Media Summary: A first look at a special type of extratropical (mid-latitude) cyclone, which can be a particularly destructive one. How does the atmosphere attempt to resolve radiative balances? One key mechanism is to create cyclones. Using the concepts discussed to explain the existence and behavior of the subtropical jet and the polar jet.

Metr2023 Lecture 18 Segment 4 - Detailed Analysis & Overview

A first look at a special type of extratropical (mid-latitude) cyclone, which can be a particularly destructive one. How does the atmosphere attempt to resolve radiative balances? One key mechanism is to create cyclones. Using the concepts discussed to explain the existence and behavior of the subtropical jet and the polar jet. A first look at the vertical structure of a typical mid-latitude cyclone. Meteorology and urban development go hand-in-hand in a lot of respects. Stationary fronts are never perfectly stationary, but are sluggish enough to be called stationary. Occluded fronts can produce very ...

The Arctic Oscillation (AO), North Atlantic Oscillation (NAO), and the Madden Julian Oscillation (MJO) can also significantly impact ... Not something you'll encounter a lot in the future, but if you're working in pressure coordinates, it might be useful to know. As important as fronts are in the atmosphere, there is no universally agreed upon definition of a front. Though, most people ... Why do we care about these pollutants so much? Here, we answer that question by looking at some of the potential impacts to ... Many meteorologists prefer to represent state variables in the atmosphere as the sum of a background (mean) state and a ... Jet streaks are narrow corridors of stronger flow in the jet-stream. Jet streaks can play a very important role in the atmosphere.

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

Photo Gallery

METR2023 - Lecture 18 - Segment 4: Shapiro-Keyser Cyclone
METR2023 - Lecture 18 - Segment 1: Cyclone Types and the Norwegian Cyclone Model
METR2023 - Lecture 14 - Segment 4: Upper Atmospheric Jets
METR2023 - Lecture 18 - Segment 3: Vertical Structure of a Standard Extratropical Cyclone
METR2023 - Lecture 26 - Segment 4: Meteorology and Urban Development
METR2023 - Lecture 19 - Segment 4: Stationary and Occluded Fronts
METR2023 - Lecture 17 - Segment 4: The Arctic, North Atlantic, and Madden Julian Oscillations
METR2023 - Lecture 27 - Segment 4: Lapse Rate in Pressure Coordinates
METR2023 - Lecture 19 - Segment 1: Introduction to Fronts
METR2023 - Lecture 25 - Segment 4: Atmospheric Pollutant Information
METR2023 - Lecture 24 - Segment 4: A Widely Used Method of Representing Atmospheric Variables
METR2023 - Lecture 16 - Segment 4: Jet Streaks
View Detailed Profile
METR2023 - Lecture 18 - Segment 4: Shapiro-Keyser Cyclone

METR2023 - Lecture 18 - Segment 4: Shapiro-Keyser Cyclone

A first look at a special type of extratropical (mid-latitude) cyclone, which can be a particularly destructive one.

METR2023 - Lecture 18 - Segment 1: Cyclone Types and the Norwegian Cyclone Model

METR2023 - Lecture 18 - Segment 1: Cyclone Types and the Norwegian Cyclone Model

How does the atmosphere attempt to resolve radiative balances? One key mechanism is to create cyclones.

METR2023 - Lecture 14 - Segment 4: Upper Atmospheric Jets

METR2023 - Lecture 14 - Segment 4: Upper Atmospheric Jets

Using the concepts discussed to explain the existence and behavior of the subtropical jet and the polar jet.

METR2023 - Lecture 18 - Segment 3: Vertical Structure of a Standard Extratropical Cyclone

METR2023 - Lecture 18 - Segment 3: Vertical Structure of a Standard Extratropical Cyclone

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

METR2023 - Lecture 26 - Segment 4: Meteorology and Urban Development

METR2023 - Lecture 26 - Segment 4: Meteorology and Urban Development

Meteorology and urban development go hand-in-hand in a lot of respects.

METR2023 - Lecture 19 - Segment 4: Stationary and Occluded Fronts

METR2023 - Lecture 19 - Segment 4: Stationary and Occluded Fronts

Stationary fronts are never perfectly stationary, but are sluggish enough to be called stationary. Occluded fronts can produce very ...

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 27 - Segment 4: Lapse Rate in Pressure Coordinates

METR2023 - Lecture 27 - Segment 4: Lapse Rate in Pressure Coordinates

Not something you'll encounter a lot in the future, but if you're working in pressure coordinates, it might be useful to know.

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 ...

METR2023 - Lecture 25 - Segment 4: Atmospheric Pollutant Information

METR2023 - Lecture 25 - Segment 4: Atmospheric Pollutant Information

Why do we care about these pollutants so much? Here, we answer that question by looking at some of the potential impacts to ...

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 16 - Segment 4: Jet Streaks

METR2023 - Lecture 16 - Segment 4: Jet Streaks

Jet streaks are narrow corridors of stronger flow in the jet-stream. Jet streaks can play a very important role in the atmosphere.

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.