Media Summary: A look at some of the physical consequences behind the Hypsometric Equation. A look at the pressure gradient force (PGF) on a surface of constant pressure (otherwise known as an isobaric surface). Cyclones often form on the east side of the Rocky Mountains. Potential vorticity offers an explanation as to why this occurs.

Metr2023 Lecture 3 Segment 2 - Detailed Analysis & Overview

A look at some of the physical consequences behind the Hypsometric Equation. A look at the pressure gradient force (PGF) on a surface of constant pressure (otherwise known as an isobaric surface). Cyclones often form on the east side of the Rocky Mountains. Potential vorticity offers an explanation as to why this occurs. A look at some of the mechanisms that can intensify cyclones, and the introduction of a new concept known as "potential vorticity". What do all the fancy lines and symbols on a hodograph mean? Link to the splitting storm animation: ... An exercise to check your understanding of the Hypsometric Equation (and a discussion of the results behind this specific ...

What is thermal wind and why does it exist? A graphical representation of what we explored in the previous What happens between weather (days) and climate (decades)? That's when oscillations enter the story, which are variations ... A look at some of the physical consequences behind the centripetal and centrifugal forces. An overview of what atmospheric factors favor strong straight-line wind gusts. Please keep in mind that there are multiple different ... A first look at the horizontal structure of a typical mid-latitude cyclone.

Photo Gallery

METR2023 - Lecture 3 - Segment 2: Physical Interpretation of the Hypsometric Equation
METR2023 - Lecture 2 - Segment 3: Pressure Gradient Force on an Isobaric Surface
METR2023 - Lecture 15 - Segment 3: Using Potential Vorticity to Explain Lee Cyclogenesis
METR2023 - Lecture 15 - Segment 2: Rossby Wave Formation and Potential Vorticity
METR2023 - Lecture 22 - Segment 3: Hodographs
METR2023 - Lecture 3 - Segment 3: Hypsometric Equation Exercise
METR2023 - Lecture 12 - Segment 2: Introduction to Thermal Wind
METR2023 - Lecture 11 - Segment 3: Illustrating the Solutions of the Gradient Wind Balance
METR2023 - Lecture 17 - Segment 2: Teleconnections and Oscillations
METR2023 - Lecture 4 - Segment 2: Physical Consequences of Centripetal and Centrifugal Force
METR2023 - Lecture 23 - Segment 3: Diagnosing Straight-Line Wind Potential
METR2023 - Lecture 18 - Segment 2: Horizontal Structure of a Standard Extratropical Cyclone
View Detailed Profile
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 2 - Segment 3: Pressure Gradient Force on an Isobaric Surface

METR2023 - Lecture 2 - Segment 3: Pressure Gradient Force on an Isobaric Surface

A look at the pressure gradient force (PGF) on a surface of constant pressure (otherwise known as an isobaric surface).

METR2023 - Lecture 15 - Segment 3: Using Potential Vorticity to Explain Lee Cyclogenesis

METR2023 - Lecture 15 - Segment 3: Using Potential Vorticity to Explain Lee Cyclogenesis

Cyclones often form on the east side of the Rocky Mountains. Potential vorticity offers an explanation as to why this occurs.

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 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 3 - Segment 3: Hypsometric Equation Exercise

METR2023 - Lecture 3 - Segment 3: Hypsometric Equation Exercise

An exercise to check your understanding of the Hypsometric Equation (and a discussion of the results behind this specific ...

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 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 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 4 - Segment 2: Physical Consequences of Centripetal and Centrifugal Force

METR2023 - Lecture 4 - Segment 2: Physical Consequences of Centripetal and Centrifugal Force

A look at some of the physical consequences behind the centripetal and centrifugal forces.

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 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