Delisle to Fahrenheit Converter

Convert degrees Delisle to degrees Fahrenheit with our free online temperature converter.

Quick Answer

1 Delisle = 210.8 degrees Fahrenheit

Formula: Delisle × conversion factor = Fahrenheit

Use the calculator below for instant, accurate conversions.

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All conversion formulas on UnitsConverter.io have been verified against NIST (National Institute of Standards and Technology) guidelines and international SI standards. Our calculations are accurate to 10 decimal places for standard conversions and use arbitrary precision arithmetic for astronomical units.

Last verified: February 2026Reviewed by: Sam Mathew, Software Engineer

Delisle to Fahrenheit Calculator

How to Use the Delisle to Fahrenheit Calculator:

  1. Enter the value you want to convert in the 'From' field (Delisle).
  2. The converted value in Fahrenheit will appear automatically in the 'To' field.
  3. Use the dropdown menus to select different units within the Temperature category.
  4. Click the swap button (⇌) to reverse the conversion direction.
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How to Convert Delisle to Fahrenheit: Step-by-Step Guide

Temperature conversions like Delisle to Fahrenheit use specific non-linear formulas.

Formula:

First convert °De to °C: °C = 100 - °De × 2/3. Then convert °C to °F: °F = (°C × 9/5) + 32

Example Calculation:

Convert 10°De:
1. °C = 100 - (10 × 2/3) = 93.33°C
2. °F = (93.33 × 9/5) + 32 = 200.0°F

Disclaimer: For Reference Only

These conversion results are provided for informational purposes only. While we strive for accuracy, we make no guarantees regarding the precision of these results, especially for conversions involving extremely large or small numbers which may be subject to the inherent limitations of standard computer floating-point arithmetic.

Not for professional use. Results should be verified before use in any critical application. View our Terms of Service for more information.

What is a Delisle and a Fahrenheit?

The Delisle scale (symbol: °De or °D) is an inverted temperature scale that divides the interval between the boiling point and freezing point of water into 150 equal divisions under standard atmospheric pressure, with numerical values decreasing as temperature increases.

Scale Calibration (Inverted)

Fixed Points:

  • Boiling point of water: 0 degrees Delisle (0°De) - the ZERO reference
  • Freezing point of water: 150 degrees Delisle (150°De) - 150° higher than boiling
  • Degree size: Each Delisle degree = 2/3 Celsius degree (or 0.667°C)

The Inversion: Unlike Celsius, Fahrenheit, Réaumur, and Kelvin, which all increase with temperature:

  • Hotter temperatures = LOWER Delisle numbers (approaching 0°De)
  • Colder temperatures = HIGHER Delisle numbers (above 150°De)
  • Temperature increases = Delisle decreases

Mathematical Relationships

Delisle to Celsius:

  • °C = 100 - (°De × 2/3)
  • Or: °C = 100 - (°De ÷ 1.5)

Celsius to Delisle:

  • °De = (100 - °C) × 3/2
  • Or: °De = (100 - °C) × 1.5

Delisle to Fahrenheit:

  • °F = 212 - (°De × 6/5)
  • Or: °F = 212 - (°De × 1.2)

Examples:

  • 0°De = 100°C (boiling water)
  • 75°De = 50°C (halfway between boiling and freezing)
  • 150°De = 0°C (freezing water)
  • 300°De = -100°C (extreme cold, -148°F)

Why 150 Degrees?

Delisle chose 150 degrees for the freezing point due to:

  1. Mercury contraction observation: His mercury thermometers showed 150 units of contraction between boiling and freezing
  2. Divisibility: 150 = 2 × 3 × 5², offering factors (2, 3, 5, 6, 10, 15, 25, 30, 50, 75, 150)
  3. Convenient fractional divisions: 150/3 = 50°, 150/2 = 75°, 150/10 = 15° for practical measurements
  4. Empirical basis: Based on actual instrument behavior rather than abstract decimal preference

Why Invert the Scale?

Delisle's inversion was methodological rather than arbitrary:

Calibration Process:

  • Started with boiling water (100°C) as reference point zero
  • Observed mercury column contraction as water cooled
  • Counted degrees of contraction downward from boiling
  • At freezing point (0°C), mercury had contracted 150 divisions

Result: A scale that measured "degrees of cooling" from boiling, making hotter temperatures numerically smaller. While counterintuitive by modern standards, it reflected the experimental process.

Degree Fahrenheit (symbol: °F) is a unit of temperature on the Fahrenheit scale, developed by physicist Daniel Gabriel Fahrenheit in 1724. It is one of the most commonly used temperature scales in the United States.

