How does cold fronts move




















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Want to add a little wonder to your website? Help spread the wonder of families learning together. We sent you SMS, for complete subscription please reply. Follow Twitter Instagram Facebook. What is a cold front? Does a cold front always bring precipitation? When are cold fronts most common? Wonder What's Next? Tomorrow's Wonder of the Day will help you overcome daily obstacles!

Try It Out Are you ready to predict the weather? Ask a friend or family member to help you check out the following activities: Do you keep an eye on the weather? Some people like to watch the weather forecast every day and then see if the weather forecaster was right or not. Some people watch weather shows on television like they were primetime shows! Whether pun totally intended or not you usually keep track of the weather, try to keep a weather journal for the next week.

Each day, find out what the forecast is by watching a local weather report or looking it up online. Then watch and see what happens with the weather. Record the high temperature, low temperature, and whether or not you got any precipitation rain or snow. Weather Fronts. Principle Fronts are zones of transition between two different air masses. The zone may be 20 miles across or it may be miles across, but from one side of a front to the other, one clearly would sense that the properties of an air mass had changed significantly e.

If the wedge is moving into an area of warmer air, the front is called a cold front. If the wedge is retreating and warmer air is moving into an area previously occupied by cool air, the front is termed a warm front. Figure 1 - Types of Fronts Definition Fronts are boundaries between air masses of different temperatures. Fronts are actually zones of transition, but sometimes the transition zone, called a frontal zone, can be quite sharp.

There are four types of fronts that will be described below: cold front, warm front, stationary front, and occluded front. Not all of these patterns may be obvious or even occur, but these are some signs. This results from the fact that low-level southerly winds in the "warm sector" of the cyclone rise up and over the cooler, more dense air at the surface located north of the warm front.

The lifting leads to saturation, cloud formation, and, ultimately, to some form of precipitation. Stationary Fronts Stationary front- a front that does not move or barely moves. The weather at a cold front varies with the season. Along a warm front , a warm air mass slides over a cold air mass. When warm, less dense air moves over the colder, denser air, the atmosphere is relatively stable.

Imagine that you are on the ground in the wintertime under a cold winter air mass with a warm front approaching. The transition from cold air to warm air takes place over a long distance so the first signs of changing weather appear long before the front is actually over you. Initially, the air is cold: the cold air mass is above you and the warm air mass is above it. High cirrus clouds mark the transition from one air mass to the other.

Over time, cirrus clouds become thicker and cirrostratus clouds form. As the front approaches, altocumulus and altostratus clouds appear and the sky turns gray. Since it is winter, snowflakes fall.

The clouds thicken and nimbostratus clouds form. Snowfall increases. Winds grow stronger as the low pressure approaches. As the front gets closer, the cold air mass is just above you but the warm air mass is not too far above that.

The weather worsens. As the warm air mass approaches, temperatures rise and snow turns to sleet and freezing rain. Warm and cold air mix at the front, leading to the formation of stratus clouds and fog. On the other hand, if warmer air is replacing cold air, then the front should be analyzed as a warm front. Common characteristics associated with cold fronts have been listed in the table below. Terms for using data resources.



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