Media Summary: A commonly used parameter in forecasting thunderstorms and severe weather is Convective Available Potential Energy (CAPE). A graphical representation of what we explored in the previous Another parameter used for forecasting thunderstorms and severe weather is the environmental lapse rate. Here, we'll take a look ...

Metr2023 Lecture 21 Segment 3 - Detailed Analysis & Overview

A commonly used parameter in forecasting thunderstorms and severe weather is Convective Available Potential Energy (CAPE). A graphical representation of what we explored in the previous Another parameter used for forecasting thunderstorms and severe weather is the environmental lapse rate. Here, we'll take a look ... An overview of what atmospheric factors favor strong straight-line wind gusts. Please keep in mind that there are multiple different ... What the acceleration vector looks like in natural coordinates. A review of the buoyant force and a look at how it applies itself to the atmosphere.

Not all values of V are solutions to the gradient wind balance. Here, we list out what situations are theoretical possible. Remember the good ol' quadratic equation? An overview of what atmospheric factors favor tornadoes. Now that we have this fancy equation, what the heck does it mean for the atmosphere? The answer is in this video... An overview of what atmospheric factors can favor excessive rainfall and flash flooding. Flooding can be caused slow-moving ... As important as fronts are in the atmosphere, there is no universally agreed upon definition of a front. Though, most people ...

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METR2023 - Lecture 21 - Segment 3: Convective Available Potential Energy
METR2023 - Lecture 21 - Segment 2: Processes Neglected in the Atmospheric Buoyancy Equation
METR2023 - Lecture 11 - Segment 3: Illustrating the Solutions of the Gradient Wind Balance
METR2023 - Lecture 21 - Segment 4: Lapse Rates
METR2023 - Lecture 23 - Segment 3: Diagnosing Straight-Line Wind Potential
METR2023 - Lecture 10 - Segment 3: Horizontal Acceleration Vector in Natural Coordinates
METR2023 - Lecture 21 - Segment 1: Atmospheric Buoyancy
METR2023 - Lecture 11 - Segment 2: Mathematical Solutions of the Gradient Wind Balance
METR2023 - Lecture 11 - Segment 1: Solving for V in the Gradient Wind Balance
METR2023 - Lecture 23 - Segment 2: Diagnosing Tornado Potential
METR2023 - Lecture 8 - Segment 3: Physical Interpretation of the Mass Continuity Equation
METR2023 - Lecture 23 - Segment 6: Diagnosing Flooding Potential
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METR2023 - Lecture 21 - Segment 3: Convective Available Potential Energy

METR2023 - Lecture 21 - Segment 3: Convective Available Potential Energy

A commonly used parameter in forecasting thunderstorms and severe weather is Convective Available Potential Energy (CAPE).

METR2023 - Lecture 21 - Segment 2: Processes Neglected in the Atmospheric Buoyancy Equation

METR2023 - Lecture 21 - Segment 2: Processes Neglected in the Atmospheric Buoyancy Equation

The buoyancy equation from

METR2023 - Lecture 11 - Segment 3: Illustrating the Solutions of the Gradient Wind Balance

METR2023 - Lecture 11 - Segment 3: Illustrating the Solutions of the Gradient Wind Balance

A graphical representation of what we explored in the previous

METR2023 - Lecture 21 - Segment 4: Lapse Rates

METR2023 - Lecture 21 - Segment 4: Lapse Rates

Another parameter used for forecasting thunderstorms and severe weather is the environmental lapse rate. Here, we'll take a look ...

METR2023 - Lecture 23 - Segment 3: Diagnosing Straight-Line Wind Potential

METR2023 - Lecture 23 - Segment 3: Diagnosing Straight-Line Wind Potential

An overview of what atmospheric factors favor strong straight-line wind gusts. Please keep in mind that there are multiple different ...

METR2023 - Lecture 10 - Segment 3: Horizontal Acceleration Vector in Natural Coordinates

METR2023 - Lecture 10 - Segment 3: Horizontal Acceleration Vector in Natural Coordinates

What the acceleration vector looks like in natural coordinates.

METR2023 - Lecture 21 - Segment 1: Atmospheric Buoyancy

METR2023 - Lecture 21 - Segment 1: Atmospheric Buoyancy

A review of the buoyant force and a look at how it applies itself to the atmosphere.

METR2023 - Lecture 11 - Segment 2: Mathematical Solutions of the Gradient Wind Balance

METR2023 - Lecture 11 - Segment 2: Mathematical Solutions of the Gradient Wind Balance

Not all values of V are solutions to the gradient wind balance. Here, we list out what situations are theoretical possible.

METR2023 - Lecture 11 - Segment 1: Solving for V in the Gradient Wind Balance

METR2023 - Lecture 11 - Segment 1: Solving for V in the Gradient Wind Balance

Remember the good ol' quadratic equation?

METR2023 - Lecture 23 - Segment 2: Diagnosing Tornado Potential

METR2023 - Lecture 23 - Segment 2: Diagnosing Tornado Potential

An overview of what atmospheric factors favor tornadoes.

METR2023 - Lecture 8 - Segment 3: Physical Interpretation of the Mass Continuity Equation

METR2023 - Lecture 8 - Segment 3: Physical Interpretation of the Mass Continuity Equation

Now that we have this fancy equation, what the heck does it mean for the atmosphere? The answer is in this video...

METR2023 - Lecture 23 - Segment 6: Diagnosing Flooding Potential

METR2023 - Lecture 23 - Segment 6: Diagnosing Flooding Potential

An overview of what atmospheric factors can favor excessive rainfall and flash flooding. Flooding can be caused slow-moving ...

METR2023 - Lecture 19 - Segment 1: Introduction to Fronts

METR2023 - Lecture 19 - Segment 1: Introduction to Fronts

As important as fronts are in the atmosphere, there is no universally agreed upon definition of a front. Though, most people ...