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Hakuba vs Wrocław

Cfa Humid subtropicalCfb Oceanic / temperate

Comparing Hakuba change · Wrocław change

Bottom line

Hakuba and Wrocław have nearly identical year-round temperatures; Hakuba is the wetter, with 34 in more rain a year.

Year-round temp About the same within 2°F on the year
Wetter Hakuba 34 in more a year
Sunnier Wrocław 6 pp less cloud
Colder winters Hakuba 5°F colder nights

How the seasons compare

The differences between Hakuba and Wrocław, in everyday terms.

Summers

Hakuba has hotter summers

Hakuba: Warm
Wrocław: Mild

Winters

Wrocław has milder winters

Hakuba: Very cold
Wrocław: Cold

Rain & snow

Hakuba is much wetter

Hakuba: Wet
Wrocław: Fairly dry

Sky

Similar amounts of sun

Hakuba: Often grey
Wrocław: Often cloudy

Month-by-month charts

Temperature

Hakuba and Wrocław run remarkably close all year.

20°40°60°80° JanAprJulOct HakubaWrocław

Precipitation

Hakuba is the wetter — about 34 in more across the year.

PRECIPITATION (in) 048 JanAprJulOct HakubaWrocław

Clear skies

The two cities see a similar amount of sun.

0%25%50%75%100% JanAprJulOct HakubaWrocław

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 (°F) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba353745596975818375645341
Wrocław364148596873777768584739
Difference+1+4+3-1-2-4-7-7-5-6-2
Jan – JunJanFebMarAprMayJun
Hakuba353745596975
Wrocław364148596873
Difference+1+4+3-1-2
Jul – DecJulAugSepOctNovDec
Hakuba818375645341
Wrocław777768584739
Difference-4-7-7-5-6-2
Avg low (°F) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba191926364756636457453425
Wrocław242631394652565450413427
Difference+5+7+5+3-1-4-7-10-7-4+2
Jan – JunJanFebMarAprMayJun
Hakuba191926364756
Wrocław242631394652
Difference+5+7+5+3-1-4
Jul – DecJulAugSepOctNovDec
Hakuba636457453425
Wrocław565450413427
Difference-7-10-7-4+2
Precipitation (in) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba3.33.13.93.94.46.37.75.46.55.12.73.1
Wrocław1.211.31.32.32.53.32.121.61.21.1
Difference-2.2-2-2.7-2.6-2.1-3.8-4.4-3.2-4.5-3.5-1.5-2
Jan – JunJanFebMarAprMayJun
Hakuba3.33.13.93.94.46.3
Wrocław1.211.31.32.32.5
Difference-2.2-2-2.7-2.6-2.1-3.8
Jul – DecJulAugSepOctNovDec
Hakuba7.75.46.55.12.73.1
Wrocław3.32.121.61.21.1
Difference-4.4-3.2-4.5-3.5-1.5-2
Cloud cover (%) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba787573697180797076717277
Wrocław747369636567656364707474
Difference-4-2-3-5-6-13-13-7-11-1+2-3
Jan – JunJanFebMarAprMayJun
Hakuba787573697180
Wrocław747369636567
Difference-4-2-3-5-6-13
Jul – DecJulAugSepOctNovDec
Hakuba797076717277
Wrocław656364707474
Difference-13-7-11-1+2-3
Relative humidity (%) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba908782767579818183848588
Wrocław928983757267656471819092
Difference+2+2+1-1-3-12-16-16-12-4+4+4
Jan – JunJanFebMarAprMayJun
Hakuba908782767579
Wrocław928983757267
Difference+2+2+1-1-3-12
Jul – DecJulAugSepOctNovDec
Hakuba818183848588
Wrocław656471819092
Difference-16-16-12-4+4+4

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 → · Wrocław 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.

Wrocław

Temperature & precipitation — 1991–2020 normals computed from 20 years of daily observations at Strachowice, a weather station, about 10 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 →