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Santiago vs Tokyo

Csb Warm-summer MediterraneanCfa Humid subtropical

Comparing Santiago change · Tokyo change

Bottom line

Santiago and Tokyo have nearly identical year-round temperatures; Tokyo is the wetter, with 1272 mm more rain a year, and Santiago the sunnier.

Year-round temp About the same within 1°C on the year
Wetter Tokyo 1272 mm more a year
Sunnier Santiago 8 pp less cloud
Colder winters Tokyo 3°C colder nights

How the seasons compare

The differences between Santiago and Tokyo, in everyday terms.

Summers

Summers are nearly the same

Santiago: Warm
Tokyo: Hot

Winters

Santiago has milder winters

Santiago: Chilly
Tokyo: Chilly

Rain & snow

Tokyo is much wetter

Santiago: Fairly dry
Tokyo: Very wet

Sky

Santiago is sunnier

Santiago: Partly cloudy
Tokyo: Often cloudy

Month-by-month charts

Temperature

Santiago and Tokyo run remarkably close all year.

-10°10°20°30°40° JanAprJulOct SantiagoTokyo

Precipitation

Tokyo is the wetter — about 1272 mm more across the year.

PRECIPITATION (mm) 0120240 JanAprJulOct SantiagoTokyo

Clear skies

Santiago has the clearer skies — the higher line.

0%25%50%75%100% JanAprJulOct SantiagoTokyo

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
Santiago302928231916151720232629
Tokyo101114192426303128221712
Difference-20-19-13-4+5+10+15+14+8-1-9-17
Jan – JunJanFebMarAprMayJun
Santiago302928231916
Tokyo101114192426
Difference-20-19-13-4+5+10
Jul – DecJulAugSepOctNovDec
Santiago151720232629
Tokyo303128221712
Difference+15+14+8-1-9-17
Avg low (°C) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Santiago14131297545781013
Tokyo1251015192224201594
Difference-13-11-7+1+8+14+19+19+14+7-2-9
Jan – JunJanFebMarAprMayJun
Santiago141312975
Tokyo125101519
Difference-13-11-7+1+8+14
Jul – DecJulAugSepOctNovDec
Santiago45781013
Tokyo2224201594
Difference+19+19+14+7-2-9
Precipitation (mm) Tokyo runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Santiago0241945885454301676
Tokyo60561161341401681561552252359658
Difference+59+55+112+114+95+80+102+100+195+219+89+52
Jan – JunJanFebMarAprMayJun
Santiago024194588
Tokyo6056116134140168
Difference+59+55+112+114+95+80
Jul – DecJulAugSepOctNovDec
Santiago5454301676
Tokyo1561552252359658
Difference+102+100+195+219+89+52
Cloud cover (%) Tokyo runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Santiago333136536873706968624838
Tokyo465260647082756471675645
Difference+13+21+24+11+2+9+5-5+4+5+8+7
Jan – JunJanFebMarAprMayJun
Santiago333136536873
Tokyo465260647082
Difference+13+21+24+11+2+9
Jul – DecJulAugSepOctNovDec
Santiago706968624838
Tokyo756471675645
Difference+5-5+4+5+8+7
Relative humidity (%) Tokyo runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Santiago313232344251535150443531
Tokyo757475777982838182828077
Difference+44+42+44+42+37+31+30+30+32+38+45+47
Jan – JunJanFebMarAprMayJun
Santiago313232344251
Tokyo757475777982
Difference+44+42+44+42+37+31
Jul – DecJulAugSepOctNovDec
Santiago535150443531
Tokyo838182828077
Difference+30+30+32+38+45+47

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. Santiago trends → · Tokyo trends →

Methodology & sources

Santiago

Temperature & precipitation — the official 1991–2020 climate normals from the WMO's CLINO 1991–2020 collection, measured at Eulogiosancheztobalabaad, about 9 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.

Tokyo

Temperature & precipitation — the official 1991–2020 climate normals from the Japan Meteorological Agency, measured at Tokyo, about 5 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 →