Media Summary: A closer look at turbulence, including some of the mathematics behind turbulence. If you know what you're looking for, you can determine the depth of the boundary layer using a sounding. A look at some of the mechanisms that can intensify cyclones, and the introduction of a new concept known as "potential vorticity".

Metr2023 Lecture 24 Segment 2 - Detailed Analysis & Overview

A closer look at turbulence, including some of the mathematics behind turbulence. If you know what you're looking for, you can determine the depth of the boundary layer using a sounding. A look at some of the mechanisms that can intensify cyclones, and the introduction of a new concept known as "potential vorticity". Many meteorologists prefer to represent state variables in the atmosphere as the sum of a background (mean) state and a ... A look at some of the physical consequences behind the Hypsometric Equation. Will the wind flow over the obstacle or around it? The Froude Number can help us answer this question. Also, we look at some ...

An overview of what atmospheric factors favor tornadoes. Outflow boundaries are mesoscale currents of cold moist air produced by thunderstorms. These can have a profound influence on ... Single cells, multi-cells, and supercells carry their own unique threats and have their own preferred environments. Here, we fill in ... CORRECTION: It is asserted in this video that evapotranspiration increases buoyancy. This is not entirely accurate, because this ... What is the Polar Cell and why does it exist? What is thermal wind and why does it exist?

Photo Gallery

METR2023 - Lecture 24 - Segment 2: Turbulence
METR2023 - Lecture 24 - Segment 3: Identifying the Atmospheric Boundary Layer on a Sounding
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 24 - Segment 4: A Widely Used Method of Representing Atmospheric Variables
METR2023 - Lecture 3 - Segment 2: Physical Interpretation of the Hypsometric Equation
METR2023 - Lecture 24 - Segment 6: Froude Number and Urban Flow Patterns
METR2023 - Lecture 23 - Segment 2: Diagnosing Tornado Potential
METR2023 - Lecture 20 - Segment 2: Outflow Boundaries
METR2023 - Lecture 22 - Segment 1 (p2 / 2): Threats and Characteristics of Each Convection Type
METR2023 - Lecture 24 - Segment 1: Atmospheric Boundary Layer (ABL) Introduction
METR2023 - Lecture 14 - Segment 3: The Polar Cell
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METR2023 - Lecture 24 - Segment 2: Turbulence

METR2023 - Lecture 24 - Segment 2: Turbulence

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

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 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 24 - Segment 4: A Widely Used Method of Representing Atmospheric Variables

METR2023 - Lecture 24 - Segment 4: A Widely Used Method of Representing Atmospheric Variables

Many meteorologists prefer to represent state variables in the atmosphere as the sum of a background (mean) state and a ...

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 24 - Segment 6: Froude Number and Urban Flow Patterns

METR2023 - Lecture 24 - Segment 6: Froude Number and Urban Flow Patterns

Will the wind flow over the obstacle or around it? The Froude Number can help us answer this question. Also, we look at some ...

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 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 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 1: Atmospheric Boundary Layer (ABL) Introduction

METR2023 - Lecture 24 - Segment 1: Atmospheric Boundary Layer (ABL) Introduction

CORRECTION: It is asserted in this video that evapotranspiration increases buoyancy. This is not entirely accurate, because this ...

METR2023 - Lecture 14 - Segment 3: The Polar Cell

METR2023 - Lecture 14 - Segment 3: The Polar Cell

What is the Polar Cell and why does it exist?

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?