IB Physics SL Topic B.1 — Heat & Thermal Transfer Paper 1 & 2 Measuring Temperature ~6 min read

Measuring Temperature

Celsius is what you’ll see on a weather app, but physics runs on a different scale entirely — one that starts at the coldest temperature the universe can possibly reach, and never dips below it.

📘 What you need to know

Absolute Zero and the Kelvin Scale

On the thermodynamic, or Kelvin, scale, absolute zero is the coldest temperature that can possibly exist. Since molecules at absolute zero have no kinetic energy left to lose, it’s simply not possible to cool a system any further once it gets there — there’s no more energy left to remove.

Even the depths of space aren’t quite at absolute zero — the background temperature of the universe sits at around 2.7 K, just a few degrees above it.

Converting Between Celsius and Kelvin

Kelvin to Celsius θ⁄°C = T⁄K − 273
Celsius to Kelvin T⁄K = θ⁄°C + 273
0 K −273 °C Absolute zero 273 K 0 °C Ice melts 300 K 27 °C A warm day
Kelvin and Celsius share the same size of division — only the zero point is shifted by 273
Quick recap: T/K = θ/°C + 273. Kelvin never goes negative, and a 1 K change always matches a 1 °C change.
WE 1

Average human body temperature is 37 °C. Express this temperature in kelvin.

Step 1 — Recall the conversion T/K = θ/°C + 273 Step 2 — Substitute T = 37 + 273 = 310 K
WE 2

A cold-storage sensor reads 194 K. Convert this to degrees Celsius, and comment on what this temperature is close to in everyday terms.

Step 1 — Recall the conversion θ/°C = T/K − 273 Step 2 — Substitute θ = 194 − 273 = −79 °C This is close to the sublimation temperature of solid carbon dioxide (dry ice), around −78.5 °C.

💡 Top tips

⚠ Common mistakes

Up next: Temperature & Kinetic Energy — where we connect this temperature scale to the actual motion of particles.

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