Media Summary: What do all the fancy lines and symbols on a hodograph mean? Link to the splitting storm animation: ... An overview of what atmospheric factors favor strong straight-line wind gusts. Please keep in mind that there are multiple different ... Most hodograph shapes can be broken down into categories, and the ambient wind profile can say a lot about how thunderstorms ...

Metr2023 Lecture 22 Segment 3 - Detailed Analysis & Overview

What do all the fancy lines and symbols on a hodograph mean? Link to the splitting storm animation: ... An overview of what atmospheric factors favor strong straight-line wind gusts. Please keep in mind that there are multiple different ... Most hodograph shapes can be broken down into categories, and the ambient wind profile can say a lot about how thunderstorms ... An overview of what atmospheric factors favor tornadoes. Single cells, multi-cells, and supercells carry their own unique threats and have their own preferred environments. Here, we fill in ... If you know what you're looking for, you can determine the depth of the boundary layer using a sounding.

A look at some past severe weather events that showed high significant tornado index values, but had seemingly underwhelming ... See online syllabus at www.freepilotgroundschool.ca. Dynamic and thermodynamic parameters can be combined to assess certain severe weather threats, which can provide some ... Now that we have this fancy equation, what the heck does it mean for the atmosphere? The answer is in this video... The Arctic Oscillation (AO), North Atlantic Oscillation (NAO), and the Madden Julian Oscillation (MJO) can also significantly impact ... In the United States, a "severe thunderstorm" is a thunderstorm that produces at least one of the following: tornado, 50+ knot (58+ ...

A look at surface warm fronts. Though slow-moving, warm fronts play an important role in destabilizing the atmosphere.

Photo Gallery

METR2023 - Lecture 22 - Segment 3: Hodographs
METR2023 - Lecture 23 - Segment 3: Diagnosing Straight-Line Wind Potential
METR2023 - Lecture 22 - Segment 4: Typical Hodograph Classifications
METR2023 - Lecture 23 - Segment 2: Diagnosing Tornado Potential
METR2023 - Lecture 22 - Segment 1 (p2 / 2): Threats and Characteristics of Each Convection Type
METR2023 - Lecture 24 - Segment 3: Identifying the Atmospheric Boundary Layer on a Sounding
METR2023 - Lecture 22 - Segment 7: Case Study of High Parameter Values with Low Performance
Meteorology 22 - Weather Interpretation 3
METR2023 - Lecture 22 - Segment 6: Severe Weather Composite Parameters
METR2023 - Lecture 8 - Segment 3: Physical Interpretation of the Mass Continuity Equation
METR2023 - Lecture 17 - Segment 4: The Arctic, North Atlantic, and Madden Julian Oscillations
METR2023 - Lecture 23 - Segment 1: Definition of Severe Weather
View Detailed Profile
METR2023 - Lecture 22 - Segment 3: Hodographs

METR2023 - Lecture 22 - Segment 3: Hodographs

What do all the fancy lines and symbols on a hodograph mean? Link to the splitting storm animation: ...

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 22 - Segment 4: Typical Hodograph Classifications

METR2023 - Lecture 22 - Segment 4: Typical Hodograph Classifications

Most hodograph shapes can be broken down into categories, and the ambient wind profile can say a lot about how thunderstorms ...

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 22 - Segment 1 (p2 / 2): Threats and Characteristics of Each Convection Type

METR2023 - Lecture 22 - Segment 1 (p2 / 2): Threats and Characteristics of Each Convection Type

Single cells, multi-cells, and supercells carry their own unique threats and have their own preferred environments. Here, we fill in ...

METR2023 - Lecture 24 - Segment 3: Identifying the Atmospheric Boundary Layer on a Sounding

METR2023 - Lecture 24 - Segment 3: Identifying the Atmospheric Boundary Layer on a Sounding

If you know what you're looking for, you can determine the depth of the boundary layer using a sounding.

METR2023 - Lecture 22 - Segment 7: Case Study of High Parameter Values with Low Performance

METR2023 - Lecture 22 - Segment 7: Case Study of High Parameter Values with Low Performance

A look at some past severe weather events that showed high significant tornado index values, but had seemingly underwhelming ...

Meteorology 22 - Weather Interpretation 3

Meteorology 22 - Weather Interpretation 3

See online syllabus at www.freepilotgroundschool.ca.

METR2023 - Lecture 22 - Segment 6: Severe Weather Composite Parameters

METR2023 - Lecture 22 - Segment 6: Severe Weather Composite Parameters

Dynamic and thermodynamic parameters can be combined to assess certain severe weather threats, which can provide some ...

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 17 - Segment 4: The Arctic, North Atlantic, and Madden Julian Oscillations

METR2023 - Lecture 17 - Segment 4: The Arctic, North Atlantic, and Madden Julian Oscillations

The Arctic Oscillation (AO), North Atlantic Oscillation (NAO), and the Madden Julian Oscillation (MJO) can also significantly impact ...

METR2023 - Lecture 23 - Segment 1: Definition of Severe Weather

METR2023 - Lecture 23 - Segment 1: Definition of Severe Weather

In the United States, a "severe thunderstorm" is a thunderstorm that produces at least one of the following: tornado, 50+ knot (58+ ...

METR2023 - Lecture 19 - Segment 3: Warm Fronts

METR2023 - Lecture 19 - Segment 3: Warm Fronts

A look at surface warm fronts. Though slow-moving, warm fronts play an important role in destabilizing the atmosphere.