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). A graphical representation of what we explored in the previous

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). 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 ... Cyclones often form on the east side of the Rocky Mountains. Potential vorticity offers an explanation as to why this occurs. 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 ... A first look at friction and how it affects atmospheric flow. An exercise to check your understanding of the Hypsometric Equation (and a discussion of the results behind this specific ... A first look at the horizontal structure of a typical mid-latitude cyclone. 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 centripetal and centrifugal forces.

A first look at the second apparent force that arises from a rotating (non-inertial) reference frame. Also, here's a nice little animation ... A look at some of the mechanisms that can intensify cyclones, and the introduction of a new concept known as "potential vorticity". A closer look at turbulence, including some of the mathematics behind turbulence. Here we answer the question: "What exactly is flux? And what exactly is mass flux?" Please note: When demonstrating the time ... 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 3 - Segment 2: Physical Interpretation of the Hypsometric Equation
METR2023 - Lecture 2 - Segment 3: Pressure Gradient Force on an Isobaric Surface
METR2023 - Lecture 11 - Segment 3: Illustrating the Solutions of the Gradient Wind Balance
METR2023 - Lecture 17 - Segment 2: Teleconnections and Oscillations
METR2023 - Lecture 15 - Segment 3: Using Potential Vorticity to Explain Lee Cyclogenesis
METR2023 - Lecture 22 - Segment 3: Hodographs
METR2023 - Lecture 23 - Segment 3: Diagnosing Straight-Line Wind Potential
METR2023 - Lecture 6 - Segment 3: Friction in the Atmosphere
METR2023 - Lecture 3 - Segment 3: Hypsometric Equation Exercise
METR2023 - Lecture 18 - Segment 2: Horizontal Structure of a Standard Extratropical Cyclone
METR2023 - Lecture 19 - Segment 2: Cold Fronts
METR2023 - Lecture 4 - Segment 2: Physical Consequences of Centripetal and Centrifugal Force
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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).

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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 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.

Sponsored
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 6 - Segment 3: Friction in the Atmosphere

METR2023 - Lecture 6 - Segment 3: Friction in the Atmosphere

A first look at friction and how it affects atmospheric flow.

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 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 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 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 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 12 - Segment 3: Derivation of Thermal Wind

METR2023 - Lecture 12 - Segment 3: Derivation of Thermal Wind

The math behind thermal wind.

METR2023 - Lecture 5 - Segment 2: Introduction to Coriolis Force

METR2023 - Lecture 5 - Segment 2: Introduction to Coriolis Force

A first look at the second apparent force that arises from a rotating (non-inertial) reference frame. Also, here's a nice little animation ...

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 2: Turbulence

METR2023 - Lecture 24 - Segment 2: Turbulence

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

METR2023 - Lecture 8 - Segment 2: A Closer Look at (Mass) Flux

METR2023 - Lecture 8 - Segment 2: A Closer Look at (Mass) Flux

Here we answer the question: "What exactly is flux? And what exactly is mass flux?" Please note: When demonstrating the time ...

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 ...

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