Key reference points:

  • Water freezing point: 32°F (at standard atmospheric pressure)
  • Water boiling point: 212°F (at standard atmospheric pressure)
  • Degree span: 180°F between freezing and boiling (212 - 32 = 180)
  • Absolute zero: -459.67°F (theoretical lowest temperature)

Conversion formulas:

Common temperature ranges:

  • Below 0°F: Extremely cold
  • 0-32°F: Very cold (below freezing)
  • 32-50°F: Cold
  • 50-65°F: Cool
  • 65-75°F: Comfortable/room temperature
  • 75-85°F: Warm
  • 85-95°F: Hot
  • Above 95°F: Very hot

Note: The degree symbol (°) is always used with Fahrenheit. Write "32°F" not "32F" or "32 degrees F."

Convert between temperature units: Fahrenheit converter

Note: The Delisle is part of the imperial/US customary system, primarily used in the US, UK, and Canada for everyday measurements. The Fahrenheit belongs to the imperial/US customary system.

History of the Delisle and Fahrenheit

The Delisle scale's 290-year history is inseparable from the development of Russian science and the Imperial Academy's early years.

Joseph-Nicolas Delisle (1688-1768)

Born in Paris to artistic parents, Delisle became one of France's leading astronomers, specializing in celestial mechanics and cartography. His work on planetary transits and lunar theory earned him election to the French Academy of Sciences (1714) and international recognition.

1725: Invitation to Russia

Tsar Peter the Great, determined to modernize Russia through Western science, invited Delisle to St. Petersburg to establish an astronomical observatory and help found the Imperial Russian Academy of Sciences. Delisle arrived in St. Petersburg in August 1725, months after Peter's death, but Empress Catherine I honored the invitation.

1725-1747: Russian Academy Directorship

As the Academy's first director of astronomy, Delisle:

  • Established St. Petersburg Observatory (1726)
  • Trained Russian astronomers and instrument makers
  • Standardized scientific measurements across the Russian Empire
  • Corresponded with European scientific societies

Creation of the Delisle Scale (1732)

The Problem: Russia's vast territory and extreme climate variations required standardized temperature measurements for meteorology, agriculture, and scientific research. Existing thermometers used inconsistent scales, making comparison impossible.

Delisle's Solution (1732):

  1. Boiling water reference: Started with boiling point as 0° (easiest to reproduce reliably)
  2. Mercury contraction: Observed mercury column shrinking as temperature decreased
  3. Freezing point calibration: Marked freezing water at 150° of contraction
  4. Uniform divisions: Divided the interval into 150 equal degrees

1732 Paper: Delisle presented his scale to the Imperial Russian Academy, arguing that starting from boiling point provided greater calibration accuracy than starting from freezing (where ice-water mixtures could vary slightly).

Official Adoption in Russia (1738-1840s)

1738: Imperial Decree

The Russian Imperial government officially adopted the Delisle scale for all government and scientific purposes, making Russia the first nation to standardize on a single temperature scale nationwide.

Implementation:

  • Meteorological stations: All Russian weather observation posts used Delisle thermometers
  • Scientific research: Academy publications reported temperatures in Delisle
  • Military applications: Army and Navy used Delisle for weather reporting
  • Educational institutions: Russian universities taught Delisle as standard

Geographic Spread: The scale's use extended across the Russian Empire:

  • St. Petersburg and Moscow (primary centers)
  • Baltic provinces (Estonia, Latvia, Lithuania)
  • Siberian outposts and exploration expeditions
  • Crimea and southern territories

Coexistence with Réaumur (1780s-1840s)

By the late 18th century, Western European science had largely standardized on Réaumur (continental Europe) or Fahrenheit (Britain), creating communication challenges for Russian scientists.

1780s-1820s: Gradual Transition

Russian instrument makers began producing dual-scale thermometers (Delisle/Réaumur) to facilitate:

  • International scientific correspondence
  • Translation of Western European research
  • Trade with European partners

1840s: Réaumur Dominance

By the 1840s, Réaumur had effectively replaced Delisle in Russian scientific practice:

  • Younger Russian scientists trained with Réaumur
  • International standardization pressure increased
  • French scientific influence (Réaumur) outweighed earlier German connections

Final Decline (1850-1917)

1850-1870: Delisle relegated to historical archives, antique thermometers, and elderly scientists' habit 1871: German unification's adoption of Celsius influenced Russian scientific circles 1900-1917: Celsius gaining ground in Russian universities and research institutions 1917-1925: Bolshevik Revolution brought metric system adoption, officially ending Delisle use

Legacy and Modern Recognition

The Delisle scale survives as:

  • Historical curiosity: The only inverted scale to achieve governmental adoption
  • Archival research: Russian meteorological data (1738-1840s) requires Delisle conversion
  • Thermometer collecting: Delisle/Réaumur dual-scale antique thermometers from Russia
  • Scientific history: Example of how methodology (cooling observation) shaped measurement design
  • Daniel Gabriel Fahrenheit (1686-1736): A Polish-German physicist and instrument maker who invented the mercury thermometer and developed the Fahrenheit temperature scale.

