Media Summary: PRESENTER: Let's see how to find the equivalent potential temperature, called theta-e, on this Skew-T. The equivalent potential ... PRESENTER: Let's see how to find the wet-bulb potential temperature on the Skew-T. The first step is to find the LCL. Once we ... ... smaller than the distance between the 1008 millibar and the 1016 millibar isobars, which is about

Meteo 300 Supersaturation Processes - Detailed Analysis & Overview

PRESENTER: Let's see how to find the equivalent potential temperature, called theta-e, on this Skew-T. The equivalent potential ... PRESENTER: Let's see how to find the wet-bulb potential temperature on the Skew-T. The first step is to find the LCL. Once we ... ... smaller than the distance between the 1008 millibar and the 1016 millibar isobars, which is about And so we can estimate, since this is x direction, and since this is north, we can estimate that this is about And since the lower layer also has a uniform temperature, it must also be emitting two arrows down to Earth's surface. With one ... The temperature lines are tilted 45 degrees to the right and are in degrees C. Dry adiabats, which indicate constant potential ...

We can imagine what temperature and dew point are radius on record if you were to launch one from below the cloud. Initially we ...

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METEO 300: Supersaturation Processes
METEO 300: Supersaturation Processes 2
METEO 300: SkewT_FindingTheta_e
METEO 300: SkewT_Finding_Wetbulb_Theta
METEO 300: PGF Example
METEO 300: Finding Advection
METEO 300: Pressure Surfaces
METEO 300: Divergence Area
METEO 300: Climate Model
METEO 300: Four Force Balances
METEO 300: Coriolis Explanation
METEO 300: Skew-T Basics
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