Lesson Atmosphere and Pressure Flashcards
Easterly Winds
Near the Equator surface
Top of the troposphere
Westerly winds
Pressure = force/area
Pascals = N/m*m
100 Pa = 1 hPa = 1mb (millibar)
Ideal Gas Law
P=pRT
P Pressure
p density
R gas constant
T temperature
Pressure and Density, positive
Pressure and Temperature, positive
Temperature and density, negative
Pressure Gradient Force
Direction of air movement goes down the pressure gradient - high pressure to low pressure
mass x velocity x radius must remain constant
Coriolis Effect
Conservation of Angular Momentum
Winds away from the equator move slower in the rotation than winds near the equator
CF - objects go to the right in the N hemisphere - counterclockwise
Deflects left in S hemisphere
Only affects direction, not speed
Strength of deflection is proportional to the speed
Geostrophic Balance
PGF and Coriolis
PGF solely , always points high to low
Coriolis must be opposite and equal - points down
Friction
Main issues near the surface with topographic features
Turbulent eddies slow down wind flow
Only close to the surface of the Earth
Cyclone
Low pressure system
Convergence at the surface forces air to rise
^ | --> L < ----
Anticyclones
High Pressure system
—–>
Heating of the Earth
Low pressure at the equator - high temp, low pressure
High pressure at the poles - low temp, high pressure
Cold air sinks in high pressure
Warm Temp, low surface pressure
- less dense at surface, warm air expands and rises
Cold temp, high surface pressure
- more dense at the surface, cold air contracts and sinks