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Èze vs Nagoya

Csa Hot-summer MediterraneanCfa Humid subtropical

Comparing Èze change · Nagoya change

Bottom line

Èze and Nagoya have nearly identical year-round temperatures; Nagoya is the wetter, with 833 mm more rain a year, and Èze the sunnier.

Year-round temp About the same within 1°C on the year
Wetter Nagoya 833 mm more a year
Sunnier Èze 21 pp less cloud
Colder winters Nagoya 4°C colder nights

How the seasons compare

The differences between Èze and Nagoya, in everyday terms.

Summers

Nagoya has much hotter summers

Èze: Warm
Nagoya: Hot

Winters

Èze has milder winters

Èze: Cool
Nagoya: Chilly

Rain & snow

Nagoya is wetter

Èze: Moderate rainfall
Nagoya: Very wet

Sky

Èze is sunnier

Èze: Partly cloudy
Nagoya: Often cloudy

Month-by-month charts

Temperature

Èze and Nagoya run remarkably close all year.

-10°0°10°20°30°40° JanAprJulOct ÈzeNagoya

Precipitation

Nagoya is the wetter — about 833 mm more across the year.

PRECIPITATION (mm) 0120240 JanAprJulOct ÈzeNagoya

Clear skies

Èze has the clearer skies — the higher line.

0%25%50%75%100% JanAprJulOct ÈzeNagoya

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
Èze131416182125282825211714
Nagoya91115202528313329231712
Difference-4-3-1+3+3+3+4+5+4+2—-3
Jan – JunJanFebMarAprMayJun
Èze131416182125
Nagoya91115202528
Difference-4-3-1+3+3+3
Jul – DecJulAugSepOctNovDec
Èze282825211714
Nagoya313329231712
Difference+4+5+4+2—-3
Avg low (°C) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Èze5681014182121181496
Nagoya1151015192425211593
Difference-4-4-3-1+1+1+3+4+3+1-1-3
Jan – JunJanFebMarAprMayJun
Èze568101418
Nagoya115101519
Difference-4-4-3-1+1+1
Jul – DecJulAugSepOctNovDec
Èze2121181496
Nagoya2425211593
Difference+3+4+3+1-1-3
Precipitation (mm) Nagoya runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Èze72534864423411246611612989
Nagoya51651161281501872111392321657957
Difference-21+12+68+63+108+153+200+116+166+49-50-32
Jan – JunJanFebMarAprMayJun
Èze725348644234
Nagoya5165116128150187
Difference-21+12+68+63+108+153
Jul – DecJulAugSepOctNovDec
Èze11246611612989
Nagoya2111392321657957
Difference+200+116+166+49-50-32
Cloud cover (%) Nagoya runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Èze575652555442323444545957
Nagoya757269666980776671666772
Difference+18+17+17+11+16+38+45+32+28+12+8+15
Jan – JunJanFebMarAprMayJun
Èze575652555442
Nagoya757269666980
Difference+18+17+17+11+16+38
Jul – DecJulAugSepOctNovDec
Èze323444545957
Nagoya776671666772
Difference+45+32+28+12+8+15
Relative humidity (%) Nagoya runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Èze727274777877747373767372
Nagoya817876767882838281808082
Difference+9+7+2-1—+5+9+8+8+4+6+10
Jan – JunJanFebMarAprMayJun
Èze727274777877
Nagoya817876767882
Difference+9+7+2-1—+5
Jul – DecJulAugSepOctNovDec
Èze747373767372
Nagoya838281808082
Difference+9+8+8+4+6+10

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. Èze trends → · Nagoya trends →

Methodology & sources

Èze

Temperature & precipitation — 1991–2020 normals computed from 26 years of daily observations at Cote D Azur, a weather station, about 14 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.

Nagoya

Temperature & precipitation — the official 1991–2020 climate normals from the Japan Meteorological Agency, measured at Nagoya, about 6 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.

How we build these numbers →