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Answer:isothermal
Explanation:isothermal can be defined as a line on a map or chart of the earth's surface connecting points having the same temperature at a given time or the same mean temperature for a given period.
An isothermal process is a change of a system, in which the temperature remains constant: ΔT =0. ... In contrast, an adiabatic process is where a system exchanges no heat with its surroundings (Q = 0).
No thermocline exists in high-latitude regions because there is little temperature difference between the top and bottom of the water column. In such a situation the water column is said to be isothermal.
- No presence of thermocline in high-latitude ocean waters. This is due to the fact that surface waters are cooler. The temperature is said to be like that of deeper waters and as such there is no rapid change in temperature.
An isothermal process is known to be a thermodynamic process where the temperature of the system remains constant.
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