  • Early Development (1724): Fahrenheit proposed his temperature scale with three reference points:

    • 0°F: Temperature of a brine solution (mixture of ice, water, and ammonium chloride salt) - the coldest temperature he could reliably reproduce in his laboratory
    • 32°F: Freezing point of water (later standardized)
    • 96°F: Human body temperature (later adjusted to 98.6°F)
  • Original Rationale: Fahrenheit chose these points to:

    • Avoid negative numbers in normal weather (unlike earlier scales)
    • Create finer graduations for better precision (180 degrees between freezing and boiling vs 100 in Celsius)
    • Use easily reproducible reference points with 18th-century technology
  • Refinements (1750s onward): The scale was gradually standardized:

    • Water's freezing point: exactly 32°F
    • Water's boiling point: exactly 212°F (at standard atmospheric pressure)
    • This created 180 degrees between the two points
    • Human body temperature was remeasured at 98.6°F (not 96°F)
  • Rapid Adoption (1700s-1800s): The Fahrenheit scale quickly became popular:

    • Adopted throughout the British Empire
    • Standard in English-speaking countries
    • Used in scientific work until the late 19th century
    • Mercury thermometers using Fahrenheit became widespread
  • Celsius Competition (1742): Anders Celsius proposed the centigrade scale (later renamed Celsius) with 0° at water freezing and 100° at boiling. Simpler, but both scales coexisted.

  • Metric Movement (1900s): As the metric system spread globally:

    • Most countries switched from Fahrenheit to Celsius
    • Scientific community adopted Celsius/Kelvin
    • UK officially switched to Celsius in the 1960s-1970s
    • Canada switched to Celsius in the 1970s
  • United States Today: The US remains the only major country using Fahrenheit for everyday temperatures:

    • Weather forecasts in °F
    • Thermostats and home heating/cooling in °F
    • Cooking temperatures in °F
    • Medical thermometers in °F (though hospitals also use Celsius)
    • Scientific and medical research uses Celsius/Kelvin
  • Why the US Kept Fahrenheit:

    • Deeply ingrained in culture and infrastructure
    • Costly to replace all thermostats, ovens, signs
    • Public resistance to metric conversion
    • Fahrenheit provides finer resolution for weather (1°F = 0.56°C)
  • Global Usage Today:

    • Primary users: United States, some Caribbean nations (Bahamas, Belize, Cayman Islands), Palau, Federated States of Micronesia, Marshall Islands
    • Former users: UK, Canada, Australia (all switched to Celsius)
    • Rest of world: Uses Celsius exclusively
  • Cultural Impact: Fahrenheit remains a distinctive American characteristic, like miles and pounds, symbolizing resistance to metric adoption.

Historical Anecdote: The Case of the Missing 2.6 Degrees

Why did the body temperature change from Fahrenheit's original 96°F to the modern 98.6°F?

  1. Measurement Error: Early 18th-century thermometers were not yet standardized.
  2. The Brine Mystery: Fahrenheit used the freezing point of brine for 0°F, but the concentration of ammonium chloride and ice varies.
  3. Wunderlich's Research: In 1851, German physician Carl Reinhold August Wunderlich measured the temperatures of 25,000 patients and established the "new" average of 37°C, which was converted to 98.6°F.

Fahrenheit in Science Fiction: The Branding of Heat

The Fahrenheit scale has entered popular culture as a symbol of intense heat. Ray Bradbury's novel Fahrenheit 451 refers to the temperature at which book paper catches fire and burns. While scientists argue that the actual ignition temperature of paper varies with the type of paper and the oxygen levels, "451°F" has become an iconic cultural reference for censorship and destruction.

Common Uses and Applications: degrees Delisle vs degrees Fahrenheit

Explore the typical applications for both Delisle (imperial/US) and Fahrenheit (imperial/US) to understand their common contexts.

