'Which temperature changes' presentation slideshows

Atmospheric Stability

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Cloud Formation

Cloud Formation. Formation of clouds requires a mechanism that results in the uplift of air. First, recall. Adiabatic process - process in which temperature changes but heat energy is not added or removed. p . ?V = - Cv . ?T. ? H - Change in heat p - pressure ?V - Volume Change

832 views • 58 slides

Chapter 7

Chapter 7. Bits of Vector Calculus. (1) Vector Magnitude and Direction. Consider the vector to the right. We could determine the magnitude by determining the x-component and the y-component. Then use the equation:.

460 views • 33 slides

Chapter 5 Atmospheric Moisture

Chapter 5 Atmospheric Moisture. The process whereby molecules break free of liquid water is known as evaporation . The opposite process is condensation , wherein water vapor molecules become a liquid. The change of phase directly from ice to water vapor,

455 views • 25 slides

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Rates of Heat Transfer

Rates of Heat Transfer. January 17, 2013 Coach Stephens. Rate of Heat Transfer. This topic is of great importance because of the frequent need to either increase or decrease the rate at which heat flows between two locations. . Rates of Heat Transfer.

338 views • 18 slides

Lecture 6

Lecture 6. The radiation field and opacity. Review. The main sequence is a mass sequence More massive stars are closer to the top-left (hot and bright). M=30M Sun. M=M Sun. M=0.2M Sun. Radiation intensity.

432 views • 14 slides

The Deep Blue Sea

By Jessica Tancordo. The Deep Blue Sea. Geography. covers 360 million km 2 3 major ocean basins Pacific-180 million km 2 Atlantic-106 million km 2 Indian-75 million km 2. Structure . Temperature. Sunlight absorbed Kinetic state Temperature

269 views • 11 slides