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Luxor vs Kyoto

BWh Hot desertCfa Humid subtropical

Comparing Luxor change · Kyoto change

Bottom line

Luxor is the warmer of the two — about 9°C on the annual average; Kyoto is the wetter, with 1501 mm more rain a year, and Luxor the sunnier.

Warmer Luxor 9°C on the year
Wetter Kyoto 1501 mm more a year
Sunnier Luxor 58 pp less cloud
Colder winters Kyoto 5°C colder nights

How the seasons compare

The differences between Luxor and Kyoto, in everyday terms.

Summers

Luxor has far hotter summers

Luxor: Extreme heat
Kyoto: Hot

Winters

Luxor has much milder winters

Luxor: Cool
Kyoto: Chilly

Rain & snow

Kyoto is much wetter

Luxor: Very dry
Kyoto: Wet

Sky

Luxor is far sunnier

Luxor: Sunny
Kyoto: Often grey

Month-by-month charts

Temperature

Luxor is the warmer of the two — about 9°C on the annual average.

-0°20°40° JanAprJulOct LuxorKyoto

Precipitation

Kyoto is the wetter — about 1501 mm more across the year.

PRECIPITATION (mm) 0115230 JanAprJulOct LuxorKyoto

Clear skies

Luxor has the clearer skies — the higher line.

0%25%50%75%100% JanAprJulOct LuxorKyoto

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
Kyoto91014202528323429231712
Difference-14-15-16-15-14-13-9-8-10-12-12-13
Jan – JunJanFebMarAprMayJun
Luxor232530353941
Kyoto91014202528
Difference-14-15-16-15-14-13
Jul – DecJulAugSepOctNovDec
Luxor414139352924
Kyoto323429231712
Difference-9-8-10-12-12-13
Avg low (°C) Luxor runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Luxor791317222526252319138
Kyoto224915192425211484
Difference-5-7-8-8-7-5-2-1-3-5-5-5
Jan – JunJanFebMarAprMayJun
Luxor7913172225
Kyoto22491519
Difference-5-7-8-8-7-5
Jul – DecJulAugSepOctNovDec
Luxor26252319138
Kyoto2425211484
Difference-2-1-3-5-5-5
Precipitation (mm) Kyoto runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Luxor2022120001130
Kyoto53651061171512002241541791437457
Difference+51+65+105+115+140+200+223+154+178+142+71+57
Jan – JunJanFebMarAprMayJun
Luxor2022120
Kyoto5365106117151200
Difference+51+65+105+115+140+200
Jul – DecJulAugSepOctNovDec
Luxor001130
Kyoto2241541791437457
Difference+223+154+178+142+71+57
Cloud cover (%) Kyoto runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Luxor242525272410989111522
Kyoto848175697181776674707480
Difference+60+56+49+43+47+71+68+58+65+59+58+58
Jan – JunJanFebMarAprMayJun
Luxor242525272410
Kyoto848175697181
Difference+60+56+49+43+47+71
Jul – DecJulAugSepOctNovDec
Luxor989111522
Kyoto776674707480
Difference+68+58+65+59+58+58
Relative humidity (%) Kyoto runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Luxor463727201818202125304047
Kyoto858381798184868485848485
Difference+39+46+54+59+63+66+66+63+60+54+44+38
Jan – JunJanFebMarAprMayJun
Luxor463727201818
Kyoto858381798184
Difference+39+46+54+59+63+66
Jul – DecJulAugSepOctNovDec
Luxor202125304047
Kyoto868485848485
Difference+66+63+60+54+44+38

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 → · Kyoto 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.

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.

How we build these numbers →