Common Uses for degrees Delisle

Historical Russian Meteorology (1738-1840s)

The primary application of the Delisle scale was Russian weather observation:

Imperial Meteorological Network:

  • St. Petersburg Observatory: Daily temperatures recorded in Delisle
  • Moscow weather stations: Imperial Academy network standardized on Delisle
  • Siberian frontier posts: Military expeditions reported temperatures in Delisle
  • Black Sea and Baltic ports: Naval meteorological data in Delisle

Record Keeping: Archives from this period contain:

  • Handwritten logbooks with Delisle readings
  • Published annual weather summaries
  • Agricultural yield correlations with Delisle temperatures
  • Military campaign weather reports (e.g., Napoleon's 1812 invasion)

18th-Century Russian Scientific Research

Russian Academy scientists used Delisle for:

Physics Experiments:

  • Thermal expansion studies
  • Phase transition research (freezing, melting, boiling)
  • Instrument calibration standards

Biological Research:

  • Plant growth temperature requirements
  • Animal physiology studies
  • Seed germination experiments

Astronomical Observations:

  • Observatory temperature logs (affecting telescope precision)
  • Atmospheric refraction corrections based on temperature

Historical Document Interpretation

Modern researchers encounter Delisle in:

Russian Imperial Archives:

  • Government reports (1738-1840s)
  • Military campaign records
  • Agricultural survey data
  • Medical records from Russian hospitals

Scientific Publications:

  • Imperial Russian Academy journals
  • European scientific correspondence with Russian researchers
  • Exploration expedition reports (Bering, Kamchatka expeditions)

Literature and Personal Correspondence:

  • Letters between Russian aristocracy
  • Travel journals of European visitors to Russia
  • Historical novels set in 18th-19th century Russia

Antique Thermometer Collecting

Delisle thermometers are rare and valuable collectibles:

Rarity Factors:

  • Limited production period: 1732-1850s primarily
  • Geographic concentration: Almost exclusively Russian Empire
  • Destruction: Many lost during Russian Revolution, World Wars
  • Dual-scale models: Delisle/Réaumur thermometers from 1780s-1840s most sought

Market Value:

  • Original Delisle thermometers: $1,000-$10,000+ (extreme rarity)
  • Dual-scale Delisle/Réaumur: $800-$5,000 (more common)
  • Reproductions/modern curiosities: $50-$200

Education and Science Museums

Science museums use Delisle thermometers to teach:

  • History of measurement: Evolution of temperature scales
  • Scientific methodology: How observation shapes measurement design
  • Cultural context: Russian Empire's scientific development
  • Inverted scales: Challenging students' assumptions about "hotter = higher number"

Online Temperature Converters

Delisle appears in comprehensive temperature conversion tools:

  • Historical conversion calculators for archival research
  • "Exotic scales" demonstrations alongside Rømer, Newton scales
  • Educational tools teaching temperature scale diversity

When to Use degrees Fahrenheit

Fahrenheit is the standard temperature scale for daily life in the United States:

Weather Reporting

Primary temperature scale for weather forecasts and reporting in the United States and its territories.

Weather applications:

  • Daily temperature forecasts (high/low)
  • Current temperature readings
  • Heat index calculations
  • Wind chill factor
  • Severe weather alerts (heat advisories, freeze warnings)
  • Historical climate data
  • Weather maps and graphics

Why Fahrenheit in weather:

  • Finer resolution (1°F increments vs 1°C)
  • Human comfort range (0-100°F covers most livable temps)
  • Cultural familiarity in the US
  • All infrastructure uses Fahrenheit

Convert for international weather: Fahrenheit to Celsius


Home Heating and Cooling

Standard for thermostats, HVAC systems, and climate control in American homes and buildings.

HVAC uses:

  • Thermostat settings (heat/cool)
  • Programmable temperature schedules
  • Smart home temperature control
  • Zone heating/cooling
  • Energy efficiency monitoring
  • Comfort optimization

Typical settings:

  • Winter: 68-70°F daytime, 65°F night
  • Summer: 75-78°F when home, 82-85°F when away
  • Energy saving: Adjust 7-10°F from comfort level when absent

Cooking and Food Preparation

Universal standard for oven temperatures, cooking instructions, and food safety in American kitchens.

Cooking applications:

  • Oven temperature settings
  • Recipe instructions
  • Meat thermometer readings
  • Food safety guidelines
  • Candy/deep-fry thermometers
  • Sous vide cooking

Why Fahrenheit in cooking:

  • All US recipes use °F
  • All ovens manufactured for US in °F
  • Food safety standards in °F
  • Cookbooks and packaging use °F

Medical Temperature

Standard for body temperature measurement in US healthcare and home use.

Medical uses:

  • Fever detection and monitoring
  • Patient vital signs
  • Hypothermia/hyperthermia diagnosis
  • Pediatric care (baby temperature)
  • Home health monitoring
  • Medical charts and records

Key thresholds:

  • Normal: 98.6°F (97-99°F range)
  • Fever: Above 100.4°F
  • High fever: Above 103°F
  • Hypothermia: Below 95°F

Note: US hospitals often use both Fahrenheit and Celsius for international standardization.


