-40°
Celsius and Fahrenheit give the same number at minus forty.
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Photo: Anonimski · CC BY-SA 3.0
The short answer
Minus forty degrees Celsius is the same temperature as minus forty degrees Fahrenheit. It is the single temperature at which these two scales display the same numerical value.
Why it's true
The conversion from Celsius to Fahrenheit is F = 9C/5 + 32. The multiplier accounts for the different sizes of the degrees, and the added 32 accounts for the different zero points. Both pieces are necessary when converting an actual temperature reading.
To find the shared reading, set F equal to C. Then C = 9C/5 + 32, so subtracting C gives 0 = 4C/5 + 32. Rearranging produces C = -40, and substitution into the original equation gives F = -40 as well.
Matching numbers do not mean the scales become identical. A Celsius degree remains 1.8 times the size of a Fahrenheit degree even at the crossing point. Moving one Celsius degree upward from the shared temperature changes the Fahrenheit reading by 1.8 degrees, so the numbers immediately separate.
By the numbers
−40°C
Shared temperature
−40°F
Same temperature in Fahrenheit
1.8
Fahrenheit degrees per Celsius degree
The backstory
The familiar water reference points make the conversion easy to understand. At standard atmospheric pressure, water freezes at 0°C or 32°F and boils at approximately 100°C or 212°F. The Celsius interval between those points contains 100 degrees, while the Fahrenheit interval contains 180. Dividing 180 by 100 gives the scale factor 1.8, or nine fifths.
These reference points explain the relationship but should not be mistaken for a guarantee that water always boils at 100°C. Boiling temperature depends on pressure, and dissolved substances can change freezing and boiling behavior. Modern temperature measurement rests on formal unit definitions and calibrated instruments, rather than assuming every sample of water provides an exact fixed point under any conditions.
On a graph with Celsius on one axis and Fahrenheit on the other, the conversion is a straight line. Equal numerical readings lie on a second line described by F = C. Because the conversion line has a slope of 1.8 rather than one, the two lines intersect only once. Their intersection represents the minus-forty match, not a broad region where the scales can be used interchangeably.
The wider picture
Temperature intervals need different treatment from temperature readings. A rise of 10 Celsius degrees corresponds to a rise of 18 Fahrenheit degrees, with no added 32. The offset cancels when subtracting one temperature from another. Confusing an interval with a reading is a common reason for incorrect conversions in weather, recipes, and laboratory calculations.
Kelvin provides another useful comparison. Celsius and kelvin use equally sized increments but have different zero points: kelvin temperature equals Celsius temperature plus 273.15. The shared Celsius-Fahrenheit temperature is therefore 233.15 K, not absolute zero. A negative reading on either everyday scale indicates a position below that scale's zero, not a negative amount of thermal energy.
Worth remembering
- The Celsius and Fahrenheit readings agree only at minus forty; the equality concerns their numbers, not their degree sizes.
- Use F = 9C/5 + 32 for a temperature reading, but multiply by 1.8 without the offset for a temperature interval.
- Minus forty on these scales is 233.15 kelvin, so the shared value has no special connection to absolute zero.
In context
The matching reading is a property of two scale labels, not an unusual state of matter. At that temperature, objects still behave according to their composition and conditions. Nothing special happens to water, metal or air merely because the Celsius and Fahrenheit numbers coincide.
A closer look
A crossing of two straight lines
The conversion combines a scale factor with an offset. Finding a matching numerical reading means solving for where the converted value equals the original value. Because the scales have different interval sizes, their straight-line relationship has only one such crossing. This algebra explains the coincidence without invoking a physical transition or a special thermometer.
Readings and changes need different rules
Converting an absolute reading requires the offset; converting a temperature difference does not. A rise on one scale represents a rise on the other, but it is not calculated by adding the freezing-point offset to the change. Confusing these tasks can produce incorrect weather comparisons, laboratory reports and engineering calculations even when the conversion formula is remembered correctly.
Related facts
Absolute zero distinguishes a physical temperature limit from a coincidental scale crossing. Absolute zero is exactly -273.15 degrees Celsius.
Gallium’s melting point is a material property rather than a matching thermometer label. Gallium can melt at a temperature below normal human body temperature.
Thermal expansion depends on temperature changes, making interval conversion relevant. The Eiffel Tower grows about 15 centimeters taller in summer.
The logarithmic pH scale contrasts with linear temperature conversions. One pH unit represents a tenfold change in hydrogen-ion activity.
Key terms
- Offset
- A fixed additive difference between the origins of two related scales.
- Temperature interval
- A change or difference in temperature rather than an absolute scale reading.
People also ask
Is minus forty a phase transition?
Not because the scale readings agree. Any phase transition depends on the substance and pressure, not this numerical coincidence.
Are Celsius and Fahrenheit degrees equally large?
No. Their interval sizes differ, which is why a conversion needs a multiplier as well as an offset.
Does the same offset apply to a temperature rise?
No. Temperature differences use the scale factor without the offset used for absolute readings.
Could the scales match at another temperature?
Not under their standard linear relationship. The equality equation has a single solution.
Does this make Celsius and kelvin match too?
No. Celsius and kelvin share an interval size but have different origins, so their numerical readings retain a constant difference.