Convert Delisle to Fahrenheit easily.
212 - (1 °De x 2÷3) = 211.333 °F
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Ever stumbled up on temperature measurements in Delisle while reading historical documents or old scientific papers? Don't worry if it looks backwards to what you're used to. This peculiar scale has a fascinating story, and converting it to Fahrenheit isn't as complicated as you might think. Whether you're a history buff decoding 18th-century weather records or just curious about obscure measurement systems, we've got you covered.
Unit definitions
What is a Delisle (°De)?
The Delisle scale is one of those old temperature measurements that went against the grain. Created by French astronomer Joseph-Nicolas Delisle in 1732, it flips our modern expectations. Water boils at 0°De and freezes at 150°De, making it decrease as temperature increases. Back in its heyday, it was actually quite popular in Russia for meteorological observations.
Symbol: °De
Common uses: Historical scientific records, 18th-century Russian weather data
Definition: Based on mercury thermometers with water's boiling point as zero
What is a Fahrenheit (°F)?
Most Americans know this one by heart. Developed by Daniel Fahrenheit in 1724, it's that quirky scale where water freezes at 32°F and boils at 212°F. While much of the world has switched to Celsius, Fahrenheit remains the go-to for weather reports and ovens in the United States.
Symbol: °F
Common uses: US weather forecasts, cooking temperatures, medical measurements
Definition: Originally based on brine solutions and human body temperature
Conversion formula
The mathematical relationship between these two scales reflects their contrasting philosophies. To convert Delisle to Fahrenheit:
Fahrenheit = 212 - (Delisle × 2/3)
This formula essentially reverses the Delisle scale's downward progression while adjusting its magnitude to match Fahrenheit's range.
Example calculations
Let's walk through two practical examples:
- Converting 100°De to Fahrenheit:
212 - (100 × 2/3) = 212 - 66.666... ≈ 145.33°F
That's hotter than your average sauna session! - Converting 30°De to Fahrenheit:
212 - (30 × 2/3) = 212 - 20 = 192°F
Almost at the boiling point of water under standard pressure.
Conversion tables
Delisle to Fahrenheit
Delisle (°De) | Fahrenheit (°F) |
---|---|
0 | 212.00 |
50 | 178.67 |
100 | 145.33 |
150 | 112.00 |
200 | 78.67 |
250 | 45.33 |
300 | 12.00 |
Fahrenheit to Delisle
Fahrenheit (°F) | Delisle (°De) |
---|---|
212 | 0.00 |
150 | 93.00 |
100 | 168.00 |
32 | 270.00 |
0 | 318.00 |
-40 | 378.00 |
From Russia with cold: The Delisle scale's journey
Joseph-Nicolas Delisle didn't set out to confuse future generations. His scale made perfect sense in the context of early thermometry. When he took up residence at the Saint Petersburg Academy of Sciences in 1732, Russia needed a reliable temperature measurement system for its brutal winters. The Delisle scale, with its mercury-based thermometers and large gradations, became the official standard for Russian meteorological observations for nearly a century.
Funny thing is, Delisle originally set water's boiling point at 0°De and calibration marks decreased as temperatures droped. This seemed logical when working with contraction of mercury, but later scales like Celsius (1742) flipped this orientation. By the time Fahrenheit's scale gained international traction, Delisle's creation was already becoming a historical footnote.
Interesting facts
- The Delisle scale holds the record for the coldest "zero point" among temperature scales, starting at boiling rather than freezing
- Some surviving 18th-century Russian thermometers show both Delisle and Réaumur scales for dual readability
- At -20°F, the Delisle equivalent would be 348°De – numbers that feel more dramatic than the actual cold
- Delisle's student Mikhail Lomonosov later improved upon his mentor's work, contributing to Russia's scientific revolution
- The scale's 150-degree freezing point was chosen for its divisibility by 2, 3, 5, 6, 10, 15, 25, 30, 50, and 75
FAQ
The Delisle scale was designed with 0°De as boiling point and 150°De as freezing point, making it decrease as temperature rises. This was based on early thermometric observations.
The mathematical relationship is precise, but since the Delisle scale isn't used in modern measurements, practical accuracy depends on your initial data quality.
Mainly historical research or interpreting old scientific records. Some Russian weather archives from the 1700s still contain Delisle measurements.
Absolutely. The reverse formula is Delisle = (212 - Fahrenheit) × 1.5. Though you'll rarely need this outside academic contexts.
Russia used it extensively during the 18th century. Delisle himself worked at teh Saint Petersburg Academy of Sciences, which helped popularize his scale there.