Swimming Pools and Spas

Standard for pool heating, hot tubs, and aquatic facilities in the US.

Pool/spa uses:

  • Pool heater settings
  • Spa/hot tub temperature
  • Chemical effectiveness (temperature-dependent)
  • Comfort optimization
  • Energy cost management

Standard temperatures:

  • Swimming pool: 78-82°F
  • Competitive swimming: 77-82°F
  • Hot tub: 100-104°F (max 104°F)
  • Therapy pool: 92-98°F

Automotive

Used for engine monitoring and climate control in US vehicles.

Automotive uses:

  • Engine temperature gauge
  • Coolant temperature warning
  • Cabin climate control
  • Outside temperature display
  • Oil temperature monitoring

Everyday Decisions

Influences daily choices in clothing, activities, and comfort throughout the US.

Daily decisions based on temperature:

  • What to wear (shorts vs jacket)
  • Indoor/outdoor activities
  • Exercise safety
  • Pet care (walk dog or not)
  • Home comfort adjustments

Use our Fahrenheit converter for everyday conversions.

Additional Unit Information

About Delisle (°De)

What are the freezing and boiling points of water in Delisle?

Water boils at 0°De and freezes at 150°De. This is inverted compared to all other major temperature scales (Celsius, Fahrenheit, Réaumur, Kelvin), where higher numbers indicate hotter temperatures.

Why does the Delisle scale decrease with increasing temperature?

Delisle's methodology determined the scale's direction:

  1. Calibration process: He started with boiling water (100°C) as his zero reference point
  2. Cooling observation: He watched mercury contract as water cooled from boiling
  3. Counting contraction: Each unit of contraction represented one Delisle degree
  4. Result: At freezing point, the mercury had contracted 150 divisions from boiling

The scale thus measured "degrees of cooling" from boiling water, making hotter temperatures numerically smaller. While counterintuitive, it reflected his experimental procedure.

How does Delisle relate to Celsius?

Conversion formulas:

  • Delisle → Celsius: °C = 100 - (°De × 2/3)
  • Celsius → Delisle: °De = (100 - °C) × 1.5

Relationship: Each Delisle degree = 2/3 Celsius degree (0.667°C), but running in opposite direction.

Example:

  • 0°De = 100°C (boiling)
  • 150°De = 0°C (freezing)
  • 75°De = 50°C (midpoint)

The "100 -" in the formula accounts for the inversion.

Was the Delisle scale ever widely used?

Yes, in Imperial Russia (1738-1840s):

The Delisle scale was the official temperature standard of the Russian Empire for approximately one century. It was mandatory for:

  • All government meteorological stations
  • Imperial Russian Academy scientific research
  • Military weather reporting
  • Educational institutions

Not widely used elsewhere: Aside from Russia, Delisle remained a curiosity. Western Europe used Réaumur or Fahrenheit; Delisle was essentially a Russian phenomenon.

Why didn't other countries adopt the Delisle scale?

Several factors limited adoption:

  1. Counterintuitive: The inversion (hotter = lower number) confused users
  2. Late arrival: By 1732, Fahrenheit (1714) and Réaumur (1730) were established
  3. Geographic isolation: Russia's distance from Western European scientific centers
  4. Communication barriers: Language and political isolation limited dissemination
  5. No compelling advantage: The inversion offered no practical benefit over conventional scales

The scale succeeded in Russia due to Delisle's position at the Imperial Academy and government decree, not scientific merit.

How do you convert a Delisle temperature to Fahrenheit?

Two-step method:

  1. Convert Delisle to Celsius: °C = 100 - (°De × 2/3)
  2. Convert Celsius to Fahrenheit: °F = (°C × 9/5) + 32

Direct formula: °F = 212 - (°De × 6/5) or °F = 212 - (°De × 1.2)

Example: 120°De (Russian "room temperature")

  • Step 1: °C = 100 - (120 × 2/3) = 100 - 80 = 20°C
  • Step 2: °F = (20 × 1.8) + 32 = 36 + 32 = 68°F

Direct: 212 - (120 × 1.2) = 212 - 144 = 68°F ✓

Can you still find Delisle thermometers?

Original antiques: Extremely rare and valuable

  • Russian-made Delisle thermometers (1738-1850): $1,000-$10,000+
  • Dual-scale Delisle/Réaumur (1780-1840): $800-$5,000
  • Most survive in Russian museums, private collections, or academic institutions

Modern reproductions: Very limited availability

  • Some specialty scientific instrument makers produce educational replicas
  • Mostly for museum exhibits or science education purposes
  • Generally not commercially available

Why so rare:

  • Short production period (≈110 years)
  • Limited geographic area (Russian Empire only)
  • Wars and revolutions destroyed many (1812, 1917, WWII)
  • Glass fragility means few survived intact

What does negative Delisle mean?

