because why not
relief rainfall convectional rainfall Frontal rainfall
Convectional rainfall
convectional rainfall
Equatorial regions experience convectional rainfall because of the intense heating of the sun, which warms the air near the surface. This warm air rises rapidly, cools, condenses, and forms clouds that lead to heavy rainfall. The constant heating and rising of warm, moist air in these regions create a cycle of convectional rainfall.
Convectional rainfall occurs when the ground surface becomes heated by the sun, causing air near the surface to warm, rise, and cool at higher altitudes. It is typically associated with cumulonimbus clouds that produce localized, heavy downpours. Convectional rainfall is common in tropical regions with high temperatures and humidity, leading to rapid and intense rainfall.
Convectional and orographic are types of rainfall. Convectional rainfall occurs when the ground is heated, causing warm air to rise and form cumulonimbus clouds that can result in localized heavy downpours. Orographic rainfall happens when moist air is forced to rise over mountain ranges, leading to cooling, condensation, and precipitation on the windward side of the mountains.
Rainforests are wet because the air pressure at the equator is low. Air is sucked in from the oceans which contains moisture. Low air pressure also means that air rises upwards. As the strong overhead sun evaporates moisture from the forest, the damp air rises, cools and condenses, producing thunderclouds and rainfall on a daily basis. This process is known as convectional rainfall.
Some fancy names have been given to this question, Convectional, Orographic and Frontal. I will stick to the more simple types such as Lite falls , mediums falls and heavy or flooding rains. I am also including mist and fog because they both contain water vapour.
Rainforests are wet because the air pressure at the equator is low. Air is sucked in from the oceans which contains moisture. Low air pressure also means that air rises upwards. As the strong overhead sun evaporates moisture from the forest, the damp air rises, cools and condenses, producing thunderclouds and rainfall on a daily basis. This process is known as convectional rainfall.
thunderstorm and lightning rainfall and floodings
Convectional rainfall is when the sun heats the ground and hot air rises, the hot air then cools down and forms clouds then it rains
The monthly amount of rainfall in Asian rainforests can vary greatly depending on the specific location and time of year. Generally, Asian rainforests receive high amounts of rainfall, with some regions experiencing up to 400 inches per year. Rainfall tends to be more evenly distributed throughout the year in tropical rainforests compared to monsoonal rainforests.