Lec 6. Global Energy Movement Flashcards

1
Q

how is solar radiation distributed across the globe

A

It is concentrated at the equator, but it stretches near the “top” North and “bottom” South, the area absorbing the energy is greater at the poles

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2
Q

how does solar radiation distribution impact the global energy?

A
  • it creates energy surpluses and deficits.

At the poles; Energy emitted as IR radiation is greater than solar radiation being absorbed.

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3
Q

At what latitude is there an energy deficit (negative net radiation) ?

A

above 35° lattitude !

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4
Q

why are areas above the 35° latitude not cooling down if they have an energy deficit?

A

It has to do with the global systems that are in place; that transfer surplus heat from the equator to the colder regions at the higher lattitudes

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5
Q

What are the 2 main systems that move the energy surplus ?

A

Atmospheric circulation
Oceanic circulation

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6
Q

What are the 4 types of movement that are part of the atmospheric circulation?

A
  1. pressure-driven air movement
  2. landform-driven air movement
  3. rotation driven air-movement
  4. water vapor transport
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7
Q

What are the 2 currents found in the oceanic circulation?

A
  1. Surface ocean currents
  2. Deep ocean currents
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8
Q

what is air pressure?

A

the weight of molecules pressing down on each other in the atmosphere

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9
Q

How does air move when it is under high pressure?

A

it gets pulled towards the areas with lower pressure

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10
Q

what is the relation between temperature, air, density and pressure

A

Pressure = Density x (constant) x Temperature

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11
Q

what is an air parcel?

A

an area of air that is of a different temperature or pressure than the surrounding air

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12
Q

What is the initial cause of pressure-driven air movement?

A

the uneven distribution of solar radiations on the planet

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13
Q

why is there snow on top of mountains even in the equator?

A

Because of landform-driven air movement, Higher reliefs of landforms force parcels of air higher into the atmosphere,
As air is forced upwards:
- Decrease in pressure, molecules in. the air expand, they lose energy, air becomes colder

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14
Q

How does the rotation of the planet affect air movement?

A

Mouvement which would normally be straight actually curves with the rotation of the planet (the Coriolis effect)

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15
Q

Do they release or take in energy?
1. Evaporation
2. Condensation

A
  1. takes in
  2. releases
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16
Q

when is condensation common in the atmosphere?

A
  1. air temperatures decrease
  2. where air rises and expands
17
Q

what are common scenarios where condensation happens?

A
  • circulation cells where warm and humid air rises, and as a result expands and cools
  • on the side of a high landform as an air parcel is pushed vertically upwards and cools
  • at night, as air temperatures decrease in response to the loss of incoming solar radiation
18
Q

what are the 3 main circulation cells

A
  1. Hadley Cell
  2. Ferrel Cell
  3. Polar Cell
19
Q

What is the Polar cell?

A

It starts at 60° north and south and ends up falling at the polar regions
much colder but enough of an energy different to drive a circulation cell

20
Q

What is the Hadley Cell?

A

It is the big circulation cell
starts at the equator
goes 30° north and south
relatively free of water vapor

21
Q

What is the Ferrel Cell?

A
  • rises at 60° and falls at 30°
  • moves in the opposite direction of the Hadley and Polar
  • driven by the movement of the Hadley and the Polar
  • weaker and more variable
22
Q

what are surface winds?

A
  • global pattern of movement of air in the atmosphere
  • driven by circulation cells and the rotation of the planet (Coriolis effect)
23
Q

what are surface currents driven by?

A

surface winds

24
Q

what do landforms do to currents?

A

they can trap or deflect currents

25
Q

what are the differences that drive deep ocean circulation?

A

it is driven by differences in water density (impacted by temperature and salinity)

26
Q

what is the cause of ocean salinity?

A

minerals weathered from land and both evaporation and ice formation in the ocean

27
Q

what is the major driver behind deep ocean circulation?

A

cold polar regions
- colder water (dense)
- greater salinity (driven by ice formation)

28
Q

why does adding salt to roads delay ice formation?

A

because as ice forms, salts and minerals need to be left behind

29
Q

how does ice formation lead to greater salinity levels?

A

The water left behind by ice formation has a higher salinity because when ice forms, salts and minerals are left behind

30
Q

what is the thermohaline circulation?

A

it is the coming together of the surface currents and the deep ocean currents, forming a global circulation of oceanic currents

salt temperature driven circulation