Negative Delisle = Above boiling point (>100°C):

Since 0°De = 100°C (boiling), temperatures above boiling would be negative:

  • -15°De = 110°C (230°F) - pressurized water
  • -30°De = 120°C (248°F) - autoclave sterilization
  • -150°De = 200°C (392°F) - hot oven

Rarely used: Delisle's original design focused on ambient and cooling temperatures. High-temperature applications were uncommon in 18th-century Russia, so negative Delisle values are virtually absent from historical records.

How do historians handle Russian weather data in Delisle?

Conversion workflow:

  1. Identify Delisle readings in archival documents (e.g., "180 градусов Делиля" = 180 degrees Delisle)
  2. Apply conversion formula: °C = 100 - (180 × 2/3) = 100 - 120 = -20°C
  3. Convert to Fahrenheit if needed: (-20 × 1.8) + 32 = -4°F
  4. Document both original and converted values for scholarly accuracy

Example from historical record:

  • Original: "Санкт-Петербург, 15 января 1740, 195°De" (St. Petersburg, January 15, 1740, 195°De)
  • Conversion: 100 - (195 × 2/3) = 100 - 130 = -30°C = -22°F (severe cold)

Why is Delisle important to the history of science?

Scientific significance:

  1. Methodological diversity: Demonstrates how experimental procedure shaped measurement design
  2. Governmental standardization: First empire-wide temperature scale adoption (1738)
  3. Cultural context: Reflects Russian Empire's scientific modernization under Peter the Great's legacy
  4. Measurement evolution: Shows the pre-standardization diversity of temperature scales
  5. Unique inversion: Only inverted scale to achieve widespread official use

Lessons:

  • Measurement standards require international consensus, not just local adoption
  • Intuitive design matters for widespread acceptance
  • Historical contingency (Delisle's Academy position) can temporarily override scientific merit

Are there any other inverted temperature scales?

No other major inverted scales achieved significant use.

Minor historical attempts:

  • Some early thermometers were calibrated from hot to cold simply due to construction methods
  • Individual scientists occasionally created personal inverted scales for specific experiments

Why Delisle is unique:

  • Only inverted scale adopted by a government (Imperial Russia, 1738)
  • Only inverted scale used for over a century
  • Only inverted scale with substantial archival presence

All other successful temperature scales (Fahrenheit, Celsius, Réaumur, Kelvin, Rankine) use conventional orientation where higher numbers = hotter.

About Fahrenheit (°F)

Why does the US use Fahrenheit?

The United States uses Fahrenheit due to historical adoption, infrastructure investment, and cultural resistance to change.

Historical reasons:

  • Fahrenheit scale adopted in 1700s when US was British colony
  • Became deeply embedded in American culture
  • All infrastructure built around Fahrenheit (thermostats, ovens, etc.)

Why didn't US switch to Celsius?

  • Cost: Replacing millions of thermostats, ovens, signs would cost billions
  • Cultural resistance: Americans prefer familiar system
  • Perceived complexity: Relearning temperature reference points
  • Failed metric conversion: 1970s Metric Conversion Act was voluntary and largely unsuccessful

Advantages of Fahrenheit (often cited):

  • Finer resolution (1°F = 0.56°C) for everyday temps
  • Human comfort range fits roughly 0-100°F
  • Weather forecasts use whole numbers more often

Current status:

  • US is only major country using Fahrenheit daily
  • Science and medicine use Celsius/Kelvin
  • Unlikely to change in near future

How do you convert Fahrenheit to Celsius?

Use the formula: °C = (°F - 32) × 5/9

Step-by-step:

  1. Subtract 32 from the Fahrenheit temperature
  2. Multiply the result by 5
  3. Divide by 9 (or multiply by 5/9)

Examples:

  • 68°F: (68 - 32) × 5/9 = 36 × 5/9 = 20°C
  • 86°F: (86 - 32) × 5/9 = 54 × 5/9 = 30°C
  • 32°F: (32 - 32) × 5/9 = 0°C (freezing point)
  • 212°F: (212 - 32) × 5/9 = 100°C (boiling point)
  • -40°F: (-40 - 32) × 5/9 = -40°C (same in both!)

Quick approximations:

  • Rough estimate: Subtract 30, then divide by 2
  • Example: 80°F ≈ (80-30)/2 = 25°C (actual: 26.7°C)

Use our Fahrenheit to Celsius converter for accurate conversions.

