'Vertical pressure gradient force' presentation slideshows

Basic dynamics ?The equations of motion and continuity scaling Hydrostatic relation

771 views • 74 slides

773 views • 62 slides

Chapter 5

Chapter 5. Soundings. There are four basic types of sounding observations. (1) Radiosondes An instrument package lifted by a balloon with sensors for pressure, temperature, humidity. (2) Pibals (Pilot balloons)

662 views • 44 slides

General Circulation of the Atmosphere

General Circulation of the Atmosphere. Lisa Goddard. 19 September 2006. Main Points. * Atmosphere wants to attain balance - Circulation results from the atmosphere adjusting to remove imposed imbalances

762 views • 39 slides

General Circulation of the Atmosphere

General Circulation of the Atmosphere. Lisa Goddard. 19 September 2006. Main Points. * Atmosphere wants to attain balance - Circulation results from the atmosphere adjusting to remove imposed imbalances

410 views • 39 slides

Chapter 4 Atmospheric Pressure and Wind

Chapter 4 Atmospheric Pressure and Wind. The atmosphere contains a tremendous number of gas molecules being pulled toward Earth by the force of gravity. These molecules exert a force on all surfaces with which they are in contact, and the amount of that force exerted

527 views • 28 slides

Basic dynamics ? The equations of motion and continuity Scaling Hydrostatic relation

296 views • 27 slides

Things to look for on the weather maps

Things to look for on the weather maps.

267 views • 26 slides

Typhoon Dynamics

Typhoon Dynamics. Roger K. Smith University of Munich. Aim To review some of the fundamental processes involved in the dynamics and thermodynamics of typhoon structure and evolution. Outline of talk. Structure of a mature hurricane Basic dynamics Primary circulation The eye

270 views • 26 slides

Class #12: Friday, September 25

332 views • 21 slides

ATMOSPHERIC PROCESSES--PSEUDOADIABATIC Adiabatic wet-bulb temperature Adiabatic equivalent temperature Conservative p

ATMOSPHERIC PROCESSES--PSEUDOADIABATIC Adiabatic wet-bulb temperature Adiabatic equivalent temperature Conservative properties. Reversible Saturated Adiabatic Processes If we consider a closed parcel of rising, cloudy air, the process is reversible since all the

624 views • 17 slides

Lecture 4: The Fundamental Conservation Laws

Lecture 4: The Fundamental Conservation Laws. Weather Analysis Forecasting Ch. 4. Outline. The Hydrostatic Equation The Thickness Equation Conservation of Mass Conservation of Momentum Conservation of Energy. Introduction.

168 views • 0 slides