Zones within latitudes between 5 degrees to 35 degrees, experiences a non-arid climate with an average temperature above 18 degrees Celsius, humid weather with active vertical uplift and precipitation accompanied by thunderstorms
An overturning circulation in which warm water flows poleward near the surface and is subsequently converted to cold water that sinks and flows equatorward in the interior
Act much like a conveyor belt, transporting warm water and precipitation from the equator toward the poles and cold water from the poles back to the tropics
Higher-altitude areas typically experience cooler temperatures, more precipitation and has strong winds compared to the areas at lower-altitude that experience warmer temperatures
Happens at night where land cools faster than water as does the corresponding air, in this case, the warm air over the water rises and is replaced by the cooler denser air from the land creating an offshore wind
During daytime, land heats faster than water so the air over the land becomes warmer and less dense. It rises and is replaced by a cooler, denser air flowing from over the water