?

A

It closes the global ocean circulation, absorbs a large fraction of anthropogenic CO₂ and excess heat, and supports unique ecosystems.

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12
Q

What are typical wind patterns around Antarctica?

A

Westerlies over the ACC and coastal easterlies near the continent.

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13
Q

What is the relationship between wind, Ekman transport, and upwelling in the Southern ocean?

A

Westerly wind causes northward Ekman transport, leading to divergence and upwelling of deep water.

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14
Q

What does static stability depend on in the ocean?

A

The vertical gradient of density; positive gradient = stable, negative = unstable.

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