Media Summary: Using the concepts discussed to explain the existence and behavior of the subtropical jet and the polar jet. Most hodograph shapes can be broken down into categories, and the ambient wind profile can say a lot about how thunderstorms ... Meteorology and urban development go hand-in-hand in a lot of respects.

Metr2023 Lecture 14 Segment 4 - Detailed Analysis & Overview

Using the concepts discussed to explain the existence and behavior of the subtropical jet and the polar jet. Most hodograph shapes can be broken down into categories, and the ambient wind profile can say a lot about how thunderstorms ... Meteorology and urban development go hand-in-hand in a lot of respects. What the pressure gradient force looks like in natural coordinates. Stationary fronts are never perfectly stationary, but are sluggish enough to be called stationary. Occluded fronts can produce very ... Many meteorologists prefer to represent state variables in the atmosphere as the sum of a background (mean) state and a ...

What is the Polar Cell and why does it exist? Radiative imbalances ultimately drive Earth's weather, but where do these imbalances come from? What is the Hadley Cell and why does it exist? 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 how thermal wind can sometimes (not always) tell us something about temperature advection at some level in the ... Weather is the variation of an atmospheric variable over short time-scales (hours or days). Climate is the mean state of an ...

What happens between weather (days) and climate (decades)? That's when oscillations enter the story, which are variations ...

Photo Gallery

METR2023 - Lecture 14 - Segment 4: Upper Atmospheric Jets
METR2023 - Lecture 22 - Segment 4: Typical Hodograph Classifications
METR2023 - Lecture 26 - Segment 4: Meteorology and Urban Development
METR2023 - Lecture 10 - Segment 4: Pressure Gradient Force in Natural Coordinates
METR2023 - Lecture 19 - Segment 4: Stationary and Occluded Fronts
METR2023 - Lecture 24 - Segment 4: A Widely Used Method of Representing Atmospheric Variables
METR2023 - Lecture 14 - Segment 3: The Polar Cell
METR2023 - Lecture 14 - Segment 1: Global Imbalances of Solar Radiation
METR2023 - Lecture 14 - Segment 2: The Hadley Cell
METR2023 - Lecture 19 - Segment 2: Cold Fronts
METR2023 - Lecture 12 - Segment 4: Physical Consequences of Thermal Wind
METR2023 - Lecture 17 - Segment 1: Weather and Climate
View Detailed Profile
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 22 - Segment 4: Typical Hodograph Classifications

METR2023 - Lecture 22 - Segment 4: Typical Hodograph Classifications

Most hodograph shapes can be broken down into categories, and the ambient wind profile can say a lot about how thunderstorms ...

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 10 - Segment 4: Pressure Gradient Force in Natural Coordinates

METR2023 - Lecture 10 - Segment 4: Pressure Gradient Force in Natural Coordinates

What the pressure gradient force looks like in natural coordinates.

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 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 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 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 14 - Segment 2: The Hadley Cell

METR2023 - Lecture 14 - Segment 2: The Hadley Cell

What is the Hadley Cell and why does it exist?

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 12 - Segment 4: Physical Consequences of Thermal Wind

METR2023 - Lecture 12 - Segment 4: Physical Consequences of Thermal Wind

A look at how thermal wind can sometimes (not always) tell us something about temperature advection at some level in the ...

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 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 ...