The Newton rate of temperature change is a unit of measurement used to describe the rate at which temperature changes. It is based on the Newton scale, which was developed by Sir Isaac Newton in the early 18th century.
The Newton rate of temperature change is calculated by dividing the change in temperature by the time it takes for the temperature to change. It is expressed in degrees Newton per hour (°N/h).
The main difference between the Newton rate of temperature change and other temperature scales, such as Celsius or Fahrenheit, is the unit of measurement. The Newton scale is based on a different reference point and is not commonly used in everyday temperature measurements.
The Newton scale is not widely used because it is based on a reference point that is not commonly encountered in everyday life. It also does not have a consistent relationship with other temperature scales, making it difficult to compare temperatures measured in different scales.
The Newton rate of temperature change is most useful in scientific research and engineering applications where precise and consistent temperature measurements are needed. It can also be used to describe extreme temperature changes, such as in industrial processes involving rapid heating or cooling.