---
### Atmospheric Moisture & Weather – Core Topics Explained
#### Humidity Concepts
* Relative Humidity (RH): Ratio (%) of the actual water vapor in the air to the maximum amount the air can hold at that temp.
* Specific Humidity (SH): Mass of water vapor per mass of air (g/kg); does not change with temp.
* Temp vs. RH: As air temp rises, RH drops (if SH stays the same). Warm air holds more moisture.
* Dew Point: Temp at which air becomes saturated (RH = 100%). A high dew point means high SH.
#### Daily RH Pattern
* Lowest in mid-afternoon (hottest part of day), highest around dawn (coldest time).
---
### Fog & Cloud Formation
* Types of Fog:
* Radiation Fog: Forms overnight as ground cools.
* Advection Fog: Warm moist air over a cool surface (coastal).
* Upslope Fog: Moist air pushed uphill cools.
* Orographic Lifting:
* Air rises on windward side → cools → RH ↑ → condensation → clouds/precip.
* LCL (Lifted Condensation Level): Height where dew point is reached and clouds form.
* On leeward side: air descends, warms → RH ↓ → dry conditions.
---
### Lifting Mechanisms
1. Orographic: Air lifted over mountains.
2. Convectional: Sun heats surface → warm air rises.
3. Frontal: Warm air forced over cold at fronts.
4. Convergent: Air flows toward low pressure → rises.
---
### Clouds
* Cumulus: Puffy, fair weather.
* Stratus: Layered, overcast skies.
* Nimbostratus: Steady rain.
* Cumulonimbus: Thunderstorms, hail, lightning.
---
### Precipitation Processes
* Collision-Coalescence: Common in warm clouds (tropics).
* Bergeron Process: Common in cold clouds; involves ice crystals growing at the expense of supercooled droplets.
* Hail: Forms in cumulonimbus clouds with strong updrafts cycling ice pellets.
* Lightning/Thunder: Charge separation in clouds → discharge (lightning), rapid heating causes thunder.
---
### Latent Heat
* Released: During condensation, freezing, deposition → fuels storms.
* Absorbed: During evaporation, melting, sublimation → cools environment.
---
### Air Masses & Fronts
* Air Mass Types:
* mT: maritime tropical (warm, humid)
* cT: continental tropical (hot, dry)
* mP: maritime polar (cool, moist)
* cP: continental polar (cold, dry)
* Fronts:
* Cold Front: Fast, steep slope; short, intense rain; temps drop after.
* Warm Front: Slower, gradual slope; long, steady rain; temps rise after.
* Occluded Front: Cold catches warm front; mix of weather.
---
### Mid-Latitude Cyclones
* Structure: Low pressure system with warm and cold fronts.
* Movement: West to east (guided by polar jet stream).
* Rotation: Counterclockwise in Northern Hemisphere.
* Precip & Wind:
* Ahead of warm front: Light/moderate rain.
* At cold front: Thunderstorms possible.
* Behind cold front: Clearer, cooler.
---
### Thunderstorms
* Three Stages:
1. Cumulus: Rising warm air; updrafts dominate.
2. Mature: Up & downdrafts; most intense weather.
3. Dissipating: Downdrafts dominate, storm dies out.
* Cloud: Cumulonimbus.
* Duration: Typically 30 mins to a few hours.
* WA Connection: West side cooler, more stable (less storms); East side warmer, drier (more storms with lifting).
---