SUMMARY
The highest theoretical temperature on Earth is estimated to be between 90 and 100 °C (194 to 212 °F) for dry, darkish soils of low thermal conductivity. This figure is derived from the limitations imposed by mid-level temperatures and the dry adiabatic lapse rate. The highest measured temperature recorded was 56.7 °C (134 °F) in Death Valley on July 10, 1913, although this record has faced scrutiny regarding its accuracy. Future projections indicate that if current environmental trends continue, Earth may resemble Venus in terms of temperature conditions within two billion years.
PREREQUISITES
- Understanding of dry adiabatic lapse rate
- Familiarity with meteorological temperature definitions
- Knowledge of thermal conductivity in soils
- Awareness of historical temperature measurement controversies
NEXT STEPS
- Research the concept of dry adiabatic lapse rate in meteorology
- Study the historical accuracy of temperature records, particularly in extreme environments
- Explore the implications of climate change on Earth's temperature projections
- Investigate the thermal properties of different soil types and their impact on temperature measurements
USEFUL FOR
Climate scientists, meteorologists, environmental researchers, and anyone interested in the implications of temperature extremes on Earth.