thermocline
The temperate zone has warm summers and cool or cold winters.
The midnight zone, also known as the abyssopelagic zone, is typically found in cold water. This zone lies between about 3,280 to 13,124 feet (1,000 to 4,000 meters) below the ocean surface, where temperatures are generally colder due to the lack of sunlight and proximity to deep ocean currents.
The aquifer zone that lies between the water table and Earth's surface is called the unsaturated zone or vadose zone. This zone contains soil and rock layers where pores are not completely filled with water, allowing for the movement of both water and air.
This is known as the phreatic surface or water table.
The water table or phreatic surface.
The temperate zone has warm summers and cool or cold winters.
the zone of aeration
warm water
The layer of water where temperature drops sharply is called the thermocline. This is a zone of rapid temperature change in the ocean that separates the warm surface water from the colder deep water.
They live in warm temperatures.
The upper surface of the zone of saturation is known as the water table. This is the level beneath the Earth's surface where the soil and rock are fully saturated with water. Above the water table lies the unsaturated zone, where both water and air are present in the soil and rock.
The sun’s rays hit the surface directly.
The midnight zone, also known as the abyssopelagic zone, is typically found in cold water. This zone lies between about 3,280 to 13,124 feet (1,000 to 4,000 meters) below the ocean surface, where temperatures are generally colder due to the lack of sunlight and proximity to deep ocean currents.
The aquifer zone that lies between the water table and Earth's surface is called the unsaturated zone or vadose zone. This zone contains soil and rock layers where pores are not completely filled with water, allowing for the movement of both water and air.
The transition between the warm surface layer and the deep cold water in the oceans is marked by a distinct boundary called the thermocline. The thermocline is a region where temperature decreases rapidly with depth, signaling the shift from warmer surface waters to cooler deep waters in the ocean.
Its when a Aquifer recharges bc the surface has to much water realeasing the discharge of water.
aeration zone