Media Summary: As important as fronts are in the atmosphere, there is no universally agreed upon definition of a front. Though, most people ... 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 ... How does the atmosphere attempt to resolve radiative balances? One key mechanism is to create cyclones.

Metr2023 Lecture 19 Segment 1 - Detailed Analysis & Overview

As important as fronts are in the atmosphere, there is no universally agreed upon definition of a front. Though, most people ... 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 ... How does the atmosphere attempt to resolve radiative balances? One key mechanism is to create cyclones. A look at surface warm fronts. Though slow-moving, warm fronts play an important role in destabilizing the atmosphere. CORRECTION: At some point in the video, I mention that the Himalayas create a form of dry line in India. This is an inaccuracy. A review of the buoyant force and a look at how it applies itself to the atmosphere.

Radiative imbalances ultimately drive Earth's weather, but where do these imbalances come from? There are a few techniques that can be used to locate fronts on a map. Some are more reliable than others. When in doubt, find ... Weather is the variation of an atmospheric variable over short time-scales (hours or days). Climate is the mean state of an ... A look at some of the physical mechanisms that can strengthen a front (the process of frontogenesis) or weaken a front (the ... A look at the coordinate system most frequently used in meteorology. If the Earth really was flat, that would make the math a lot ... How to incorporate Newton's Second Law into meteorology. This will provide a framework for the next several

A first look at what we mean by "kinematic flow patterns" (vs "dynamic flow patterns").

Photo Gallery

METR2023 - Lecture 19 - Segment 1: Introduction to Fronts
METR2023 - Lecture 19 - Segment 2: Cold Fronts
METR2023 - Lecture 18 - Segment 1: Cyclone Types and the Norwegian Cyclone Model
METR2023 - Lecture 19 - Segment 3: Warm Fronts
METR2023 - Lecture 20 - Segment 1: The Dry Line
METR2023 - Lecture 21 - Segment 1: Atmospheric Buoyancy
METR2023 - Lecture 14 - Segment 1: Global Imbalances of Solar Radiation
METR2023 - Lecture 19 - Segment 5: Identifying Fronts
METR2023 - Lecture 17 - Segment 1: Weather and Climate
METR2023 - Lecture 19 - Segment 6: Frontogenesis and Frontolysis
METR2023 - Lecture 1 - Segment 1: Meteorological Coordinate System
METR2023 - Lecture 1 - Segment 5: Newton's Second Law
View Detailed Profile
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 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 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 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.

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 21 - Segment 1: Atmospheric Buoyancy

METR2023 - Lecture 21 - Segment 1: Atmospheric Buoyancy

A review of the buoyant force and a look at how it applies itself to the atmosphere.

METR2023 - Lecture 14 - Segment 1: Global Imbalances of Solar Radiation

METR2023 - Lecture 14 - Segment 1: Global Imbalances of Solar Radiation

Radiative imbalances ultimately drive Earth's weather, but where do these imbalances come from?

METR2023 - Lecture 19 - Segment 5: Identifying Fronts

METR2023 - Lecture 19 - Segment 5: Identifying Fronts

There are a few techniques that can be used to locate fronts on a map. Some are more reliable than others. When in doubt, find ...

METR2023 - Lecture 17 - Segment 1: Weather and Climate

METR2023 - Lecture 17 - Segment 1: Weather and Climate

Weather is the variation of an atmospheric variable over short time-scales (hours or days). Climate is the mean state of an ...

METR2023 - Lecture 19 - Segment 6: Frontogenesis and Frontolysis

METR2023 - Lecture 19 - Segment 6: Frontogenesis and Frontolysis

A look at some of the physical mechanisms that can strengthen a front (the process of frontogenesis) or weaken a front (the ...

METR2023 - Lecture 1 - Segment 1: Meteorological Coordinate System

METR2023 - Lecture 1 - Segment 1: Meteorological Coordinate System

A look at the coordinate system most frequently used in meteorology. If the Earth really was flat, that would make the math a lot ...

METR2023 - Lecture 1 - Segment 5: Newton's Second Law

METR2023 - Lecture 1 - Segment 5: Newton's Second Law

How to incorporate Newton's Second Law into meteorology. This will provide a framework for the next several

METR2023 - Lecture 9 - Segment 1: Definition of Kinematic Flow

METR2023 - Lecture 9 - Segment 1: Definition of Kinematic Flow

A first look at what we mean by "kinematic flow patterns" (vs "dynamic flow patterns").