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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 876 mm more rain a year.

Year-round temp About the same within 1°C on the year
Wetter Hakuba 876 mm more a year
Sunnier Wrocław 6 pp less cloud
Colder winters Hakuba 3°C 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°20°40° JanAprJulOct HakubaWrocław

Precipitation

Hakuba is the wetter — about 876 mm more across the year.

PRECIPITATION (mm) 0100200 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 (°C) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba23715212427292418125
Wrocław2591520232525201584
Difference+1+2+1-1-1-2-4-4-3-3-1
Jan – JunJanFebMarAprMayJun
Hakuba237152124
Wrocław259152023
Difference+1+2+1-1-1
Jul – DecJulAugSepOctNovDec
Hakuba27292418125
Wrocław2525201584
Difference-2-4-4-3-3-1
Avg low (°C) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba-8-7-3281317181471-4
Wrocław-4-3-1481113121051-3
Difference+3+4+3+2-1-2-4-6-4-2+1
Jan – JunJanFebMarAprMayJun
Hakuba-8-7-32813
Wrocław-4-3-14811
Difference+3+4+3+2-1-2
Jul – DecJulAugSepOctNovDec
Hakuba17181471-4
Wrocław13121051-3
Difference-4-6-4-2+1
Precipitation (mm) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba8578100981121591951361651297079
Wrocław292632335864845450413128
Difference-55-52-68-65-53-96-112-82-115-88-39-51
Jan – JunJanFebMarAprMayJun
Hakuba857810098112159
Wrocław292632335864
Difference-55-52-68-65-53-96
Jul – DecJulAugSepOctNovDec
Hakuba1951361651297079
Wrocław845450413128
Difference-112-82-115-88-39-51
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 →