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Chapter 9 — Weather Patterns & Fronts

PHY 116 • Introduction to Meteorology • Fall 2026

TEST 4 — WEDNESDAY, DECEMBER 9, 2026

Chapters 9, 10 and 11. Exam during your scheduled class time. Questions? Email Professor Hoffman.

The original course notes state that a missed exam is replaced by the final exam grade; confirm details in the current course syllabus.

Midlatitude Cyclones and Weather Patterns

Midlatitude cyclones are large low-pressure systems, often over 600 miles (1,000 km) across, that commonly travel west to east in the prevailing westerlies. In the Northern Hemisphere, winds circulate counterclockwise and inward around the surface low. A cold front and often a warm front extend from the low-pressure center.

Important connection to Chapter 4: Frontal lifting forces warmer air upward, where cooling and condensation can produce clouds and precipitation. Wind direction describes where the wind comes from. Your position relative to the low-pressure center matters.

Chapter 9 Class Videos

Chapter 9 — Part 1

Chapter 9 — Part 2

Fronts and Air Masses — Video 1

Fronts and Air Masses — Video 2

Fronts and Air Masses — Video 3

Fronts and Air Masses — Video 4

Five Types of Fronts and Boundaries

Fronts separate air masses with different temperature and density. The surface weather can change rapidly as a boundary passes.

Cold Front

Advancing colder, denser air pushes beneath warmer air. A band of showers or thunderstorms may develop. Winds often shift and temperatures fall after passage.

Warm Front

Advancing warm air rises over retreating colder air. Clouds often lower and thicken ahead of the front, with widespread precipitation possible.

Stationary Front

A boundary with little movement. Clouds and precipitation may persist near it.

Occluded Front

A faster cold front catches a warm front and lifts the warm air away from the surface. Cold-type and warm-type occlusions depend on the relative temperatures of the surrounding air.

Dryline

A sharp boundary between humid and much drier air, common in the Plains. It can help trigger severe thunderstorms when other ingredients are present.

Frontal boundary diagrams
Frontal boundary diagrams
Cold front cross-section
Cold front cross-section
Warm front cross-section
Warm front cross-section
Warm front structure
Warm front structure

Weather Before, During and After a Front

Cold Front — Typical Changes

ElementBeforeDuring PassageAfter
WindsSouth to southwestGusty and shiftingWest to northwest
TemperatureWarmOften drops sharplyCooler
PressureFallingNear minimum, then risingRising
CloudsIncreasing cloudsOften cumulonimbusCumulus, then clearing
PrecipitationPossible showersShowers or thunderstorms; sometimes heavyShowers ending
Dew PointOften higherMay dropUsually lower

Warm Front — Typical Changes

ElementBeforeDuring PassageAfter
WindsOften easterly or southeasterlyVariable or shiftingOften southerly
TemperatureCoolRisingWarmer
PressureFallingLeveling offVariable
CloudsCirrus → cirrostratus → altostratus → nimbostratusLow clouds possibleMay break up
PrecipitationWidespread rain or wintry precipitation possibleDrizzle or light precipitation possibleOften ending
Dew PointOften risingHigherTypically more humid

These are typical patterns, not guarantees. Actual wind shifts, cloud types and precipitation depend on the storm track, season and atmospheric profile.

Life Cycle of a Midlatitude Cyclone

In the Norwegian cyclone model, a disturbance develops along a frontal boundary. A wave and surface low form; warm air moves poleward while cold air advances equatorward. The cold front often catches the warm front, creating an occlusion. As the temperature contrast and upper-level support diminish, the system generally weakens.

Midlatitude cyclone
Midlatitude cyclone
Cyclone circulation
Cyclone circulation
Warm front
Warm front
Air masses
Air masses
Cyclone structure
Cyclone structure
Cross-section
Cross-section
Cyclone evolution
Cyclone evolution
Cyclone evolution
Cyclone evolution
Wind field around a storm
Wind field around a storm
Wind direction compass
Wind direction compass

Upper-Level Support

When divergence aloft removes air from the column faster than low-level convergence replaces it, surface pressure can fall and the cyclone can intensify. When this balance reverses, surface pressure may rise and the cyclone can weaken.

Textbook focus: Pages 241–243, including how cloud cover, wind, temperature, precipitation and pressure change as a storm moves past a location.

Analyze Current Weather Maps

Practice locating low-pressure centers, frontal boundaries, wind shifts and precipitation areas. These links open current operational charts rather than relying on older embedded graphics that may no longer load.

WPC Surface Analysis

Open Surface Map

WPC National Forecast Charts

Open Forecast Maps

NWS New York Forecast Office

NYC & Long Island Forecasts

WPC Precipitation Forecasts

Open Rainfall Outlook

PowerPoint Presentations and Diagrams

Clouds and Precipitation

Open PowerPoint

Four Ways Air Rises

Open PowerPoint

Chapter 9 Fronts

Open PowerPoint

Additional station-plot and weather-symbol material appeared below the original “STOP HERE FOR TEST 4” line and is therefore not included in the required exam review. For enrichment, use WPC station plot explanations.

Test 4 — Chapter 9 Review

Wednesday, December 9, 2026 • Chapters 9, 10 and 11

Ask a Chapter 9 Question