Lecture 9- Ocean Circulation Flashcards

1
Q

wind belts

A

alternate direction

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2
Q

primary wind belts

A
  • polar easterlies
  • westerlies
  • northeast/ southeast trades
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3
Q

wind belt (0-30)

A

northeast trades

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4
Q

wind belt (30-60)

A

westerlies

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5
Q

wind belt (60-90)

A

polar easterlies

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6
Q

wind belt (0-30 S)

A

southeast trades

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7
Q

wind belt (30S - 60S)

A

westerlies

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8
Q

wind belt (60S - 90)

A

polar easterlies

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9
Q

ocean surface temperature

A
  • warmest water along the equator in the western ocean basins
  • coldest water along the pole
  • tongue of cold water in the eastern equatorial region
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10
Q

Atlantic ocean temperature at depth

A
  • warm thin surface layer
  • cold thick deep layer
  • thermocline separates warm and cold layers
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11
Q

ocean surface salinity

A
  • saltiest water in the subtropics
  • Atlantic considerably more salty than the other oceans
  • North Pacific the freshest of all regions
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12
Q

Atlantic Ocean salinity at depth

A
  • high salinity in surface ocean

- deep ocean salinity more uniform

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13
Q

rotation of subtropical gyres

A
  • clockwise in the northern hemisphere

- counter-clockwise in the southern hemisphere

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14
Q

subpolar gyres

A
  • rotate counter-clockwise in the northern hemisphere

- absent in the southern hemisphere

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15
Q

Antarctic circumpolar current

A

moves eastward around the Antarctic continent

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16
Q

Why is the Coriolis force needed?

A

needed to account for the acceleration of the reference coordinate system (Newton’s law F=ma doesn’t apply anymore)

17
Q

material is warmed when

A

it absorbs radiant energy (ie. solar energy)

18
Q

visible radiant energy from the sun

A
  • short wavelength radiation

- passes through the atmosphere without being heated

19
Q

Earth’s surface

A
  • absorbs a lot of the sunlight energy so it becomes warm

- warm surface radiates infrared radiation (long) which is absorbed by the atmosphere

20
Q

atmosphere is heated from

A

below

21
Q

atmospheric convection and precipitation is strongest

A

along the equator

22
Q

air column with high amounts of water vapor

A

weighs less (creates lower sea level pressure underneath it)

23
Q

sea level pressure at Pole (90 degrees)

A

high SLP

24
Q

SLP at 60 N/S

A

low SLP

25
Q

SLP at 30 N/S

A

high SLP

26
Q

SLP at equator

A

low SLP