FLASHCARDS: Hot and Cold Hacks for Temp Conversion

Gabrielle Birchak/ March 28, 2025/ Modern History

TRANSCRIPTS

It’s Flash­card Fri­day and here at Math! Sci­ence! His­to­ry! and we’re going to fig­ure out whether you need to take a coat or a swim­suit on your next vaca­tion. Because, if the news from Van­cou­ver, Cana­da is telling you it’s 35°, you’re def­i­nite­ly going to need a swim­suit. But if the news from Los Ange­les, CA is telling you it’s 35°, you’re going to need a parka!

Today, we’re going to flash you with the fas­ci­nat­ing his­to­ry of tem­per­a­ture mea­sure­ment and explore a neat trick for con­vert­ing between Cel­sius and Fahren­heit in your head.

The sto­ry of tem­per­a­ture begins in the ear­ly 1700s, with two sci­en­tists: Gabriel Fahren­heit and Anders Celsius.

Gabriel Fahren­heit was a Pol­ish-Ger­man physi­cist and engi­neer, born in 1686 in what is now mod­ern-day Poland. He was fas­ci­nat­ed with pre­ci­sion instru­ments, and in the ear­ly 1700s, he worked exten­sive­ly with mer­cury ther­mome­ters, vast­ly improv­ing their accu­ra­cy. In 1724, he intro­duced the Fahren­heit tem­per­a­ture scale, set­ting the freez­ing point of water at 32° and the boil­ing point at 212°, with 180 equal divi­sions in between. His work became wide­ly accept­ed, espe­cial­ly in Eng­land and lat­er in the Unit­ed States.

Anders Cel­sius, born in Swe­den in 1701, was an astronomer first and fore­most. He trav­eled exten­sive­ly across Europe, work­ing with the lead­ing sci­en­tists of his time. He was par­tic­u­lar­ly inter­est­ed in mea­sur­ing the auro­ra bore­alis and improv­ing astro­nom­i­cal obser­va­tions. In 1742, he pro­posed his tem­per­a­ture scale, where water freezes at 0 degrees and boils at 100 degrees, which was far sim­pler than Fahrenheit’s sys­tem. Oth­er than the reverse of degrees for boil­ing and freez­ing, it was a sim­pler mea­sur­ing sys­tem. The rea­son why he set his tem­per­a­ture scale with 0° at boil­ing and 100° at freez­ing was that he was influ­enced by a scale that was used at the time called the Delisle scale. The Delisle scale was invent­ed in 1732 by the French astronomer Joseph-Nico­las Delisle. Though he did­n’t have a tem­per­a­ture for freez­ing, he had set the boil­ing point at zero. As a result, this par­tic­u­lar scale had increas­ing num­bers for decreas­ing tem­per­a­tures. The pur­pose was to avoid work­ing with neg­a­tive val­ues. How­ev­er, after Cel­sius died in 1744, sci­en­tists and math­e­mati­cians flipped the scale putting 0° at freez­ing and 100° at boiling.

And in case you’re won­der­ing, Fahren­heit and Cel­sius nev­er met, and their scales weren’t exact­ly part of a direct rival­ry. By the time Cel­sius intro­duced his sys­tem, Fahrenheit’s had already been in use for near­ly two decades. How­ev­er, the world nat­u­ral­ly grav­i­tat­ed toward Cel­sius’ met­ric-based sys­tem over time because of its sim­plic­i­ty and com­pat­i­bil­i­ty with sci­en­tif­ic measurements.

Fahren­heit remains the stan­dard in the Unit­ed States, as well as a few oth­er places like the Bahamas and Cay­man Islands. This is large­ly due to his­tor­i­cal adoption—when the U.S. first estab­lished stan­dard­ized mea­sure­ments, Fahren­heit was already in use, and switch­ing to Cel­sius lat­er would have required mas­sive effort and pub­lic adjust­ment. Addi­tion­al­ly, Fahren­heit is often pre­ferred for weath­er report­ing because it pro­vides more pre­cise incre­men­tal changes at com­mon tem­per­a­tures, mak­ing it eas­i­er to describe small fluctuations.

