Tropical
Convectional Precipitation
interior plains
Convectional precipitation is the type of precipitation caused by air being heated at the surface of the earth. Convectional precipitation can fall anywhere on earth.
The Earth's precipitation occurs through convectional, orographic, or frontal mechanisms. Convectional precipitation happens when warm air rises, cools, and forms clouds. Orographic precipitation occurs when moist air is forced to rise over a mountain, leading to cooling and rainfall. Finally, frontal precipitation happens at the boundary of two air masses with different temperatures and moisture levels, causing the warm air to rise and condense into precipitation.
There is more precipitation along the coast in the pacific west than the farther land because of the convectional currents that cause convectional rainfall.
climate
As the air rises, it cools and condenses. Clouds form and precipitation occurs.
Convectional precipitation and storms are caused by the heating of the Earth's surface, which warms the air above it. As the air warms, it becomes less dense and rises, creating uplifting motions that lead to the formation of clouds and eventually precipitation. This process is known as convection, and when it intensifies, it can lead to the development of thunderstorms.
Average annual precipitation is an example of climate.
the climate region that has heavy precipitation and mild temperature is the temperate marine climate
Average annual precipitation is an example of climate.
the climate region that has heavy precipitation and mild temperature is the temperate marine climate