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Prague vs Hakuba

Cfb Oceanic / temperateCfa Humid subtropical

Comparing Prague change · Hakuba change

Bottom line

Prague and Hakuba have nearly identical year-round temperatures; Hakuba is the wetter, with 32 in more rain a year.

Year-round temp About the same within 2°F on the year
Wetter Hakuba 32 in more a year
Sunnier About the same similar amount of sun
Colder winters Hakuba 8°F colder nights

How the seasons compare

The differences between Prague and Hakuba, in everyday terms.

Summers

Hakuba has hotter summers

Prague: Mild
Hakuba: Warm

Winters

Prague has milder winters

Prague: Cold
Hakuba: Very cold

Rain & snow

Hakuba is much wetter

Prague: Moderate rainfall
Hakuba: Wet

Sky

Similar amounts of sun

Prague: Often cloudy
Hakuba: Often grey

Month-by-month charts

Temperature

Prague and Hakuba run remarkably close all year.

20°40°60°80° JanAprJulOct PragueHakuba

Precipitation

Hakuba is the wetter — about 32 in more across the year.

PRECIPITATION (in) 048 JanAprJulOct PragueHakuba

Clear skies

The two cities see a similar amount of sun.

0%25%50%75%100% JanAprJulOct PragueHakuba

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) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Prague364048596873777767574537
Hakuba353745596975818375645341
Difference-1-3-3+1+1+4+6+7+7+8+3
Jan – JunJanFebMarAprMayJun
Prague364048596873
Hakuba353745596975
Difference-1-3-3+1+1
Jul – DecJulAugSepOctNovDec
Prague777767574537
Hakuba818375645341
Difference+4+6+7+7+8+3
Avg low (°F) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Prague272732404753575649413428
Hakuba191926364756636457453425
Difference-8-8-6-4-1+2+7+9+8+4-1-3
Jan – JunJanFebMarAprMayJun
Prague272732404753
Hakuba191926364756
Difference-8-8-6-4-1+2
Jul – DecJulAugSepOctNovDec
Prague575649413428
Hakuba636457453425
Difference+7+9+8+4-1-3
Precipitation (in) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Prague1.71.61.21.42.83.42.92.81.81.51.11
Hakuba3.33.13.93.94.46.37.75.46.55.12.73.1
Difference+1.6+1.5+2.8+2.5+1.6+2.8+4.8+2.5+4.7+3.6+1.6+2.1
Jan – JunJanFebMarAprMayJun
Prague1.71.61.21.42.83.4
Hakuba3.33.13.93.94.46.3
Difference+1.6+1.5+2.8+2.5+1.6+2.8
Jul – DecJulAugSepOctNovDec
Prague2.92.81.81.51.11
Hakuba7.75.46.55.12.73.1
Difference+4.8+2.5+4.7+3.6+1.6+2.1
Cloud cover (%) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Prague777573676971686566737777
Hakuba787573697180797076717277
Difference+1-1+2+2+9+10+5+10-2-5
Jan – JunJanFebMarAprMayJun
Prague777573676971
Hakuba787573697180
Difference+1-1+2+2+9
Jul – DecJulAugSepOctNovDec
Prague686566737777
Hakuba797076717277
Difference+10+5+10-2-5
Relative humidity (%) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Prague928983767268646471819093
Hakuba908782767579818183848588
Difference-3-2-1+3+11+17+17+11+3-5-5
Jan – JunJanFebMarAprMayJun
Prague928983767268
Hakuba908782767579
Difference-3-2-1+3+11
Jul – DecJulAugSepOctNovDec
Prague646471819093
Hakuba818183848588
Difference+17+17+11+3-5-5

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. Prague trends → · Hakuba trends →

Methodology & sources

Prague

Temperature & precipitation — 1991–2020 normals computed from 24 years of daily observations at Praha-libus, 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.

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.

How we build these numbers →