Documents CHAPTER 4: ATMOSPHERIC TRANSPORT Forces in the atmosphere: Gravity g Pressure-gradient Coriolis...

Slide 1 CHAPTER 4: ATMOSPHERIC TRANSPORT Forces in the atmosphere: Gravity g Pressure-gradient Coriolis Friction to R of direction of motion (NH) or L (SH) Equilibrium of…

Documents THE HADLEY CIRCULATION (1735): global sea breeze HOT COLD Explains: Intertropical Convergence Zone.....

Slide 1 THE HADLEY CIRCULATION (1735): global sea breeze HOT COLD Explains: Intertropical Convergence Zone (ITCZ) Wet tropics, dry poles Problem: does not account for Coriolis…