Ocean Atmosphere Interactions Flashcards

1
Q

Ocenan + atmosphere

A
  • Intimately connected through:
    -exhcange of water
    -gas exchange
    -energy transfer
  • This interaction:
    -controls sea surface temp
    -moderates earth’s weather and climate
    -creates waves and currents
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2
Q

Composition of the atmosphere

A

Nitrogen (78.1%), oxygen (20.9%), CO2, Argon, O3

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3
Q

Greenhouse effect

A
  • the Earth’s heat blanket
  • Incoming sunlight is converted from visible light to radiated heat, which is in the longwave spectrum
  • greenhouse gases work as a heat trap for the outgoing infrared (IR) radiation
  • some of that heat is re-radiated as infrared radiation from the Earth is absorbed by the greenhouse gases ____
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4
Q

Ozone layer

A
  • upper atmosphere works as a filter for incoming ultraviolet radiation
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5
Q

Vertical structure of the atmosphere

A

weather we experience is in the troposphere and tropopause
[pic]

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6
Q

Atmospheric circulation - what are the main ingredients that affect atmospheric circulation?

A
  • energy from the sun (the engine)
    -global distrubution of solar heating is uneven due to: seasonal variations, angle of sun over horizon, transparency of atmosphere, local reflectivity
  • Earth’s rotation (the modifier)
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7
Q

Solar energy distribution

A
  • solar heating is uneven in a spherical planet
  • diffuse radiation at high latitudes
  • Concentrated radiation at low lats
  • seasons are caused by tilt of the earth’s axis by 23.5 degrees, heating is uneven seasonally
  • [pic]
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8
Q

Why are the polar regions cold?

A
  • solar insolation/area is lower at poles (energy spread out over larger area)
  • more attenuation through atmosphere
  • higher albedo in polar regions: more reflected energy
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9
Q

Albedo

A

percent of solar radiation reflected back to space
reflectviity of earth’s surface
contributes to keeping the earth cool
average for earth = 30%, ice sheets = 85%, oceans = 7%

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10
Q

Why does abedo vary with latitude?

A

Abedo is a function of:
* angle of incidence (oblique angle more reflected)
* surface type (ice, snow, water, soil, clouds, etc)

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11
Q

Positive feedback: sea ice-abedo positive feedback

A

positive feedback: increases the intial change
negative feedback: reduces or counteracts the initial change
[pic]

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12
Q

Many important climate feedbacks between ocean and atmosphere

A
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13
Q

Heat budget as a function of latitude

A

Variations in heat recieved vs re-radiated at different latitudes
* the heat engine of atmospheric circulation
* this imbalance is compensated by ______

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14
Q

Uneven heating leads to ..?

A

vertical and horizontal air movement
net transport of heat from warm to cool regions

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15
Q

Evaporation/precipitation also play a role in transporting (redistributing) heat

A

Where water vapor is forming: absorption of latent heat
where water vapor condenses: release of latent heat

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16
Q

Vertical air moevment

A
  • air expands when heated, becomes less dense, and rises
  • it keeps rising until it reaches the same density –> level of neutral buoyancy
  • when the air cools it contracts and sinks again
17
Q

Horizontal air movement

A

air flows from high to low pressure
uneven solar heating –> areas of high & low pressure (density)
–> a force (the pressure gradient force) that drives the air from high to low pressure
(air does not always go in the direction of this force)

18
Q

Global air circulation

A

On a fictional, non-spinning Eath: a simple cell on each hemisphere, drivem by the pole-to-equator pressure gradient force
But on a rotating planet…

19
Q

The Coriolis “force”

A
  • Critical to atmospheric and ocean cirulation
  • due to the rotation of Earth on its axis
  • deflects moving air or water from its initial course
    (to the rifht in the NH, left in the SH)
  • deflection increases with latitude (no coriolis at equator, strong at the poles)
  • acts over long timescale (10+ hrs) and long distances (1+ km)
20
Q

Movement on a rotating disk

A
21
Q

Coriolis force effects

A
  • only changes the direction by deflecting to left/right, but does not change speed
  • only has an impact on motions that are slow and travel over long distances
  • important for ocean currents
22
Q

common misconceptions about coriolis force

A
  • acts equally on motions to the north/south or east/west - wrong, deflects same amount in any direction
  • not a real force, just an artifcat of looking at motion from a rotating reference frame
23
Q

Why do hurricanes spin CCW in NH but CW in SH?

A
  • low pressure system surrounded by higher pressure
    *
24
Q

Atmispheric circulation on rotating earth

A

coriolis deflection on rotating Earth produces three circulation cells in each hemisphere
Note: coriolis does not cause the wild, it impacts the direction

25
Q

Surface wind pattenrs

A
  • the bottom part of the three atmospheric ciruclation cells is what produces the global wind pattern
    Easterlies (trade winds and polar easterlies) go from east to west
    westerlies: go from west to east
26
Q

Intertropical convergence zone (ITCZ)

A
  • warm air rises at the equator where the two hadley cells meet, causing low pressure in the tropics and a zone of ______
27
Q

Cloud formation

A
  • a cloud is a parcel of air that contains condensed water
  • the amount of water that air can hold depends on the mp
  • as warm air rises it cools and water condenses to form clouds
  • ____
28
Q

Wind belts, pressure systems, and weather

A

[pic]