Most of the world, how­ev­er, uses Cel­sius due to its log­i­cal 0–100 scale, which fits well with­in the met­ric sys­tem used for sci­en­tif­ic and every­day mea­sure­ments. Coun­tries that have switched from Fahren­heit to Cel­sius, such as Cana­da and the UK, did so as part of broad­er met­ri­ca­tion efforts in the 20th century.

Now let’s say you are plan­ning your vaca­tion and you are lis­ten­ing to Radio Cana­da, one of my favorite apps, and you’re plan­ning to go to Van­cou­ver, Cana­da. Now you know they have tepid tem­per­a­tures depend­ing on the time of year. And the news is say­ing that it is 35°. And you’re think­ing ohh my gosh, it’s like July and I have to take a par­ka this is awful. And then you show up, and every­body’s walk­ing around in shorts and you’re burn­ing up in a sweater. Why did that hap­pen? Well, Cana­da mea­sures their tem­per­a­tures in Cel­sius and the Unit­ed States mea­sures their tem­per­a­tures in Fahren­heit. You for­got to con­vert the two tem­per­a­tures! But, now that will nev­er hap­pen, because there’s a way to quick­ly con­vert them in your head.

First, to con­vert Cel­sius to Fahren­heit, you can dou­ble the Cel­sius tem­per­a­ture and then add 30. Here’s how it works:

Let’s say it’s 20 degrees Cel­sius. Dou­ble it to get 40, then add 30. That gives you 70 degrees Fahrenheit.

To con­vert Fahren­heit to Cel­sius, you can sub­tract 30 and then divide by 2. For exam­ple, if it’s 86 degrees Fahren­heit, sub­tract 30 to get 56, then divide by 2, which gives you 28 degrees Celsius.

To make it even sim­pler, you can round down or up the num­bers. So in the last exam­ple, to con­vert Fahren­heit to Cel­sius, if it’s 86°, you sub­tract 30, and you have 56. Just round 56 up to 60, and divide by two, which gives you approx­i­mate­ly 30°.

But if you want more than an approx­i­ma­tion, the actu­al for­mu­la is slight­ly different:

Fahren­heit equals Cel­sius times 1.8 plus 32, and Cel­sius equals Fahren­heit minus 32 times .56

Small fluc­tu­a­tions in Fahren­heit can result in seem­ing­ly larg­er changes com­pared to Cel­sius, due to the fin­er scale divi­sions. For exam­ple, a 1‑degree Fahren­heit change is only about 0.56 degrees Cel­sius, which means Fahren­heit allows for more detailed tem­per­a­ture gra­da­tions in weath­er fore­cast­ing and day-to-day use.

And if you’re lis­ten­ing to this while you’re dri­ving and you’re try­ing to write it down and make sense of it, first, don’t write any­thing down while you’re dri­ving pay atten­tion to the road. But if you do want to write it down and you do want to solve this, don’t for­get to use PEMDAS, which is an acronym for Paren­the­ses, Expo­nents, Mul­ti­pli­ca­tion, Divi­sion, Addi­tion, and Sub­trac­tion: in that order. It’s also an acronym for Please Excuse My Dear Aunt Sal­ly, which is not only use­ful in remem­ber­ing PEMDAS, but it’s also use­ful if you and your aunt Sal­ly are in pub­lic and she’s real­ly gassy.

So what are some take­aways that we can learn from this? First, under­stand the tem­per­a­ture scales, And remem­ber that in Cel­sius, 0° is freez­ing and boil­ing is 100°. And in Fahren­heit, water freezes at 32°, and boils at 212°.

Sec­ond, Remem­ber the sim­ple rule for con­ver­sion, which is dou­ble the Cel­sius tem­per­a­ture, add 30, and you’re close to Fahrenheit.

Third, dou­ble-check your trav­el plans to ensure you’re trav­el­ing to a coun­try with a tem­per­a­ture of either Fahren­heit or Celsius.

And there you have it! A quick look at the his­to­ry of tem­per­a­ture mea­sure­ment, a men­tal short­cut to con­vert between Cel­sius and Fahren­heit, and an under­stand­ing of why some regions pre­fer one scale over the oth­er. Next time you’re check­ing the weath­er, you’ll be able to do those con­ver­sions with ease. Thanks for tun­ing in, and we’ll catch you next time on Math! Sci­ence! History!

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