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Kyoto vs Monaco

Cfa Humid subtropicalCsa Hot-summer Mediterranean

Comparing Kyoto change · Monaco change

Bottom line

Kyoto and Monaco have nearly identical year-round temperatures; Kyoto is the wetter, with 777 mm more rain a year, and Monaco the sunnier.

Year-round temp About the same within 1°C on the year
Wetter Kyoto 777 mm more a year
Sunnier Monaco 25 pp less cloud
Colder winters Kyoto 4°C colder nights

How the seasons compare

The differences between Kyoto and Monaco, in everyday terms.

Summers

Kyoto has much hotter summers

Kyoto: Hot
Monaco: Warm

Winters

Monaco has milder winters

Kyoto: Chilly
Monaco: Cool

Rain & snow

Kyoto is wetter

Kyoto: Wet
Monaco: Moderate rainfall

Sky

Monaco is far sunnier

Kyoto: Often grey
Monaco: Partly cloudy

Month-by-month charts

Temperature

Kyoto and Monaco run remarkably close all year.

-10°10°20°30°40° JanAprJulOct KyotoMonaco

Precipitation

Kyoto is the wetter — about 777 mm more across the year.

PRECIPITATION (mm) 0115230 JanAprJulOct KyotoMonaco

Clear skies

Monaco has the clearer skies — the higher line.

0%25%50%75%100% JanAprJulOct KyotoMonaco

Exact monthly numbers

Tap a metric to open its full table. Desktop shows all twelve months; on a phone each metric splits into Jan–Jun and Jul–Dec.

Avg high (°C) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Kyoto91014202528323429231712
Monaco131416182125282825211714
Difference+4+4+2-3-4-3-4-6-4-2+3
Jan – JunJanFebMarAprMayJun
Kyoto91014202528
Monaco131416182125
Difference+4+4+2-3-4-3
Jul – DecJulAugSepOctNovDec
Kyoto323429231712
Monaco282825211714
Difference-4-6-4-2+3
Avg low (°C) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Kyoto224915192425211484
Monaco5681014182121181496
Difference+4+4+4+1-1-3-4-3-1+1+3
Jan – JunJanFebMarAprMayJun
Kyoto22491519
Monaco568101418
Difference+4+4+4+1-1
Jul – DecJulAugSepOctNovDec
Kyoto2425211484
Monaco2121181496
Difference-3-4-3-1+1+3
Precipitation (mm) Kyoto runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Kyoto53651061171512002241541791437457
Monaco72534864423411246611612989
Difference+18-13-58-53-109-166-213-130-113-28+55+31
Jan – JunJanFebMarAprMayJun
Kyoto5365106117151200
Monaco725348644234
Difference+18-13-58-53-109-166
Jul – DecJulAugSepOctNovDec
Kyoto2241541791437457
Monaco11246611612989
Difference-213-130-113-28+55+31
Cloud cover (%) Kyoto runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Kyoto848175697181776674707480
Monaco575652555442323444545957
Difference-27-25-23-14-17-39-45-31-30-16-15-23
Jan – JunJanFebMarAprMayJun
Kyoto848175697181
Monaco575652555442
Difference-27-25-23-14-17-39
Jul – DecJulAugSepOctNovDec
Kyoto776674707480
Monaco323444545957
Difference-45-31-30-16-15-23
Relative humidity (%) Kyoto runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Kyoto858381798184868485848485
Monaco727274777877747373767372
Difference-12-11-6-3-3-7-12-11-11-8-10-13
Jan – JunJanFebMarAprMayJun
Kyoto858381798184
Monaco727274777877
Difference-12-11-6-3-3-7
Jul – DecJulAugSepOctNovDec
Kyoto868485848485
Monaco747373767372
Difference-12-11-11-8-10-13

How both climates are changing

Both cities are warming. Each city has its own warming trend; see its trends page for the year-by-year detail. Kyoto trends → · Monaco trends →

Methodology & sources

Kyoto

Temperature & precipitation — the official 1991–2020 climate normals from the Japan Meteorological Agency, measured at Kyoto, about 2 km from the city centre.

Cloud, humidity, wind & sunshine — modelled estimates from NASA POWER, NASA's satellite-and-reanalysis climatology. This is the standard global source for atmospheric variables, which are not measured at most weather stations.

Monaco

Temperature & precipitation — 1991–2020 normals computed from 26 years of daily observations at Cote D Azur, a weather station, about 19 km from the city centre. The underlying daily records come from NOAA's global station network.

Cloud, humidity, wind & sunshine — modelled estimates from NASA POWER, NASA's satellite-and-reanalysis climatology. This is the standard global source for atmospheric variables, which are not measured at most weather stations.

How we build these numbers →