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Luxor vs Tokyo

BWh Hot desertCfa Humid subtropical

Comparing Luxor change · Tokyo change

Bottom line

Luxor is the warmer of the two — about 10°C on the annual average; Tokyo is the wetter, with 1576 mm more rain a year, and Luxor the sunnier.

Warmer Luxor 10°C on the year
Wetter Tokyo 1576 mm more a year
Sunnier Luxor 45 pp less cloud
Colder winters Tokyo 6°C colder nights

How the seasons compare

The differences between Luxor and Tokyo, in everyday terms.

Summers

Luxor has far hotter summers

Luxor: Extreme heat
Tokyo: Hot

Winters

Luxor has much milder winters

Luxor: Cool
Tokyo: Chilly

Rain & snow

Tokyo is much wetter

Luxor: Very dry
Tokyo: Very wet

Sky

Luxor is far sunnier

Luxor: Sunny
Tokyo: Often cloudy

Month-by-month charts

Temperature

Luxor is the warmer of the two — about 10°C on the annual average.

-0°20°40° JanAprJulOct LuxorTokyo

Precipitation

Tokyo is the wetter — about 1576 mm more across the year.

PRECIPITATION (mm) 0120240 JanAprJulOct LuxorTokyo

Clear skies

Luxor has the clearer skies — the higher line.

0%25%50%75%100% JanAprJulOct LuxorTokyo

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) Luxor runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Luxor232530353941414139352924
Tokyo101114192426303128221712
Difference-13-14-15-16-16-15-12-10-12-13-12-12
Jan – JunJanFebMarAprMayJun
Luxor232530353941
Tokyo101114192426
Difference-13-14-15-16-16-15
Jul – DecJulAugSepOctNovDec
Luxor414139352924
Tokyo303128221712
Difference-12-10-12-13-12-12
Avg low (°C) Luxor runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Luxor791317222526252319138
Tokyo1251015192224201594
Difference-6-7-8-8-7-6-3-2-3-5-5-5
Jan – JunJanFebMarAprMayJun
Luxor7913172225
Tokyo125101519
Difference-6-7-8-8-7-6
Jul – DecJulAugSepOctNovDec
Luxor26252319138
Tokyo2224201594
Difference-3-2-3-5-5-5
Precipitation (mm) Tokyo runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Luxor2022120001130
Tokyo60561161341401681561552252359658
Difference+58+56+114+132+128+168+156+155+224+234+93+58
Jan – JunJanFebMarAprMayJun
Luxor2022120
Tokyo6056116134140168
Difference+58+56+114+132+128+168
Jul – DecJulAugSepOctNovDec
Luxor001130
Tokyo1561552252359658
Difference+156+155+224+234+93+58
Cloud cover (%) Tokyo runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Luxor242525272410989111522
Tokyo465260647082756471675645
Difference+21+28+35+37+45+72+66+56+63+56+40+23
Jan – JunJanFebMarAprMayJun
Luxor242525272410
Tokyo465260647082
Difference+21+28+35+37+45+72
Jul – DecJulAugSepOctNovDec
Luxor989111522
Tokyo756471675645
Difference+66+56+63+56+40+23
Relative humidity (%) Tokyo runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Luxor463727201818202125304047
Tokyo757475777982838182828077
Difference+30+38+48+57+61+65+64+60+57+52+40+30
Jan – JunJanFebMarAprMayJun
Luxor463727201818
Tokyo757475777982
Difference+30+38+48+57+61+65
Jul – DecJulAugSepOctNovDec
Luxor202125304047
Tokyo838182828077
Difference+64+60+57+52+40+30

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. Luxor trends → · Tokyo trends →

Methodology & sources

Luxor

Temperature & precipitation — 1991–2020 normals computed from 30 years of daily observations at Luxor Intl, a weather station, about 7 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 →