Temperature
Temperature is a measure of how hot or cold an object is. On a microscopic level, it is related to the average kinetic energy of the particles in a substance. When two objects are at the same temperature, there is no net energy transfer between them — they are in thermal equilibrium.
Temperature is not the same as heat. Heat is energy transferred due to a temperature difference. Temperature is a measure of the average kinetic energy of particles. A spark at 1000 °C has a very high temperature but very little internal energy (few particles); a bath of water at 40 °C has much more internal energy despite a lower temperature.
The Kelvin Scale
The absolute temperature scale (kelvin, K) is the SI unit of temperature. It starts at absolute zero (0 K), the lowest possible temperature at which particles have minimum kinetic energy.
A change of 1 K is exactly equal to a change of 1 °C — the scales have the same interval size, just different starting points. At absolute zero (0 K = −273 °C), the particles in a substance have their minimum possible kinetic energy (but not zero — quantum zero-point energy remains).
Never write "degrees kelvin" or use the ° symbol with kelvin. Write 300 K, not 300 °K. Similarly, when using temperature differences in equations, $\Delta\theta$ in °C is numerically equal to $\Delta T$ in K — so you can use either.
Thermal Equilibrium
When two objects are placed in contact, energy transfers from the hotter object to the cooler one until they reach the same temperature. At this point they are in thermal equilibrium — no net energy transfer occurs.
This principle underpins the zeroth law of thermodynamics: if A is in thermal equilibrium with B, and B is in thermal equilibrium with C, then A is in thermal equilibrium with C. This is why thermometers work — the thermometer reaches thermal equilibrium with the object being measured.