Because colder air is forcing it upward.
considerably ahead of the actual frontal boundary
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. Stationary fronts may bring several days of clouds and precipitation as air is constantly forced to rise, and multiple low pressure systems can move over the frontal boundary bringing with it rain, snow, and potentially wind.
When warm moist air rises it cools and condenses.
warm waters and moist air. the water starts to rise and the condensation forms clouds and raindrops.
There are three main types of rainfall, convectional rainfall, relief rainfall and frontal rainfall. Relief rainfall is when the warm moist air from the sea (Atlantic Ocean) is forced to rise over mountains and as the moist air gets higher it gets colder so it gradually condenses and becomes water droplets and it rains/ prcipitates. Relief rainfall is common along the west side of Britain where there are more high lands. Convestional rainfall is when the sun comes out and heats up the land, this causes the air around it to become warm too. The warm air currents rise and as it rises it gets colder so it gradually condenses and the water vapou become water droplets and it rains/precipitates. Convectional rainfall is mostly common around towards the south of Britain in the summer. Frontal rainfall is when cold air and warm air meet, the warm, light air wants to get past the heavy cold air so it casually rises above it. Its rising makes it get colder which makes the warm air cold air, it condenses and guess what? It rains/ precipitates! Frontal rainfall is mostly common all over Britain especially in the winter.
considerably ahead of the actual frontal boundary
At a frontal boundary warm, moist air can be lifted upwards, where the water vapor in it cools, and condenses producing clouds, rain, and sometimes thunderstorms. When these thunderstorms interact with another condition called wind shear, they can start rotating. In some of these storms that rotation can develop into tornadoes.
Created when warm, moist air is forces to rise over a barrier. (mountain).
Generally tornadoes form near a boundary between warm, moist air and cool, dry air. The warm, moist air mass is more important as it provide the energy that fuels the storm.
The heat of the sun.
Warm front--rise in temperature; gentle rain; longer duration Cold front--drop in temperature; violent precipitation including storms; shorter duration Stationary front--many days of precipitation along the frontal boundary Occluded front--precipitation
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. Stationary fronts may bring several days of clouds and precipitation as air is constantly forced to rise, and multiple low pressure systems can move over the frontal boundary bringing with it rain, snow, and potentially wind.
Frontal rain is rain that comes from a weather front. For example, a cold front lifts warm, moist air. This parcel of air is raised to the LCL, and higher. Saturation occurs first, and then precipitation forms. Frontal rainfall is when cool air and hot air meets together. the warm air rises above the cool air.the warm air eventually cools down and water vapour condenses then clouds forms and precipitation occurs.
When warm moist air rises it cools and condenses.
Frontal wedging is when warm air and cold air collide at the surface, or front.
warm waters and moist air. the water starts to rise and the condensation forms clouds and raindrops.
Maritime tropical air masses are warm and moist.