Meteorology:
Meteorology Unit 8 Study Guide
☀ S6E4.b – Energy from the Sun & Heat Transfer
The sun heats land, water, and air at different rates
This uneven heating causes temperature differences, which drive weather patterns

Troposphere – Lowest layer; where weather happens and where we live (up to ~8–15 km).
Stratosphere – Contains the ozone layer; temperature increases with height (~15–50 km).
Mesosphere – Coldest layer; meteors burn up here (~50–85 km).
Thermosphere – Very thin air; auroras occur here (~85–600 km).
Exosphere – Outermost layer; gradually fades into space (above ~600 km).
🌍 Climate vs. Weather
Climate
Long-term average weather (30+ years)
Helps predict what to expect
Factors that affect climate:
Latitude – closer to equator = warmer
Air Masses – carry temperature & moisture
Elevation – higher = colder
Proximity to Water – moderates temperature
Landforms – affect precipitation (rain shadows)
Weather
Short-term atmospheric conditions
Includes:
Temperature
Precipitation
Air pressure
Cloud cover
🌡 Temperature Differences & Air Movement
Warm air = less dense → rises
Cool air = more dense → sinks
This movement creates wind and weather patterns
📝 Climate vs Weather Examples
What you expect → Climate
What you get → Weather
What you see outside → Weather
Planning clothes for a trip → Climate
Bringing umbrella today → Weather
🌬 S6E4.d – Air Masses & Fronts (Quiz 2)
Air Mass
Large body of air with same:
Temperature
Humidity
Pressure
Types of Air Masses
Maritime → over water → humid
Continental → over land → dry
Tropical → warm
Polar/Arctic → cold
Air Front
Boundary where two air masses meet and don’t mix
Types of Fronts
Cold Front
Cold air pushes under warm air
🌩 Thunderstorms, heavy rain
Warm Front
Warm air rises over cold air
🌧 Light rain, cloudy
Stationary Front
Neither air mass moves
🌫 Days of clouds & rain
Occluded Front
Cold air traps warm air between two cool masses
🌨 Cloudy, rainy, or snowy
⛈ S6E4.d & e – Severe Weather
Storm
Violent disturbance caused by pressure changes
🌩 Thunderstorms
Requirements:
Moisture
Unstable air
Lift
Key Facts:
Occur mostly in spring & summer
Form tall clouds called thunderheads
Lightning
Caused by buildup of electrical charges
Thunder
Caused by rapid expansion of heated air
🌪 Tornadoes
Funnel-shaped, rotating column of air
Forms from thunderstorms
Formation:
Warm air rises, cool air sinks → creates rotation
When:
Spring & early summer
Scale:
Enhanced Fujita Scale (EF0–EF5)
🌀 Hurricanes
Large tropical storms with winds ≥119 km/h (74 mph)
Formation:
Warm ocean water fuels storm
Air rises → low pressure → winds spiral inward
Season:
Late summer → early fall
Eye of the Storm:
Calm center surrounded by intense winds
Over Land:
Weakens (loses energy source)
Storm Surge:
Ocean water rises up to 6 meters
Scale:
Saffir-Simpson Scale (Category 1–5)
🌪🌩🌀 Storm Comparison
Feature | Thunderstorm | Tornado | Hurricane |
|---|---|---|---|
Size | Small | Very small | Very large |
Duration | ~30 min | ~10 min | Days–weeks |
Location | Worldwide | Worldwide | Oceans |
Season | Spring/Summer | Spring/Fall | June–Nov |
Hazards | Lightning, hail | Flying debris | Flooding, surge |
Scale | None | EF Scale | Saffir-Simpson |
⚡ Key Things to Remember
Uneven heating → drives weather
Warm air rises, cool air sinks
Air masses determine weather conditions
Fronts = where weather changes happen
Most severe weather starts with thunderstorms
(Quiz 1)
What Are Greenhouse Gases?
Greenhouse gases (GHGs) are gases in Earth’s atmosphere that trap heat. They let sunlight in, but absorb and re-radiate heat, warming the planet. This process is called the Greenhouse Effect.
Main Greenhouse Gases
Know these core ones:
Carbon Dioxide (CO₂)
Comes from burning fossil fuels, deforestation
Biggest contributor to human-caused warming
Methane (CH₄)
Released from livestock, landfills, natural gas leaks
Much stronger than CO₂ in the short term
Nitrous Oxide (N₂O)
From fertilizers, agriculture, combustion
Long-lasting and powerful
Water Vapor (H₂O)
Most abundant greenhouse gas
Amplifies warming but not directly controlled by humans
Fluorinated gases (F-gases)
Man-made (refrigerants, industrial processes)
Extremely potent but less common
How the Greenhouse Effect Works
Sunlight enters Earth’s atmosphere
Earth absorbs energy and warms up
Earth releases heat (infrared radiation)
Greenhouse gases trap some of this heat
Planet stays warm enough to support life
Without this effect, Earth would be too cold to live on.
Natural vs Human Causes
Natural sources: volcanoes, respiration, decomposition
Human sources: burning fossil fuels, farming, deforestation, industry
Human activity has intensified the greenhouse effect, leading to Global Warming.
Why It Matters
Increased greenhouse gases lead to:
Rising global temperatures
Melting ice caps and glaciers
Sea level rise
More extreme weather
This broader impact is called Climate Change.
Key Terms to Remember
Carbon footprint: total emissions caused by a person/activity
Fossil fuels: coal, oil, natural gas
Renewable energy: solar, wind, hydro
Carbon cycle: movement of carbon through Earth systems
Quick Memory Tricks
CO₂ = biggest volume
CH₄ = strongest short-term
Humans = main cause of increase