Skycap

Why flying east is faster: about 40 minutes coast to coast, an hour in winter

By Derek Johnson. Updated Nov 7, 2026.

Long parallel streaks of high cirrus in cold afternoon light, seen from an aircraft window.

Flying east is faster because the jet stream blows from west to east, and a plane’s speed through the air adds to the speed of the air itself. Coast to coast, that’s worth about 40 minutes over a year and about an hour in winter. The figure you usually read, “about 30 minutes”, is low for those flights, and it hides how much the season matters.

Those numbers are mine. I took 12 months of public flight records, September 2025 through August 2026, and compared the median time in the air each way. That’s wheels-off to wheels-on, so taxiing and schedule padding don’t count.

RouteWestboundEastboundDifferenceDecember to FebruaryJune to August
Boston and San Francisco363 min303 min60 min75 min54 min
JFK and San Francisco349 min296 min53 min70 min41 min
Atlanta and Seattle293 min248 min45 min69 min33 min
JFK and Los Angeles327 min289 min38 min59 min20 min
Chicago and Los Angeles230 min209 min21 min28 min13 min
Chicago and Denver128 min114 min14 min19 min11 min
Dallas and Los Angeles165 min154 min11 min20 min-2 min

How it scales with distance

Across 373 US east-west routes between 1,000 and 3,000 miles, each with at least 600 flights a year in both directions, the median gap looks like this:

Route lengthRoutesOver the yearDecember to FebruaryJune to August
1,000 to 1,500 mi17520 min31 min7 min
1,500 to 2,000 mi9432 min47 min15 min
2,000 to 2,300 mi3939 min58 min17 min
2,300 to 3,000 mi6541 min63 min28 min

So “about 30 minutes” is a fair figure for a mid-length route averaged over a year. On a long route in January it’s half the story. On a short one in July it’s four times too high.

What’s doing it

Jet streams are narrow bands of fast wind, usually about 30,000 feet up, right where airliners cruise. NOAA says they can top 275 mph and that they’re strongest in winter.

You can work out the wind a flight sees from these times. JFK to San Francisco is 2,580 miles on the great circle. At the median times, that’s about 444 mph going west and 523 mph going east, which means an average wind along the route of about 40 mph. In winter it comes to about 52 mph, and in summer about 31. Those are whole-flight averages, climb and descent included, and westbound flights choose tracks that avoid the worst of it, so the jet’s peak is far stronger than this.

Why the south loses it in summer

In summer the polar jet stream typically moves up toward the US-Canada border, and the table shows it happening. Boston to San Francisco keeps 54 minutes of its gap in summer. Atlanta to Los Angeles, on a route much farther south, goes from 45 minutes in winter to 5. Dallas to Los Angeles disappears altogether, and in those three months the eastbound flight ran 2 minutes slower.

For a single route the seasons look like this. JFK to Los Angeles has a median of 342 minutes in February and 308 in July. The trip back takes 279 minutes in February and 298 in July. The westbound flight gains 34 minutes from winter to summer, and the eastbound loses 19.

The Earth’s spin has nothing to do with it

A common explanation is that the planet turns beneath you, so flying east or west changes the distance. The air turns along with the planet, though, and a plane flies through the air. With no wind, both directions would take the same time.

North-south routes make the point, since they cross the jet stream instead of riding it. Minneapolis to Dallas has a median of 119 minutes one way and 117 the other. Seattle to Los Angeles is 130 and 133.

What it means for your day

Airlines build these differences into schedules, so the printed times already lean this way. What a schedule can’t know is this week’s wind. On JFK to Los Angeles, one westbound flight in ten took 307 minutes or less, and one in ten took 350 or more, across the year. That’s 43 minutes of spread on the same route, without a single delay on the ground counted.

If you’re meeting someone off a winter flight from the West Coast, it can arrive well before you’d guess. A westbound flight in January is the one to pad, especially if your connection is tight.

The line your flight takes depends on the same wind, which is covered in why your flight path curves. It’s also why a westbound sunset lasts so long: you’re running with it. And the edges of the jet stream are where much clear-air turbulence comes from, as how to read a turbulence forecast explains.

What the records leave out

The records cover US airlines’ domestic flights, so the Atlantic and Pacific aren’t here. Medians hide the unusual days, and air time also includes detours around storms and holds. This is one year, with one winter in it, and another year will differ. The route figures are medians for each direction, so a difference isn’t any single flight’s gap.

Skycap checks the winds along your route and says about how many minutes they should add or save on this flight. See what it shows in the air

Sources