Definitions: Modules 11-15 Flashcards
winds
- air that is moving horizontally relative to Earth’s surface
- caused by the unequal heating of Earth’s atmosphere, creating a pressure gradient
- they blow in an attempt to equalize the imbalances in air pressure in the atmosphere
constant height maps
- smoothed and drawn relative to a constant elevation
- can be used to show variations in pressure at any altitude
constant pressure maps
- show variations in altitudes for a constant pressure
- high altitudes for a given pressure correspond to higher than normal pressures at a given latitude
- low altitudes for a given pressure correspond to lower than normal pressures at a given latitude
cyclone
- a centre of low pressure with a counterclockwise rotation in the Northern hemisphere and a clockwise rotation in the Southern Hemisphere
- creates surface convergence
anticyclone
- centre of high pressure with a clockwise rotation in the Northern hemisphere and a counterclockwise rotation in the Southern Hemisphere
- creates surface divergence
subgeostrophic flow
- when Coriolis force < PGF
- wind flows slowly
cyclostrophic
Coriolis force is negligible near the equator
supergeostrophic flow
- when Coriolis force > PGF
- wind flows quickly
Coriolis effect
- force caused by earth’s rotation
- only important for broad-scale winds
- northern hemisphere: Coriolis effect pulls to the right
- Southern Hemisphere: Coriolis effect pulls to the left
- with this effect, any free-moving object heading in any direction will appear to deviate from its path
one-cell model
assumes earth is covered by uniform water surface, sun’s directly overhead the equator, and earth doesn’t rotate
three-cell model
incorporates Earth’s rotation, assumes no land surface
polar front
polar jet occurs here, warm air from the Ferrell cell meets cold air from the Polar cell
ekman spiral
generated by surface currents that don’t move in the same direction as the wind and whose speed and direction isn’t uniform with depth
gyres
large-scale circular currents bounded by continents and turn under the Subtropical highs
thermohaline circulation
- slow circuit of deep currents, starting from 1km below the surface to the ocean bottom
- begins as surface currents reach the waters near Greenland
- it becomes colder, saltier, and more dense
- then water sinks to ocean depths in the high latitude waters of the North and South Atlantic
- forms deep water currents, coupled with slow surface circulation