Above
Water is denser below the thermocline. The thermocline is a layer in a body of water where temperature decreases rapidly with depth, leading to increased density in the colder, deeper water. This stratification means that the warmer water above the thermocline is less dense compared to the cooler water below it.
The temperature in the zone beneath the thermocline remains relatively stable as it experiences minimal mixing with the warmer water above and the cooler water below. This results in a sharp temperature gradient between the layers above and below the thermocline.
a
The sun can't reach the thermocline layer to heat that depth of water
It located in the lowest portion of the brain. It is connected to the spinal cord below, and the pons above.
This is essentially correct, the correct use of Thermocline is often misunderstood. the temperature of the water is nearly always cooler than the outside air, the temperature declines- thermo-heat- pluc Decline- hence thermocline, with increasing depth but the external pressure goes up, an important problem for submarine designers, divers, and the like. almost always the water temperature is lower than the surrounding air, as shore-types well know.
The thermocline is a layer in the ocean where temperature changes rapidly with depth, typically separating warmer surface waters from cooler, deeper waters. This gradient affects marine life by influencing nutrient availability, as the cooler, nutrient-rich waters below the thermocline are often less accessible to surface-dwelling organisms. Additionally, the thermocline can impact ocean circulation and climate patterns, as it plays a crucial role in the mixing of water layers. Overall, the thermocline is essential for maintaining the ecological balance in marine environments.
The average temperature of the deep water below the thermocline can vary depending on the location and depth, but it typically ranges from 2 to 4 degrees Celsius in most ocean regions. This deep water is characterized by its colder temperatures due to lack of sunlight and limited interaction with the atmosphere.
It is most difficult to locate the location of sounds directly above the head or below the chin. This is because the ears are located on the sides of the head, making it challenging to discern vertical directionality.
point b - apex
the deep sea is the lowest layer in the ocean,existing below the thermocline,at a depth of 1,000 fathoms(1,800) or more.
Yes, more dense (colder water) sinks below less dense (warmer) water. That is the reason for the Thermocline.^^^^^^A widespread permanent thermocline exists beneath the relatively warm, well-mixed surface layer, from depths of about 200 m (660 feet) to about 1,000 m (3,000 feet), in which interval temperatures diminish steadily. The deep waters below the thermocline layer decrease in temperature much more gradually toward the seafloor. In latitudes marked by distinct seasons, a seasonal thermocline at much shallower depths forms during the summer as a result of solar heating, and it is destroyed by diminished insolation and increased surface turbulence during the winter. Water density is governed by temperature and salinity; consequently, the thermocline coincides generally with the pycnocline, or layer in which density increases rapidly with depth. The middle layer of water in a lake or reservoir during the summer is also called a thermocline.^^^^"thermocline." Encyclopædia Britannica. Encyclopædia Britannica 2009 Deluxe Edition. Chicago: Encyclopædia Britannica, 2009.