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Hakuba vs Tusayan

Cfa Humid subtropicalCsb Warm-summer Mediterranean

Comparing Hakuba change · Tusayan change

Bottom line

Hakuba is the warmer of the two — about 2°C on the annual average; Hakuba is the wetter, with 1078 mm more rain a year, and Tusayan the sunnier.

Warmer Hakuba 2°C on the year
Wetter Hakuba 1078 mm more a year
Sunnier Tusayan 33 pp less cloud
Colder winters Tusayan 3°C colder nights

How the seasons compare

The differences between Hakuba and Tusayan, in everyday terms.

Summers

Summers are nearly the same

Hakuba: Warm
Tusayan: Warm

Winters

Hakuba has milder winters

Hakuba: Very cold
Tusayan: Very cold

Rain & snow

Hakuba is much wetter

Hakuba: Wet
Tusayan: Fairly dry

Sky

Tusayan is far sunnier

Hakuba: Often grey
Tusayan: Fairly sunny

Month-by-month charts

Temperature

Hakuba is the warmer of the two — about 2°C on the annual average.

-20°20°40° JanAprJulOct HakubaTusayan

Precipitation

Hakuba is the wetter — about 1078 mm more across the year.

PRECIPITATION (mm) 0100200 JanAprJulOct HakubaTusayan

Clear skies

Tusayan has the clearer skies — the higher line.

0%25%50%75%100% JanAprJulOct HakubaTusayan

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) Tusayan runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba23715212427292418125
Tusayan781316222830282519127
Difference+5+5+5+1+1+5+3+1+1+1+2
Jan – JunJanFebMarAprMayJun
Hakuba237152124
Tusayan7813162228
Difference+5+5+5+1+1+5
Jul – DecJulAugSepOctNovDec
Hakuba27292418125
Tusayan30282519127
Difference+3+1+1+1+2
Avg low (°C) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba-8-7-3281317181471-4
Tusayan-10-9-6-4-13994-2-7-10
Difference-2-1-3-6-9-10-8-9-9-9-8-7
Jan – JunJanFebMarAprMayJun
Hakuba-8-7-32813
Tusayan-10-9-6-4-13
Difference-2-1-3-6-9-10
Jul – DecJulAugSepOctNovDec
Hakuba17181471-4
Tusayan994-2-7-10
Difference-8-9-9-9-8-7
Precipitation (mm) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba8578100981121591951361651297079
Tusayan27262618159495334331820
Difference-57-52-74-80-96-150-146-83-131-96-52-59
Jan – JunJanFebMarAprMayJun
Hakuba857810098112159
Tusayan27262618159
Difference-57-52-74-80-96-150
Jul – DecJulAugSepOctNovDec
Hakuba1951361651297079
Tusayan495334331820
Difference-146-83-131-96-52-59
Cloud cover (%) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba787573697180797076717277
Tusayan484946413727504632323748
Difference-30-26-27-28-34-53-29-23-43-39-35-29
Jan – JunJanFebMarAprMayJun
Hakuba787573697180
Tusayan484946413727
Difference-30-26-27-28-34-53
Jul – DecJulAugSepOctNovDec
Hakuba797076717277
Tusayan504632323748
Difference-29-23-43-39-35-29
Relative humidity (%) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba908782767579818183848588
Tusayan615749413525374340425060
Difference-28-30-33-35-40-54-45-38-43-42-35-28
Jan – JunJanFebMarAprMayJun
Hakuba908782767579
Tusayan615749413525
Difference-28-30-33-35-40-54
Jul – DecJulAugSepOctNovDec
Hakuba818183848588
Tusayan374340425060
Difference-45-38-43-42-35-28

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. Hakuba trends → · Tusayan trends →

Methodology & sources

Hakuba

Temperature & precipitation — the official 1991–2020 climate normals from the Japan Meteorological Agency, measured at Omachi, about 20 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 →