Week 3 Flashcards

1
Q

AMOC

A

Atlantic Meridional Overturning Circulation

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2
Q

SMOC

A

Southern Meridional Overturning Circulation

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3
Q

The main path for deep ocean waters to return to the surface is through upwelling at the ________________.

A

Antarctic Divergence

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4
Q

The Antarctic Circumpolar Current (ACC) links _______, _________, and ________ basins.

A

Atlantic
Pacific
Indian

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5
Q

Upwelling at the ____________ brings deep-ocean, nutrient rich waters to the surface.

A

Antarctic Divergence (AD)

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6
Q

The formation of _____________ and ______________ brings some of these upwelled nutrients to low latitudes at intermediate depths.

A

Antarctic Intermediate Water (AAIW)
Subantarctic Mode Water (SMW)

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7
Q

Formation of _____________ along the coast, produces the densest water in the oceans, which sinks to seafloor and spreads northwards along the bottom.

A

Antarctic Bottom Water (AABW)

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8
Q

____________ is formed as NADW and AABW mix in the Southern Ocean.

A

Circumpolar Deep Water (CDW)

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9
Q

The western boundary currents of the _______ all carry warm waters poleward, while the eastern boundary currents move cooler waters towards equator.

A

subtropical gyres

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10
Q

Lots of ____________ along the poleward boundary of the subtropical gyres.

A

heat is release to the atmosphere

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11
Q

Semi-regular ____________, with the large changes to in the Pacific, but weaker impacts worldwide.

A

perturbation of the ocean-atmosphere system

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12
Q

During strong El Nino Souther Oscillation or ENSO events

A

weakening trades wings, weakens equatorial upwelling
coastal upwelling in CA, Ecuador, and Peru greatly reduced
Collapse of fisheries off CA, Peru, and Ecuador

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13
Q

_______ measure sea surface height (distance from satellite to ocean) with cm scale accuracy.

A

Satellite altimeters

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14
Q

The _____ is ice covered most of the year, with only partial melt back during summer months.

A

Arctic Ocean

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15
Q

The _______ (at lower latitudes than the Arctic) has a much bigger seasonal swing in sea ice cover.

A

Southern Ocean

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16
Q

Summer sea ice cover in the Arctic has been declining rapidly due to global warming. ___________ predict continuing decline.

A

Earth System Models (ESMs)

17
Q

Addition of anthropogenic CO2 is adding H+ ions, lowering ocean pH.
This is referred to as _____________.

A

ocean acidification

18
Q

The equilibrium constants Ki, for each of these reactions change with changes in _____, ________, and _________.

A

temperature
pressure
salinity

19
Q

Only the ______ influences the air-sea exchange of CO2.

A

dCO2

20
Q

Because CO2 gas combines chemically with water, the oceans have a great capacity to ___________, relatively much more so than for other gases such as Oxygen or Nitrogen.

A

absorb CO2

21
Q

The ____ and __________ gas in seawater are a function of ________, ______, __________, __________, and ___________.

A

pCO2
solubility of CO2
temperature*
[DIC]*
salinity
alkalinity
pressure
* means strongest influences

22
Q

Solubility is also influenced by ______ and _________.

A

alkalinity
salinity

23
Q

________ is a measure of the number of H+ ions required to neutralize the solutions (or of the solutions capacity to remove H+).

A

Alkalinity

24
Q

equation of the net flux of a gas (X) across the air-sea interface

A

Flux of X = K (pXair - pXseaw)

25
Q

The _________ (or ___________), _ , is often estimated as a function the Schmidt number and wind speed at a reference height (typically 10m)

A

Piston Velocity
transfer velocity
K

26
Q

_______________ is the time it takes to reach equilibration given a transfer velocity and initial gas concentrations in the air and water.

A

Equilibration Time

27
Q

The equilibration time for most gases (___ and ____) is relatively short, a couple of _______.

A

O2
N2
weeks

28
Q

The timescale for _____ is much longer (~______), because CO2 reacts chemically with the seawater

A

CO2
1 year

29
Q

IN EACH CASE THE ________ IN TEMPERATURE IS
CRITICAL IN DRIVING THE AIR-SEA FLUX.

A

CHANGE