verical ransfer of hea is known as convecion process
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Glasgow
The difference lies in what causes the rainfall to occur. In convectional rainfall, the sun heats the earth and the heat causes moisture from soil, plants and open water bodies to evaporate. This moisture is carried upwards through convective air currents until it reaches a certain altitude. At that point, where the air is cooler, it condenses and creates water droplets (rain). This usually occurs in the afternoon on warm summer days. Frontal rainfall occurs because of the movement of the fronts of two air masses. When a cold front is moving over a mass of warm air, it causes the warm moist air to rise. In this case, rain occurs ahead of the cold front. When a warm front is moving over a mass of cold air, the warm moist air is forced upward, and the rain occurs over or behind the front. Finally, relief rainfall is caused by changes in topography. Moist warm air can be forced upward by mountains, for example, which causes the moisture to condense into rain. This type of rainfall occurs on the side of the mountain away from the wind direction.
It is a low pressure area, formed at the boundry between two different air-masses.They occur in middle or high latitudes. the formation of frontal depression is known as frontogenesis.
The result will most likely be a frontal low.
Thumb abduction and adduction is in the sagittal plane. However, finger abduction and adduction is in the frontal/coronal plane. Do these movements in the anatomical position and that will help you see that the thumb is not abducting or adducting in the frontal plane rather the sagittal plane.
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Glasgow
Al the time.
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.
Conventional rainfall occurs because the ground is heated in early morning.so it occurs in early afternoon.Relief rainfall occur only when the South East Trade Wind blows with full force and the South East Trade Wind can blows at any time of the day
When the Earth surface is heated by the sun, the AIR above the surface is also warm. The warm air rises, and when it rises it cools down. Then it condenses and form clouds. And then it rains. (If the air rises very quickly cumulonimbus clouds can form) So the simple answer, Convectional Rainfall: Water forces to rise by heat.
Relief rainfall occurs when moist air is forced to rise over topographic barriers such as mountains. As the air rises, it cools, condenses, and forms clouds, leading to rainfall on the windward side of the mountain. This phenomenon is common in areas with mountain ranges, such as the western coast of North and South America.
Frequently occur near mountains Occur when warm moist air rises
interior plains
this a relief rain fall. Here western High land Climate dominates. Murree located in sub himalayas.
Clouds and precipitation
Frontal Plane