Showing posts with label Fronts. Show all posts
Showing posts with label Fronts. Show all posts

Friday, December 2, 2011

Weather Systems Are Created by the Movement of Air Fronts

The sun and atmosphere work together to create different climates. The air masses are moved by the changes in temperature. The disparate temperatures on the Earth's surface are caused by the different proximity of these areas to the sun. The equator is near the sun on the Earth's entire orbit.

This means that the surface on the Earth at the equator is hot, sunny and has many hours of daylight. The poles are the farthest from the sun and are the coldest and darkest areas of the planet when it is winter and sunny but still cold in what is considered summer there. The farther from the equator you get, the more seasonal the climates become. The climates in the middle of the equators and poles at what are called the middle latitudes are four season climates.

Irene Hurricane

The air moves in masses caused by these irregular heating patterns and the boundaries between them are called fronts. The atmosphere is constantly moving the air around in an attempt to gain equilibrium, or equalized pressure between the warm and cool air. Air that moves also hits stable air and all the molecules mix together. When the cold air moves into warm air, it is called a cold front; a warm front comes from the opposite motion of warm air into cold.

Warm fronts rise above and on top of cold air. As the warm air cools the molecules form water vapor, and become clouds. First are the high cirrus clouds, then come the aptly named mid level followed by thick stratus clouds. Thick stratus clouds are the ones that sometimes cause rain and wind conditions.

When a cold front hits a warm air mass, the result can be more volatile. Convection occurs when the cold front sharply pushes the unstable warm air up. These winds create cumulus clouds and these clouds bring the thunderstorms. The upward motion also creates low pressure situations that make the wind blow harder. Along the cold air in front there will be the actual hard rain and sharp wind. The air behind it that has warmed a bit will simply bring rain. If the cold air takes over the warm air slowly, it becomes an occluded front and stratus clouds with light precipitation result. Stationary fronts occur when two very weak fronts meet and neither takes over the other. They simply sit and rain on the area until all of the air warms up or cools down and progresses on as a cold or warm front.

The oceanic regions of the Earth encompass 70% of the surface area. Climates in coastal areas are affected by the temperature of the seas, as saltwater is a very good conductor of both hot and cold temperatures. Great Britain is much warmer than most of the other land in its same latitude because of the warm Gulf Stream.

Weather Systems Are Created by the Movement of Air Fronts

Monday, October 31, 2011

What Are The Different Kinds Of Weather Fronts?

Weather fronts are where two air streams meet. These air steams have different temperatures and humidity. The warmer air, being less dense, rises up over the cooler air. The warm air expands and therefore cools as it rises. Colder air can hold on to less water vapour. The water condenses out of the atmosphere, forms clouds and eventually rain.

There are different kinds of fronts

Irene Hurricane

Stationary Front - a front that is not moving

When a warm or cold front stops moving, it becomes a stationary front. Once this boundary resumes its forward motion, it once again becomes a warm front or cold front.

Cold Front - transition zone from warm air to cold air

A cold front is defined as the transition zone where a cold air mass is replacing a warmer air mass. Cold fronts generally move from northwest to southeast. The air behind a cold front is noticeably colder and drier than the air ahead of it. When a cold front passes through, temperatures can drop more than 15 degrees within the first hour.

Warm Front - transition zone from cold air to warm air

A warm front is defined as the transition zone where a warm air mass is replacing a cold air mass. Warm fronts generally move from southwest to northeast and the air behind a warm front is warmer and moister than the air ahead of it. When a warm front passes through, the air becomes noticeably warmer and more humid than it was before.

Occluded Front - when a cold front overtakes a warm front

A developing cyclone typically has a preceding warm front (the lead edge of a warm moist air mass) and a faster moving cold front (the leading edge of a colder drier air mass wrapping around the storm). North of the warm front is a mass of cooler air that was in place before the storm even entered the region.

Dry Line - a moisture boundary

A dry line is a boundary that separates a moist air mass from a dry air mass. Also called a "Dew Point Front", sharp changes in dew point temperature can be observed across a dry line. Dry lines are most commonly found just east of the Rocky Mountains, separating a warm moist air mass to the east from a hot dry air mass to the west.

Find out about how Weather fronts effect our daily weather.

What Are The Different Kinds Of Weather Fronts?