SUMMARY
Relative humidity at temperatures below zero degrees Celsius is defined as the ratio of the partial pressure of water vapor to the saturated vapor pressure at that temperature. Even at temperatures as low as -58°C, as observed in Vostok, Antarctica, the air can still hold water vapor, resulting in a relative humidity (RH) of 42%. Relative humidity cannot be negative; however, the dew point temperature can be below zero. This discussion clarifies that while water condenses to form ice at 0°C, air can still contain moisture at sub-zero temperatures.
PREREQUISITES
- Understanding of relative humidity and its definition
- Knowledge of vapor pressure and saturation concepts
- Familiarity with the concept of dew point temperature
- Basic principles of thermodynamics related to phase changes
NEXT STEPS
- Research the concept of supercooling and its implications on water states
- Learn about vapor pressure and its relationship with temperature
- Explore the differences between relative humidity, absolute humidity, and dew point temperature
- Investigate real-world applications of humidity measurements in extreme environments
USEFUL FOR
Climate scientists, meteorologists, and anyone interested in atmospheric science and the behavior of water vapor at low temperatures.