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Sendai vs Tusayan

Cfa Humid subtropicalCsb Warm-summer Mediterranean

Comparing Sendai change · Tusayan change

Bottom line

Sendai is the warmer of the two — about 5°C on the annual average; Sendai is the wetter, with 948 mm more rain a year, and Tusayan the sunnier.

Warmer Sendai 5°C on the year
Wetter Sendai 948 mm more a year
Sunnier Tusayan 34 pp less cloud
Colder winters Tusayan 9°C colder nights

How the seasons compare

The differences between Sendai and Tusayan, in everyday terms.

Summers

Tusayan has hotter summers

Sendai: Warm
Tusayan: Warm

Winters

Sendai has much milder winters

Sendai: Cold
Tusayan: Very cold

Rain & snow

Sendai is much wetter

Sendai: Wet
Tusayan: Fairly dry

Sky

Tusayan is far sunnier

Sendai: Often grey
Tusayan: Fairly sunny

Month-by-month charts

Temperature

Sendai is the warmer of the two — about 5°C on the annual average.

-20°20°40° JanAprJulOct SendaiTusayan

Precipitation

Sendai is the wetter — about 948 mm more across the year.

PRECIPITATION (mm) 0100200 JanAprJulOct SendaiTusayan

Clear skies

Tusayan has the clearer skies — the higher line.

0%25%50%75%100% JanAprJulOct SendaiTusayan

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
Sendai671016202327282520148
Tusayan781316222830282519127
Difference+1+2+3+1+2+5+3-1-2-1
Jan – JunJanFebMarAprMayJun
Sendai6710162023
Tusayan7813162228
Difference+1+2+3+1+2+5
Jul – DecJulAugSepOctNovDec
Sendai27282520148
Tusayan30282519127
Difference+3-1-2-1
Avg low (°C) Sendai runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Sendai-1-11612162022181261
Tusayan-10-9-6-4-13994-2-7-10
Difference-8-8-8-10-12-13-11-13-14-14-12-11
Jan – JunJanFebMarAprMayJun
Sendai-1-1161216
Tusayan-10-9-6-4-13
Difference-8-8-8-10-12-13
Jul – DecJulAugSepOctNovDec
Sendai2022181261
Tusayan994-2-7-10
Difference-11-13-14-14-12-11
Precipitation (mm) Sendai runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Sendai423474901101441781581931515944
Tusayan27262618159495334331820
Difference-15-8-48-72-95-135-129-104-159-118-41-24
Jan – JunJanFebMarAprMayJun
Sendai42347490110144
Tusayan27262618159
Difference-15-8-48-72-95-135
Jul – DecJulAugSepOctNovDec
Sendai1781581931515944
Tusayan495334331820
Difference-129-104-159-118-41-24
Cloud cover (%) Sendai runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Sendai777573717177807176727479
Tusayan484946413727504632323748
Difference-29-26-28-30-34-49-30-25-44-41-37-31
Jan – JunJanFebMarAprMayJun
Sendai777573717177
Tusayan484946413727
Difference-29-26-28-30-34-49
Jul – DecJulAugSepOctNovDec
Sendai807176727479
Tusayan504632323748
Difference-30-25-44-41-37-31
Relative humidity (%) Sendai runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Sendai959387828183868587878993
Tusayan615749413525374340425060
Difference-33-36-38-41-46-58-49-42-46-45-39-32
Jan – JunJanFebMarAprMayJun
Sendai959387828183
Tusayan615749413525
Difference-33-36-38-41-46-58
Jul – DecJulAugSepOctNovDec
Sendai868587878993
Tusayan374340425060
Difference-49-42-46-45-39-32

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. Sendai trends → · Tusayan trends →

Methodology & sources

Sendai

Temperature & precipitation — the official 1991–2020 climate normals from the Japan Meteorological Agency, measured at Sendai, about 3 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.

Tusayan

Temperature & precipitation — 1991–2020 normals computed from 24 years of daily observations at Grand Canyon NP AP, a weather station, about 4 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.

How we build these numbers →