Meteorology Study Notes
Key Meteorological Concepts
Terms:
Advection: Horizontal movement of air.
Convergence: Air parcels moving closer to each other.
Divergence: Air parcels moving away from each other.
Convection: Upward motion associated with low pressure.
Subsidence: Downward motion associated with high pressure.
Global Circulation
Formation: Insolation causes unequal heating, creating three circulation cells:
Tropical cell (Hadley Cell) around the equator.
Mid Latitude (Ferrell) cell between tropics and poles.
Polar cell at the poles.
Pressure Patterns:
Equatorial Trough (low pressure), Subtropical Ridge (high pressure), Polar Highs and Subpolar Lows.
Jet Streams
Fast-flowing air currents at the Tropopause, generally easterly.
Types: Polar Jet (between polar and mid-latitude cells), Subtropical Jet (between mid-latitude and tropical cells).
Turbulence Types
Convective Turbulence: Caused by thermal currents.
Mechanical Turbulence: Due to physical obstructions.
Clear Air Turbulence: Associated with jet streams and high altitudes.
Icing Conditions
Types of Icing:
Rime Ice: Formed by small supercooled droplets freezing on contact.
Clear Ice: Formed by large supercooled droplets spreading upon contact.
Conditions: Icing can occur at varied temperatures and in visible moisture.
Coriolis Force
Caused by Earth's rotation, deflecting moving air: right in the northern hemisphere, left in the southern hemisphere.
Affects wind patterns and creates circular movements in the atmosphere.
Stability and Instability
Stable Air: Cooler than surroundings, tends to sink.
Unstable Air: Warmer than surroundings, tends to rise.
Conditional Instability: Depends on moisture and temperature structure.
Cloud Types and Weather Effects
Cumulonimbus (Cb): Associated with thunderstorms, heavy precipitation, and turbulence.
Stratus/Nimbostratus (Ns): Causes continuous rain, low visibility.
Cumulus (Cu): Generally fair weather, can indicate turbulence.
Precipitation Processes
Forms: Rain, snow, sleet, freezing rain.
Growth Processes: Coalescence and Bergeron processes in warmer and colder clouds, respectively.
Atmospheric Composition
Major Gases: 78% Nitrogen, 21% Oxygen, trace amounts of Argon and greenhouse gases like CO2.
Impacts: Greenhouse gases affect heat retention and climate.
Temperature Measurement and Variation
Instruments: Thermometers (Liquid in glass, thermocouples).
Conversion: Celsius to Fahrenheit and vice versa.
Heat Transfer Mechanisms
Conduction: Transfer through direct contact.
Convection: Movement of air carrying heat energy.
Radiation: Transfer through electromagnetic waves (solar radiation).