Discussion Overview
The discussion revolves around the effects of air resistance and altitude on body temperature during skydiving. Participants explore whether a skydiver would feel hot, cold, or neither due to factors such as ram pressure, friction, and the temperature gradient with altitude. The conversation includes theoretical considerations, personal anecdotes, and references to atmospheric science.
Discussion Character
- Exploratory
- Technical explanation
- Conceptual clarification
- Debate/contested
- Mathematical reasoning
Main Points Raised
- Some participants suggest that the temperature experienced during a skydive would be cold due to the altitude and the cooling effect of wind, while others consider the potential heating from air resistance and friction.
- One participant notes that the temperature at skydiving altitudes can be significantly lower than at ground level, referencing a temperature of -52°C at high altitudes.
- Another participant discusses the negligible effect of wind resistance on heating compared to the ambient temperature at altitude, emphasizing that the temperature drops with increasing altitude.
- A mathematical approximation is presented to compare the thermal power absorbed due to friction and the thermal power lost due to convection, concluding that frictional heating is minimal for skydivers.
- Several participants delve into the heating mechanisms of the stratosphere and thermosphere, discussing the role of ozone and photochemical reactions in temperature variations at different altitudes.
- Questions arise regarding the nature of UV radiation and its interaction with ozone, including whether ozone can reform after being split and the fate of UV radiation.
- Anecdotal evidence is shared about a skydiving incident, highlighting the extreme conditions experienced at high altitudes.
Areas of Agreement / Disagreement
Participants generally agree that skydivers will experience cold temperatures due to altitude, but there is disagreement regarding the extent of heating from air resistance and friction. The discussion remains unresolved regarding the specific mechanisms and effects of temperature changes at different altitudes.
Contextual Notes
Limitations include assumptions about atmospheric conditions, the idealized nature of temperature approximations, and the complexity of thermal dynamics in freefall situations. The discussion also touches on the nuances of UV radiation and ozone interactions without reaching definitive conclusions.