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The thermocline is the boundary layer between a layer of warm water on top of a layer of colder water. Warmer water is less dense, and floats on top of the cold water, which is more dense. The depth of the thermocline will vary with the season, the bottom terrain, and the weather; for example, high winds with large waves will cause considerable mixing in the top 100 feet of water. The thermocline will be below that, or may not exist at all. For scuba divers, it is sometimes possible to lay down on the thermocline; if your buoyancy is perfectly adjusted, you will sink through the less-dense warm water but "float" on top of the denser cold water. Sound waves are bent differently in different water density layers; in submarine warfare, submarines can hide or be exposed depending on where they are relative to the thermocline. In high latitudes, sunlight sometimes reflects off the water surface rather than penetrating the surface and warming the upper ocean layers.
Thermocline
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.
thermocline
the temperature drops rapidly :)
No. Water has its highest density at about 4 °C. Below and above this temperature, its density decreases.
The sun can't reach the thermocline layer to heat that depth of water
a
The thermocline is the boundary layer between a layer of warm water on top of a layer of colder water. Warmer water is less dense, and floats on top of the cold water, which is more dense. The depth of the thermocline will vary with the season, the bottom terrain, and the weather; for example, high winds with large waves will cause considerable mixing in the top 100 feet of water. The thermocline will be below that, or may not exist at all. For scuba divers, it is sometimes possible to lay down on the thermocline; if your buoyancy is perfectly adjusted, you will sink through the less-dense warm water but "float" on top of the denser cold water. Sound waves are bent differently in different water density layers; in submarine warfare, submarines can hide or be exposed depending on where they are relative to the thermocline. In high latitudes, sunlight sometimes reflects off the water surface rather than penetrating the surface and warming the upper ocean layers.
No. It is less dense. That's why it floats above water.
Thermocline
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 sun can't reach the thermocline layer to heat that depth of water
it keeps the water warm
it keeps the water warm
thermocline
The sun can't reach the thermocline layer to heat that depth of water