This page builds every symbol the parent note leans on, starting from a reader who has never seen a single one. Each entry gives you three things: plain meaning → the picture → why the topic needs it. Read top to bottom; each rung of the ladder rests on the one below it.
Picture a jar of tiny balls (atoms) that never stop trembling. In a cold jar they barely quiver; in a hot jar they shake violently.
Plain meaning:T measures average jiggle energy per atom.
The picture: left jar = slow, small arrows; right jar = fast, big arrows.
Why the topic needs it: every single formula here is driven by a temperature difference. Without T there is no "hot" and "cold", and heat has no direction to flow.
The picture: one vertical thermometer with two rulers glued side by side; the tick marks line up but the zero of each is in a different place. The spacing between ticks is identical.
Why the topic needs it — the crucial subtlety: because the ticks are the same size, a difference is the same on both scales:
ΔT=20∘C−0∘C=20 K.
But a single value is not: 20∘C=293.15 K, not 20 K.
Recall When may I leave a temperature in Celsius?
Only when it appears as a differenceΔT (as in Fourier's law). Any single value or any power of T (like T4 in radiation) must be in kelvin. ::: Differences OK in °C; single values and powers must be K.
Why this tool and not just "Q"? A wall doesn't care about total joules — it cares about flow speed. Asking "how many joules per second?" is exactly what a rate answers, and the physics symbol for "per second, instant by instant" is the derivative dtd(⋅).
The picture: water leaving a tap. Q is the total litres in the bucket; dtdQ is how fast the stream is running right now.
This rate has a name in this topic: the heat currentH.
The picture: a wall drawn as a ramp of temperature — hot face high on the left, cold face low on the right. The slope of that ramp isdxdT. A steep ramp = big gradient = strong push for heat.
Why the sign is negative: as you walk in the +x direction (into the cold), T goes down, so dxdT is a negative number. Heat flows the opposite way — toward +x — which is why Fourier's law carries a − to keep H positive.
Why the topic needs it: conduction is driven by steepness of the drop, not by the raw temperatures. The gradient is that steepness.
The picture: a slab (a brick). A = the flat front you'd paint; Δx = how deep the brick goes front-to-back.
Why the topic needs both: a wider face (A) lets more heat through in parallel; a deeper brick (Δx) makes heat travel further, slowing it. These are the two geometry knobs in Fourier's law.
The picture: four curves T, T2, T3, T4 climbing out of the origin — T4 rockets up far above the others. That steepness is why a small rise in temperature causes a huge jump in radiated power.
Why the topic needs it: radiation obeys P∝T4, so it becomes the dominant loss channel at high temperature (a filament, the Sun) even though it's tiny at room temperature.
Why the topic borrows this: you already know series/parallel resistor rules; reusing them for composite walls saves inventing new maths. Heat "flowing downhill" from high ΔT is exactly current flowing from high voltage.