What is normal body temperature in Fahrenheit?

Normal human body temperature is 98.6°F (37°C), though the normal range is 97-99°F.

Details:

  • Average: 98.6°F (37°C) when measured orally
  • Normal range: 97-99°F (individuals vary)
  • Varies by: Time of day, activity, measurement method
  • Morning: Typically lower (97.0-97.5°F)
  • Afternoon: Typically higher (98.5-99.5°F)

Fever thresholds:

  • 99-100.4°F: Low-grade fever
  • 100.4°F and above: Fever
  • 103°F and above: High fever (call doctor)
  • Above 105°F: Medical emergency

Measurement variations:

  • Oral: 98.6°F (standard)
  • Rectal: 99.6°F (1°F higher, most accurate)
  • Armpit: 97.6°F (1°F lower, least accurate)
  • Ear: ~98.6°F (when done correctly)

At what temperature does water freeze in Fahrenheit?

Water freezes at 32°F (0°C) at standard atmospheric pressure (sea level).

Freezing point details:

  • Pure water: Exactly 32°F at sea level
  • Salt water: Lower than 32°F (28°F for ocean water)
  • Higher elevation: Slightly lower than 32°F
  • Lower elevation: Slightly higher than 32°F

Related temperatures:

  • Frost formation: 32°F or below
  • Black ice: Forms around 32°F
  • Sleet: 32-34°F (rain freezing on contact)
  • Snow: Requires below 32°F air temperature

Why 32°F?

  • Fahrenheit's original scale placed water freezing at 32° based on his reference points
  • Not as intuitive as 0°C, but historically established

At what temperature does water boil in Fahrenheit?

Water boils at 212°F (100°C) at standard atmospheric pressure (sea level).

Boiling point details:

  • Sea level: 212°F exactly
  • Higher elevation: Lower than 212°F (198°F in Denver, CO)
  • Lower elevation: Higher than 212°F
  • Pressure cooker: Above 212°F (250°F at high pressure)

Elevation effects:

  • For every 500 feet above sea level, boiling point drops ~1°F
  • Denver (5,280 ft): Water boils at ~202°F
  • Mount Everest (29,000 ft): Water boils at ~160°F

Cooking implications:

  • High altitude: Longer cooking times needed
  • Pressure cookers: Faster cooking due to higher temp

Why 212°F?

  • Another fixed point on Fahrenheit's original scale
  • 180 degrees between freezing (32°F) and boiling (212°F)

What temperature is considered a fever?

A temperature of 100.4°F (38°C) or higher is generally considered a fever in adults.

Fever categories:

  • Normal: 97-99°F
  • Low-grade fever: 99-100.4°F
  • Mild fever: 100.4-102°F
  • Moderate fever: 102-103°F
  • High fever: 103-104°F
  • Very high fever: Above 104°F (seek medical care)

In children/infants:

  • Newborn (0-3 months): 100.4°F or higher (call doctor immediately)
  • Infant (3-36 months): 102°F or higher (call doctor)
  • Child: 103°F or higher (call doctor)

When to seek medical attention:

  • Adult fever above 103°F
  • Fever lasting more than 3 days
  • Infant under 3 months with any fever
  • Fever with severe symptoms (confusion, difficulty breathing)

Measurement note: Rectal temperatures are ~1°F higher, armpit ~1°F lower than oral.

Is -40°F the same as -40°C?

Yes! -40°F = -40°C exactly. This is the only temperature where both scales intersect.

Why this happens:

  • The conversion formula: °C = (°F - 32) × 5/9
  • At -40: (-40 - 32) × 5/9 = -72 × 5/9 = -40°C
  • Mathematically, this is the unique intersection point

Other relationships:

  • Below -40: Fahrenheit numbers are smaller than Celsius (e.g., -50°F = -45.6°C)
  • Above -40: Fahrenheit numbers are larger (e.g., 0°F = -17.8°C)

Practical context:

  • 40° is extremely cold (Arctic/Antarctic conditions)
  • Dangerous to humans without proper protection
  • Few places on Earth regularly reach this temperature

Fun fact: This is the most commonly cited "trivia" about temperature scales!

What is a comfortable room temperature in Fahrenheit?

68-72°F (20-22°C) is generally considered comfortable room temperature for most people.

