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Freezing temperature of finger skin
Journal of Applied Physiology
|October 1, 1976
Summary
Frostnip occurs at supercooled skin temperatures. The apparent freezing point of skin, influenced by wind speed, is lower than the true freezing point, indicating increased frostbite risk in windy, cold conditions.
Area of Science:
- Environmental Physiology
- Dermatology
- Biophysics
Background:
- Frostnip and frostbite are risks in cold environments.
- Skin supercooling precedes ice crystallization and tissue damage.
- Understanding freezing points is crucial for cold injury prevention.
Purpose of the Study:
- To determine the apparent freezing point of skin under varying wind conditions.
- To analyze the relationship between supercooled skin temperature and the apparent freezing point.
- To compare the apparent freezing point with the true freezing point of skin.
Main Methods:
- Inducing frostnips in 45 subjects by cooling fingers in -15°C air with controlled wind speeds.
- Measuring skin temperatures during cooling and ice crystallization.
- Calculating apparent freezing points and comparing them using analysis of covariance.
Main Results:
- Mean supercooled skin temperature at frostnip onset was -9.4°C.
- Mean skin temperature rise due to heat of fusion was 5.3°C.
- Apparent freezing point decreased with increasing wind velocity, though not always statistically significant.
- The highest calculated apparent freezing point was significantly lower than the true freezing point determined in brine.
Conclusions:
- Wind significantly affects the apparent freezing point of skin.
- The apparent freezing point is lower than the true freezing point, especially at higher wind speeds.
- These findings highlight the increased risk of cold injury in windy conditions.