![Lecture 2: Energy in the Atmosphere Vertical structure of the static atmosphere Basics from physics: force, work, heat Transferring energy in the atmosphere. - ppt download Lecture 2: Energy in the Atmosphere Vertical structure of the static atmosphere Basics from physics: force, work, heat Transferring energy in the atmosphere. - ppt download](https://images.slideplayer.com/26/8505486/slides/slide_3.jpg)
Lecture 2: Energy in the Atmosphere Vertical structure of the static atmosphere Basics from physics: force, work, heat Transferring energy in the atmosphere. - ppt download
![Use the formula v = √(gammaP/ρ) to explain why the speed of sound in air(a) is independent of pressure,(b) increases with temperature, (c) Increases with humidity . Use the formula v = √(gammaP/ρ) to explain why the speed of sound in air(a) is independent of pressure,(b) increases with temperature, (c) Increases with humidity .](https://i.ytimg.com/vi/8lDB5lru_qQ/maxresdefault.jpg)
Use the formula v = √(gammaP/ρ) to explain why the speed of sound in air(a) is independent of pressure,(b) increases with temperature, (c) Increases with humidity .
![SOLVED: Develop the time averaged form of the equation of state for a perfect gas, P=(rho)RT, accounting for turbulent fluctuations in the instantaneous pressure, p, density, (rho) and temperature, T. SOLVED: Develop the time averaged form of the equation of state for a perfect gas, P=(rho)RT, accounting for turbulent fluctuations in the instantaneous pressure, p, density, (rho) and temperature, T.](https://cdn.numerade.com/previews/1148f843-0210-4cd9-9723-32a3a5315ea1_large.jpg)
SOLVED: Develop the time averaged form of the equation of state for a perfect gas, P=(rho)RT, accounting for turbulent fluctuations in the instantaneous pressure, p, density, (rho) and temperature, T.
![SOLVED: Assuming an isothermal ideal gas atmosphere, evaluate the pressure and density variation with height P(r) and rho (r). Plot your equation for P(r) from 0 < r < 100km, assuming a SOLVED: Assuming an isothermal ideal gas atmosphere, evaluate the pressure and density variation with height P(r) and rho (r). Plot your equation for P(r) from 0 < r < 100km, assuming a](https://cdn.numerade.com/ask_previews/96d0c055-8eae-4fbf-9266-30e68eafca01_large.jpg)