Comfort ranges by activity:

  • Sleeping: 60-67°F (cooler is better)
  • Living areas: 68-72°F
  • Working: 68-76°F
  • Exercising indoors: 65-68°F

Factors affecting comfort:

  • Humidity: Lower humidity feels warmer
  • Air movement: Fans make it feel cooler
  • Clothing: Dress code affects ideal temp
  • Personal preference: Varies significantly
  • Age: Elderly prefer warmer (72-78°F)

Energy recommendations:

  • Department of Energy: 78°F summer, 68°F winter
  • OSHA workplace: 68-76°F
  • Energy saving: Adjust 7-10°F when away or sleeping

International differences:

  • US comfort: 68-72°F average
  • Europe comfort: 68-73°F (20-23°C)
  • Tropical regions: 75-80°F normal

How do you convert Celsius to Fahrenheit?

Use the formula: °F = (°C × 9/5) + 32

Step-by-step:

  1. Multiply the Celsius temperature by 9
  2. Divide by 5 (or multiply by 9/5 = 1.8)
  3. Add 32

Examples:

  • 20°C: (20 × 9/5) + 32 = 36 + 32 = 68°F
  • 30°C: (30 × 9/5) + 32 = 54 + 32 = 86°F
  • 0°C: (0 × 9/5) + 32 = 32°F (freezing point)
  • 100°C: (100 × 9/5) + 32 = 212°F (boiling point)
  • -40°C: (-40 × 9/5) + 32 = -40°F (same in both!)

Quick approximations:

  • Double the Celsius temp and add 30
  • Example: 20°C ≈ (20×2)+30 = 70°F (actual: 68°F)

Use our Celsius to Fahrenheit converter for accurate conversions.

What countries use Fahrenheit?

Very few countries use Fahrenheit today. The United States is the primary user.

Current Fahrenheit users:

  • United States (primary user for daily temperatures)
  • Bahamas (some usage)
  • Belize (some usage)
  • Cayman Islands
  • Palau
  • Federated States of Micronesia
  • Marshall Islands

US territories using Fahrenheit:

  • Puerto Rico
  • US Virgin Islands
  • Guam
  • American Samoa

Former users (switched to Celsius):

  • United Kingdom: Switched 1960s-1970s
  • Canada: Switched 1970s
  • Australia: Switched 1970s
  • New Zealand: Switched 1970s
  • South Africa: Switched 1960s-1970s

Rest of world: Uses Celsius exclusively (195+ countries)

In science/medicine: Even US uses Celsius and Kelvin for scientific work.

What is the difference between Fahrenheit and Celsius?

Fahrenheit and Celsius are different temperature scales with different zero points and degree sizes.

Key differences:

| Feature | Fahrenheit | Celsius | |---------|-----------|---------| | Freezing point of water | 32°F | 0°C | | Boiling point of water | 212°F | 100°C | | Degrees between | 180° | 100° | | Absolute zero | -459.67°F | -273.15°C | | Degree size | Smaller (1°F = 0.56°C) | Larger (1°C = 1.8°F) | | Primary users | USA, few others | Rest of world (195+ countries) |

Conversion:

  • °C = (°F - 32) × 5/9
  • °F = (°C × 9/5) + 32

Intersection point: -40°F = -40°C (only place scales match)

Practical differences:

  • Celsius is simpler (0° freeze, 100° boil)
  • Fahrenheit provides finer resolution
  • Celsius aligned with metric system
  • Fahrenheit embedded in US culture

Convert between them: F to C | C to F

People Also Ask

How do I convert Delisle to Fahrenheit?

To convert Delisle to Fahrenheit, enter the value in Delisle in the calculator above. The conversion will happen automatically. Use our free online converter for instant and accurate results. You can also visit our temperature converter page to convert between other units in this category.

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What is the conversion factor from Delisle to Fahrenheit?

The conversion factor depends on the specific relationship between Delisle and Fahrenheit. You can find the exact conversion formula and factor on this page. Our calculator handles all calculations automatically. See the conversion table above for common values.

Can I convert Fahrenheit back to Delisle?

Yes! You can easily convert Fahrenheit back to Delisle by using the swap button (⇌) in the calculator above, or by visiting our Fahrenheit to Delisle converter page. You can also explore other temperature conversions on our category page.

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What are common uses for Delisle and Fahrenheit?

Delisle and Fahrenheit are both standard units used in temperature measurements. They are commonly used in various applications including engineering, construction, cooking, and scientific research. Browse our temperature converter for more conversion options.

For more temperature conversion questions, visit our FAQ page or explore our conversion guides.

Other Temperature Units and Conversions

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Verified Against Authority Standards

All conversion formulas have been verified against international standards and authoritative sources to ensure maximum accuracy and reliability.

NIST ITS-90 Temperature Scale

National Institute of Standards and TechnologyInternational Temperature Scale standards

BIPM Temperature Unit

Bureau International des Poids et MesuresDefinition of the kelvin and temperature scales

Last verified: February 19, 2026