373.15 Degrees Kelvin (the same as 100 degrees Celsius)
The boiling point of water on the Römer temperature scale is 60 degrees. Römer scale was developed by René Antoine Ferchault de Réaumur where 0 degree is freezing point and 80 degree is boiling point of water.
A boiling point is a point on the temperature scale at which a substance begins to boil. A melting point is a point on the temperature scale at which a substance freezes. Melting and boiling points are unique to different types of elements.
He thought it a good idea for everyday scientific as well as personal use, to divide the range of temperature between freezing and boiling water into 100 "degrees" and call the temperature of freezing water/melting ice Zero.
Kelvin temperature scale indicates a boiling water temperature of 373º.
There are 100 degrees Celsius between the freezing point (0°C) and boiling point (100°C) on the Celsius temperature scale.
Celsius scale with freezing point of water = 0 oC boiling point of water = 100 oC
The Celsius scale is the most common temperature scale used worldwide, especially in scientific and everyday applications. It is based on 0°C as the freezing point of water and 100°C as the boiling point of water at sea level.
The boiling point of water is at 100 degrees Celsius
Anders Celsius based his temperature scale on the freezing and boiling points of water. He initially defined the scale with 0 degrees representing the boiling point of water and 100 degrees for the freezing point, but this was later reversed to the scale we use today, where 0 degrees is the freezing point and 100 degrees is the boiling point. This standardization was designed to provide a clear and practical way to measure temperature in scientific contexts.
The Kelvin scale has the highest value for the boiling point of water, which is 373.15 K.
Celsius devises the temperature scale based on the boiling point and freezing point of water.
It is a scale for temperature measurement where zero degree is freezing temperature for water and 100 is its boiling point under atmospheric pressure.