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Sundog publishing - PowerPoint PPT Presentation

We need to understand the environment around a moist air parcel in order to determine whether it will rise or sink throu

Hydrostatics. We need to understand the environment around a moist air parcel in order to determine whether it will rise or sink through the atmosphere Here we investigate parameters that describe the large-scale environment. Hydrostatics. Outline:

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354 views • 23 slides

Skew T Log P Diagram

Skew T Log P Diagram. AOS 330 LAB 7. Review. Difference between ( or dx), and Hypsometric Equation Equal Area Transformation. 3 Desirable Characteristics of a thermodynamic diagram. They are designed so that area on the diagrams is proportional to energy.

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1.3k views • 21 slides

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Sundog publishing - PowerPoint PPT Presentation

We need to understand the environment around a moist air parcel in order to determine whether it will rise or sink throu

Skew T Log P Diagram