Ocean Atmosphere Interactions Flashcards
Ocenan + atmosphere
- 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
Composition of the atmosphere
Nitrogen (78.1%), oxygen (20.9%), CO2, Argon, O3
Greenhouse effect
- 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 ____
Ozone layer
- upper atmosphere works as a filter for incoming ultraviolet radiation
Vertical structure of the atmosphere
weather we experience is in the troposphere and tropopause
[pic]
Atmospheric circulation - what are the main ingredients that affect atmospheric circulation?
- 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)
Solar energy distribution
- 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]
Why are the polar regions cold?
- 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
Albedo
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%
Why does abedo vary with latitude?
Abedo is a function of:
* angle of incidence (oblique angle more reflected)
* surface type (ice, snow, water, soil, clouds, etc)
Positive feedback: sea ice-abedo positive feedback
positive feedback: increases the intial change
negative feedback: reduces or counteracts the initial change
[pic]
Many important climate feedbacks between ocean and atmosphere
Heat budget as a function of latitude
Variations in heat recieved vs re-radiated at different latitudes
* the heat engine of atmospheric circulation
* this imbalance is compensated by ______
Uneven heating leads to ..?
vertical and horizontal air movement
net transport of heat from warm to cool regions
Evaporation/precipitation also play a role in transporting (redistributing) heat
Where water vapor is forming: absorption of latent heat
where water vapor condenses: release of latent heat