Warm Fronts

Imagine that a continental polar air mass has settled in the Midwest and a maritime tropical air mass moves toward it from the southeast. As the air masses collide, a warm front results. A warm front occurs when a warm air mass overtakes a cold air mass.

Figure 22 shows what happens when a warm front forms. Because the cold air is denser, it remains close to the ground. The advancing warm air mass rises up over the cold air mass. The surface of a warm front is usually less steep than that of a cold front, as you can see by comparing Figures 21 and 22. A warm front has a gentle slope because the advancing warm air mass gradually moves up and over the cold air mass.

Figure 22 A warm front occurs when a warm air mass overtakes a cold air mass.
Applying Concepts What types of weather are associated with cold fronts and warm fronts?

The diagram shows a that the cold air would remain closer to the ground, sinking under the warm air mass.  The warm air mass rises above the clouds over a segment of land. Precipitation occurs.

As the warm air rises, stratus clouds form. If the warm air mass contains a large amount of moisture, there will be a steady rain. Occasionally heavy showers or thunderstorms occur. Once the front has passed, the warm air mass settles in. The skies are mostly clear, often with some cumulus clouds present, and temperatures rise.

Stationary Fronts

The clash of air masses is not always as simple as those that produce cold fronts and warm fronts. Sometimes when two air masses converge, neither air mass overruns the other. Rather, a front forms, and either stays where it formed or moves slowly. When two unlike air masses have formed a boundary but neither is moving, the front is called a stationary front. Stationary fronts often result in clouds and steady rain or snow for several days.

Occluded Fronts

Another kind of front can occur because cold fronts generally move faster than warm fronts. An occluded front forms when a warm air mass is caught between two cooler air masses. The colder air masses force the warm air mass to rise, cutting it off from the ground and trapping it between the two cold air masses. As this warm air rises and cools, its water vapor typically condenses. As a result, occluded fronts are generally accompanied by cloudy skies and precipitation.


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Table of Contents

Physical Science CHAPTER 1 Science Skills CHAPTER 2 Properties of Matter CHAPTER 3 States of Matter CHAPTER 4 Atomic Structure CHAPTER 5 The Periodic Table CHAPTER 6 Chemical Bonds CHAPTER 7 Chemical Reactions CHAPTER 8 Solutions, Acids, and Bases CHAPTER 9 Carbon Chemistry CHAPTER 10 Nuclear Chemistry CHAPTER 11 Motion CHAPTER 12 Forces and Motion CHAPTER 13 Forces in Fluids CHAPTER 14 Work, Power, and Machines CHAPTER 15 Energy CHAPTER 16 Thermal Energy and Heat CHAPTER 17 Mechanical Waves and Sound CHAPTER 18 The Electromagnetic Spectrum and Light CHAPTER 19 Optics CHAPTER 20 Electricity CHAPTER 21 Magnetism CHAPTER 22 Earth's Interior CHAPTER 23 Earth's Surface CHAPTER 24 Weather and Climate CHAPTER 25 The Solar System CHAPTER 26 Exploring the Universe Skills and Reference Handbook