Saturation Vapor Pressure of Water and Ice & The Clausius-Clapeyron Equation | FWC CIV.9

We explore how saturation vapor pressure differs over liquid water and ice, and how temperature controls these values through the Clausius–Clapeyron equation. Learn why this relationship is fundamental for understanding phase changes, cloud formation, and precipitation in the atmosphere. This video follows Chapter IV (“Water and Humidity”) of Fundamentals of Weather and Climate and is Lecture 9 in this series. 0:00 Saturation vapor pressure over water 2:05 Clausius–Clapeyron equation 4:38 Undersaturation 5:58 Saturation 6:15 Supersaturation 8:44 Saturation over water and ice 12:05 Why is saturation over ice smaller than over water? 16:17 Why does it matter?\ 17:18 Consider subscribing Join this channel to get access to perks:    / @djordjeromanic   Atmospheric science playlist:    • Atmospheric Science   Wind energy playlist:    • Wind Energy   Wind engineering playlist:    • Wind Engineering   Channel's mission: --------- The dissemination of knowledge and advancement of learning by providing high-quality content in the fields of atmospheric science, wind engineering, and wind energy. --------- Did you like this video? You can help support the channel with a PayPal donation: https://www.paypal.me/DjordjeRomanic Stay in the atmosphere! See you in the next video. Cheers! #AtmosphericScience #WindEngineering #WindEnergy