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Granada vs Tokyo

Csa Hot-summer MediterraneanCfa Humid subtropical

Comparing Granada change · Tokyo change

Bottom line

Granada and Tokyo have nearly identical year-round temperatures; Tokyo is the wetter, with 1233 mm more rain a year, and Granada the sunnier.

Year-round temp About the same within 1°C on the year
Wetter Tokyo 1233 mm more a year
Sunnier Granada 20 pp less cloud
Winter nights About the same winter lows close to each other

How the seasons compare

The differences between Granada and Tokyo, in everyday terms.

Summers

Granada has much hotter summers

Granada: Very hot
Tokyo: Hot

Winters

Winters are similar

Granada: Chilly
Tokyo: Chilly

Rain & snow

Tokyo is much wetter

Granada: Fairly dry
Tokyo: Very wet

Sky

Granada is sunnier

Granada: Fairly sunny
Tokyo: Often cloudy

Month-by-month charts

Temperature

Granada and Tokyo run remarkably close all year.

-0°20°40° JanAprJulOct GranadaTokyo

Precipitation

Tokyo is the wetter — about 1233 mm more across the year.

PRECIPITATION (mm) 0120240 JanAprJulOct GranadaTokyo

Clear skies

Granada has the clearer skies — the higher line.

0%25%50%75%100% JanAprJulOct GranadaTokyo

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) Granada runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Granada141619222632363530241814
Tokyo101114192426303128221712
Difference-4-5-5-2-3-6-6-4-2-2-1-2
Jan – JunJanFebMarAprMayJun
Granada141619222632
Tokyo101114192426
Difference-4-5-5-2-3-6
Jul – DecJulAugSepOctNovDec
Granada363530241814
Tokyo303128221712
Difference-6-4-2-2-1-2
Avg low (°C) Tokyo runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Granada02471014161613942
Tokyo1251015192224201594
Difference+1+1+1+3+5+5+6+7+7+6+5+2
Jan – JunJanFebMarAprMayJun
Granada02471014
Tokyo125101519
Difference+1+1+1+3+5+5
Jul – DecJulAugSepOctNovDec
Granada161613942
Tokyo2224201594
Difference+6+7+7+6+5+2
Precipitation (mm) Tokyo runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Granada393640362981325425650
Tokyo60561161341401681561552252359658
Difference+20+21+76+97+110+159+155+152+200+193+40+8
Jan – JunJanFebMarAprMayJun
Granada39364036298
Tokyo6056116134140168
Difference+20+21+76+97+110+159
Jul – DecJulAugSepOctNovDec
Granada1325425650
Tokyo1561552252359658
Difference+155+152+200+193+40+8
Cloud cover (%) Tokyo runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Granada504850564932172338475051
Tokyo465260647082756471675645
Difference-4+4+9+8+20+50+58+41+34+20+6-5
Jan – JunJanFebMarAprMayJun
Granada504850564932
Tokyo465260647082
Difference-4+4+9+8+20+50
Jul – DecJulAugSepOctNovDec
Granada172338475051
Tokyo756471675645
Difference+58+41+34+20+6-5
Relative humidity (%) Tokyo runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Granada757267655847404355667376
Tokyo757475777982838182828077
Difference+3+8+12+21+35+44+39+27+16+7+1
Jan – JunJanFebMarAprMayJun
Granada757267655847
Tokyo757475777982
Difference+3+8+12+21+35
Jul – DecJulAugSepOctNovDec
Granada404355667376
Tokyo838182828077
Difference+44+39+27+16+7+1

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. Granada trends → · Tokyo trends →

Methodology & sources

Granada

Temperature & precipitation — 1991–2020 normals computed from 30 years of daily observations at Granada, a weather station, about 15 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.

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 →