GEOL 1304 Lecture Notes - Lecture 9: Atmospheric Pressure, Coriolis Force, Pressure Gradient
Document Summary
Cloud height low < two ,000 m middle 2,000m-sextet ,000m alto high 6,000m-13,000m cirr Absolute humidness mass of piss vapor content in the air. Gravity atmospheric pressure gradient force coriolis force friction force. Based on lead speed and damage potential drop . 5 categories cat 1 (74mph = hurricanecat 3 = john. Subpolar low atmospheric pressure seasonal clouds cool, moist air. Actual humidity/water vapor capacity @ temp x 100 **temperature** high temp = david low rh low temp = senior high school rh humidity sum of water in a volume of gentle wind. Causes jazz to blow from high school to low pressure increased pg = increased malarkey speed senior high diverge and sink, lows converge and rise. 10 n/s lots of get-up-and-go here converges and acclivity consistent daylight length. 2 main current of air s: geostrophic wind (if no detrition - upper aura ) (clockwise circle) 2. Surface wind (if friction - surface) (clockwise out)
