| CITY | LOCAL TIME | Difference | Coming up |
|---|---|---|---|
| London United Kingdom | 01:00 | −4h | Becomes −5h on 25 Oct |
| Berlin Germany | 02:00 | −3h | Becomes −4h on 25 Oct |
| Dubai UAE | 04:00 | −1h | |
| Tokyo Japan | 09:00 | +4h | |
| Sydney Australia | 10:00 | +5h | Becomes +6h on 4 Oct |
| New York United States | 20:00Wed | −9h | Becomes −10h on 1 Nov |
| Los Angeles United States | 17:00Wed | −12h | Becomes −13h on 1 Nov |
Perm, Russia runs on UTC+5. This time zone stays fixed year-round at UTC+5 — daylight saving time is not observed. The time difference between Perm and New York is 9 hours. Standard working hours don't overlap at all with New York, so meetings need an early or late slot on one side. The time difference between Perm and London is 4 hours. Standard 9-to-6 working hours overlap for about 5 hours a day with London. A good time to connect: 13:00–18:00 in Perm lines up with 09:00–14:00 in London. The time difference between Perm and Tokyo is 4 hours. Standard 9-to-6 working hours overlap for about 5 hours a day with Tokyo. A good time to connect: 09:00–14:00 in Perm lines up with 13:00–18:00 in Tokyo. This timezone is also shared with cities such as Karachi, Astana, Lahore. Keeping these offsets in mind makes it easier to schedule calls or travel to and from Perm.
Perm (Russia) is home to roughly 1.0M people. Today brings about 11.6 hours of daylight: sunrise at 07:17, sunset at 18:52. This time zone stays fixed year-round at UTC+5 — daylight saving time is not observed. It sits in the Northern Hemisphere, about 58° north of the equator. Traffic drives on the right.
Flag
Russia
Capital
Moscow
Continent
Europe & Asia
Time Zone
UTC+5 · Asia/Yekaterinburg
Coordinates
58.01°N, 56.25°E
Currency
RUB (₽)
Calling Code
+7
Driving Side
Right
Hemisphere
Northern
Language
Russian
Measurement System
Metric
Did You Know?
The Permian period — the last before the Triassic, ending in the largest mass extinction in Earth's history — is named after Perm, where the Scottish geologist Roderick Murchison defined it in 1841. It is the only geological period named after a Russian place.
The clock: Perm keeps UTC+5. Its Diaghilev festival honours the impresario who grew up here and later ran the Ballets Russes in Paris.
Perm lies at 56.3°E. Its time zone, UTC+5, is built around the 75°E meridian. The 18.8° gap between them means the clock runs roughly 75 minutes ahead of the sun: solar noon arrives at about 13:15 rather than 12:00. The zone holds UTC+5 all year — there is no daylight saving here.
The longest day of 2026 is 22 June, with 18h 11m of daylight. The shortest is 22 December, with 6h 27m. The swing between them is 11h 44m. Close to the Arctic or Antarctic circle, the year swings hard between long light and long dark.
The earliest sunrise and the latest sunset do not land on the longest day. In Perm the sun comes up earliest on 19 June at 04:11, while the latest sunset waits until 25 June at 22:23. The equation of time is what separates them: the Earth's elliptical orbit and axial tilt move solar noon back and forth by several minutes over the year.
The sky stays usably light for a while after the sun goes down. In Perm that civil twilight runs about 39 minutes at the equinox, stretching to 76 minutes at the solstice.
Every figure in this section is computed from the city's own latitude, longitude and IANA time zone using NOAA solar algorithms (Spencer, 1971), accurate to about ±2 arcminutes below 65° latitude.
The official timezone for Perm, Russia is Asia/Yekaterinburg with a current UTC offset of UTC+5.
Perm has an estimated population of 1.0M and is located at coordinates 58.01°N, 56.25°E.
Perm gets 18h 11m of daylight on its longest day and 6h 27m on its shortest, averaging 12h 21m a day across the year.
Solar noon in Perm falls at about 13:15 on UTC+5 standard time, because the city sits 18.8° from the meridian its zone is built on.
Where the Permian Period Is Named From: The Permian period — the last before the Triassic, ending in the largest mass extinction in Earth's history — is named after Perm, where the Scottish geologist Roderick Murchison defined it in 1841.