Temperature is a key concept in science and daily life. The three most commonly used scales—Fahrenheit, Celsius, and Kelvin—each have unique characteristics and uses.
Temperature measures the average kinetic energy of particles in a substance, indicating how hot or cold something is.
Developed by Daniel Gabriel Fahrenheit in the early 18th century, based on three reference points, including the freezing point of brine (0°F).
Created by Anders Celsius in 1742, using water's freezing (0°C) and boiling (100°C) points.
Proposed by Lord Kelvin in the 19th century, starting at absolute zero (0 K) with the same degree size as Celsius.
°C = (5/9) × (°F - 32)
°F = (9/5 × °C) + 32
K = °C + 273.15
°C = K - 273.15
Used in weather forecasts, cooking, and daily temperature readings in the U.S.
The international standard for weather, cooking, and scientific research.
Primarily used in physics, chemistry, and space science.
While Celsius and Kelvin are the global scientific standards, Fahrenheit remains common in the U.S. Scientific advancements continue to rely on Kelvin for absolute temperature measurements.
Understanding Fahrenheit, Celsius, and Kelvin is essential in various fields. Each scale has unique benefits, and knowing how to convert between them helps in global communication and scientific research.