Rainfall in mountain areas is called: Orographic rainfall.
The Ethiopian highlands experience predominantly orographic rainfall. This occurs when moist air is forced to rise over the high mountains, leading to cooling and condensation of the water vapor, resulting in rainfall. This type of rainfall is important for supporting agriculture in the region.
Depressional rainfall occurs when moist air is forced to rise over a depression or low-pressure system, resulting in increased condensation and precipitation. This type of rainfall often leads to heavy and prolonged rain events in the vicinity of the depression.
Convectional rainfall occurs when warm air rises, cools, and condenses to form rain clouds. Relief rainfall occurs when moist air is forced to rise over elevated terrain and cool, leading to precipitation. Frontal rainfall occurs when two air masses with different temperatures and moisture content meet, causing the warmer air to rise and condense, resulting in rainfall.
During a monsoon, heavy rainfall occurs due to the seasonal shift in wind patterns. This can result in prolonged periods of intense rainfall, leading to flooding and landslides in some regions. Monsoons are characterized by a distinct wet season followed by a dry season.
type 1
Rainfall in mountain areas is called: Orographic rainfall.
The most common type of rainfall in the UK is frontal rainfall, which occurs when warm and cold air masses meet, causing the warm air to rise and cool, leading to condensation and precipitation. This type of rainfall is often associated with the passage of weather fronts across the country.
The Ethiopian highlands experience predominantly orographic rainfall. This occurs when moist air is forced to rise over the high mountains, leading to cooling and condensation of the water vapor, resulting in rainfall. This type of rainfall is important for supporting agriculture in the region.
Another name for orthographic rainfall is relief rainfall. It occurs when warm, moist air is forced to rise over elevated terrain, leading to cooling and condensation, followed by precipitation. This type of rainfall is common in mountainous regions.
water
covectinal and relief rainfall
The retreating rainfall monsoon occurs when the temperature on land is significantly warmer or cooler than the temperature of the ocean.
Convectinal rainfall occurs when warm air rises, cools, condenses, and forms clouds, leading to precipitation. This type of rainfall is common in tropical regions where the air is warm and moist, creating convective currents that trigger rainfall.
Depressional rainfall occurs when moist air is forced to rise over a depression or low-pressure system, resulting in increased condensation and precipitation. This type of rainfall often leads to heavy and prolonged rain events in the vicinity of the depression.
Tropical climate. Rainfall occurs all the year because of the domination of low pressure.
Conventional rainfall refers to rainfall that occurs due to the lifting of warm, moist air masses and the subsequent condensation of water vapor. It is typically associated with thunderstorms and occurs in localized areas. Conventional rainfall can be intense but short-lived.