noun
: the temperature at which ice is in equilibrium with air-saturated water at standard atmospheric pressure and which is commonly used as a fixed point in calibrating thermometers and is represented by 0° C or 32° F
noun
: the temperature at which ice is in equilibrium with air-saturated water at standard atmospheric pressure and which is commonly used as a fixed point in calibrating thermometers and is represented by 0° C or 32° F
Webster's New International English Dictionary. Новый международный словарь английского языка Webster. 2012