Media Summary: Outflow boundaries are mesoscale currents of cold moist air produced by thunderstorms. These can have a profound influence on ... A first look at the horizontal structure of a typical mid-latitude cyclone. A look at some of the mechanisms that can intensify cyclones, and the introduction of a new concept known as "potential vorticity".

Metr2023 Lecture 20 Segment 2 - Detailed Analysis & Overview

Outflow boundaries are mesoscale currents of cold moist air produced by thunderstorms. These can have a profound influence on ... A first look at the horizontal structure of a typical mid-latitude cyclone. A look at some of the mechanisms that can intensify cyclones, and the introduction of a new concept known as "potential vorticity". A look at what our Cartesian wind vector (in terms of u, v, and w) looks like in natural coordinates. CORRECTION: At some point in the video, I mention that the Himalayas create a form of dry line in India. This is an inaccuracy. What happens between weather (days) and climate (decades)? That's when oscillations enter the story, which are variations ...

A look at surface cold fronts. Cold fronts that occur above ground level (often referred to as a Cold Front Aloft or CFA) can rapidly ... A look at some of the physical consequences behind the Hypsometric Equation. One might call this a backwards way of thinking, but if we're going to use pressure coordinates, we have to look at how some of ... What is thermal wind and why does it exist? An overview of what atmospheric factors favor tornadoes. A closer look at turbulence, including some of the mathematics behind turbulence.

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METR2023 - Lecture 20 - Segment 2: Outflow Boundaries
METR2023 - Lecture 18 - Segment 2: Horizontal Structure of a Standard Extratropical Cyclone
METR2023 - Lecture 21 - Segment 2: Processes Neglected in the Atmospheric Buoyancy Equation
METR2023 - Lecture 15 - Segment 2: Rossby Wave Formation and Potential Vorticity
METR2023 - Lecture 10 - Segment 2: Wind Vector in Natural Coordinates
METR2023 - Lecture 20 - Segment 1: The Dry Line
METR2023 - Lecture 17 - Segment 2: Teleconnections and Oscillations
METR2023 - Lecture 19 - Segment 2: Cold Fronts
METR2023 - Lecture 3 - Segment 2: Physical Interpretation of the Hypsometric Equation
METR2023 - Lecture 27 - Segment 2: Vertical Wind in Pressure Coordinates
METR2023 - Lecture 12 - Segment 2: Introduction to Thermal Wind
METR2023 - Lecture 23 - Segment 2: Diagnosing Tornado Potential
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METR2023 - Lecture 20 - Segment 2: Outflow Boundaries

METR2023 - Lecture 20 - Segment 2: Outflow Boundaries

Outflow boundaries are mesoscale currents of cold moist air produced by thunderstorms. These can have a profound influence on ...

METR2023 - Lecture 18 - Segment 2: Horizontal Structure of a Standard Extratropical Cyclone

METR2023 - Lecture 18 - Segment 2: Horizontal Structure of a Standard Extratropical Cyclone

A first look at the horizontal structure of a typical mid-latitude cyclone.

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 15 - Segment 2: Rossby Wave Formation and Potential Vorticity

METR2023 - Lecture 15 - Segment 2: Rossby Wave Formation and Potential Vorticity

A look at some of the mechanisms that can intensify cyclones, and the introduction of a new concept known as "potential vorticity".

METR2023 - Lecture 10 - Segment 2: Wind Vector in Natural Coordinates

METR2023 - Lecture 10 - Segment 2: Wind Vector in Natural Coordinates

A look at what our Cartesian wind vector (in terms of u, v, and w) looks like in natural coordinates.

METR2023 - Lecture 20 - Segment 1: The Dry Line

METR2023 - Lecture 20 - Segment 1: The Dry Line

CORRECTION: At some point in the video, I mention that the Himalayas create a form of dry line in India. This is an inaccuracy.

METR2023 - Lecture 17 - Segment 2: Teleconnections and Oscillations

METR2023 - Lecture 17 - Segment 2: Teleconnections and Oscillations

What happens between weather (days) and climate (decades)? That's when oscillations enter the story, which are variations ...

METR2023 - Lecture 19 - Segment 2: Cold Fronts

METR2023 - Lecture 19 - Segment 2: Cold Fronts

A look at surface cold fronts. Cold fronts that occur above ground level (often referred to as a Cold Front Aloft or CFA) can rapidly ...

METR2023 - Lecture 3 - Segment 2: Physical Interpretation of the Hypsometric Equation

METR2023 - Lecture 3 - Segment 2: Physical Interpretation of the Hypsometric Equation

A look at some of the physical consequences behind the Hypsometric Equation.

METR2023 - Lecture 27 - Segment 2: Vertical Wind in Pressure Coordinates

METR2023 - Lecture 27 - Segment 2: Vertical Wind in Pressure Coordinates

One might call this a backwards way of thinking, but if we're going to use pressure coordinates, we have to look at how some of ...

METR2023 - Lecture 12 - Segment 2: Introduction to Thermal Wind

METR2023 - Lecture 12 - Segment 2: Introduction to Thermal Wind

What is thermal wind and why does it exist?

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 24 - Segment 2: Turbulence

METR2023 - Lecture 24 - Segment 2: Turbulence

A closer look at turbulence, including some of the mathematics behind turbulence.