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The boiling point of water is 100Â°C, 212Â°F or 373.15 Kelvin under standard conditions at sea level (at one atmosphere of pressure). The boiling point of water and any other substance depends on the atmospheric pressure, which changes with elevation. At higher altitudes, the pressure is lower, and so water boils at a lower temperature. If the barometric pressure is not at the standard value, the boiling point will be different. For example, water boils at 72 degrees Celsius on Mount Everest. Under a partial vacuum water boils at room temperature.
The boiling point of water is the temperature at which the vapour pressure of the liquid water equals the surrounding pressure. Since we also know that pressure and temperature are directly proportional so water at high pressure will have high boiling point and at low pressure will have low boiling point. When we maintain vacuum (pressure below atmospheric pressure) the water begins to boil at temperature lower than 100 degree Celsius. Here is table showing the variation of boiling point of water with pressure.