20 degs Celsius
YES. A thermocline is a sudden change in the temperature of the water. A halocline is a sudden change in the salinity of the water. A pycnocline is a sudden change in both. The warmer, fresh water will advance to the top of the water, and the cold, salty water will stay at the bottom. Since there are two factors effecting this, pycnoclines happen to be more distinct.
Removing heat from the air will lower its temperature.
The Earth's temperature depends on the location. The coldest temperature can be as low as -89° C in Antarctica and the highest can be 57.7° C in the deserts.
engine coolant
the rate of contraction increases with a rise in temperature and decreases with a fall in temperature
The sun can't reach the thermocline layer to heat that depth of water
A rapid change in temperature with depth in the ocean is called thermocline. A rapid change in density with depth in the ocean is called the pynocline.Thermocline
The sun can't reach the thermocline layer to heat that depth of water
The sun can't reach the thermocline layer to heat that depth of water
all lakes have a thermocline. Summer time the thermocline will be higher. In winter lower. Thermocline is a layer of water that is separated by temperature. Some lakes have a summer thermocline of 40 feet. But colder water in any lake will fluctuate with how cold and access to sunlight.
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.
Thermocline
A thermocline is a rapid change in temperature with depth in the ocean. Depending on the latitude and season, thermoclines can be present or absent and vary in depth of occurrence, however a thermocline will usually be found in the mesopelagic zone.
It involves thermocline.
Thermocline
A zone of rapid temperature change is a thermocline.
The term you are referring to is "thermocline." It is the layer of water in the ocean where there is a rapid change in temperature with depth, serving as a barrier between warmer surface water and colder deep water.