Education

Learn °G

The fastest way to learn a temperature scale is to attach numbers to experiences you already know.

Anchor points

Start with a handful of numbers.

These are illustrative reference points, not extra definitions of the scale. The formal definition for numerical readings is TG = 2TC.

0°G
0 °C · 32 °F

Water's familiar freezing reference.

40°G
20 °C · 68 °F

A common room-temperature reference.

50°G
25 °C · 77 °F

A pleasantly warm day for many people.

60°G
30 °C · 86 °F

Hot-weather territory.

74°G
37 °C · 98.6 °F

The familiar nominal human body-temperature reference.

100°G
50 °C · 122 °F

Extreme outdoor heat.

Count the steps

One physical range, three ways to number it.

From freezing to 40 °C / 104 °F / 80 °G, nothing physical changes. Only the scale markings do.

Celsius40whole-degree intervals
Fahrenheit72whole-degree intervals

Remember: more whole-number intervals means finer numbering, not more physical information. Measurement precision still depends on the instrument.

Four-season intuition

Weather in Galliera.

These broad bands are illustrative for temperate four-season climates. They intentionally overlap; seasons are not discrete temperature bins.

Winter · −10 to 30 °G

−5 to 15 °C · 23 to 59 °F

−20040100 °G

Spring / Autumn · 10 to 50 °G

5 to 25 °C · 41 to 77 °F

−20040100 °G

Summer · 40 to 90 °G

20 to 45 °C · 68 to 113 °F

−20040100 °G

Latitude, elevation, humidity, continentality and local climate can shift these ranges substantially.

Thermostats

Count by ones instead of halves.

This is the everyday interface argument in its simplest form.

4020.0°C
4120.5°C
4221.0°C
4321.5°C
4422.0°C
4522.5°C
Practice

Think in °G.

A few quick exercises make the factor-of-two relationship automatic.

20 °C = ? °G
40 °G
43 °G = ? °C
21.5 °C
30 °C = ? °G
60 °G