The zone near the surface of a body of water is typically referred to as the epipelagic zone or photic zone, where sunlight penetrates, allowing photosynthesis to occur. In the context of the ocean, this zone extends from the surface down to about 200 meters. The middle depth zone often refers to the mesopelagic zone, which lies below the epipelagic zone, extending from approximately 200 meters to 1,000 meters deep, where light diminishes and temperatures drop. Both zones are crucial for marine life and ecosystems.
No, the nortical zone and the middle layer of the ocean are not the same. The nortical zone refers to the region of the ocean near the surface where there is abundant sunlight. The middle layer, also known as the mesopelagic zone, is the twilight zone where sunlight is limited and deeper-sea creatures reside.
The surface zone
The open ocean is split up into three parts: the intertidal zone (near the surface) the neritic zone (on the continental shelf) and the deep ocean zone. The deep-ocean zone's depth ranges from 200-9,000 meters. it is filled with a fishes bad romance from lady gaga
They live in warm temperatures.
28 degrees on surface and gradually decreasing towards depth.
between 410 and 660 kilometers below the earth's surface.
Neritic zone
the depth of the pelagic zone is 11 kilograms
the depth of the dark zone
The midnight zone comes after the Twilight zone; it extends from 3280 feet to 13,124 feet and temperatures are near-freezing. There is no light except for that of the bioluminescent animals that live there.
Photic - light; photic zone - light falling zone. Depth of photic zone refers to the distance travelled by sunlight in to the depth of the water and enable photosynthesis. It is measured using SECCHI DISC or photometer. Depth of photic zone is influenced by turbidity. It includes atmosphere-water surface to the depth where the total penetrating light intensity falls by 1%. This zone is a zone of productivity.
The temperature layers in ocean water are typically divided into three main zones: the surface zone, the thermocline, and the deep zone. The surface zone is the warmest and most variable in temperature due to interaction with the atmosphere. Below the surface zone is the thermocline, where temperature decreases rapidly with depth. Finally, the deep zone is characterized by consistently cold temperatures.