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Grindelwald vs Hakuba

Cfb Oceanic / temperateCfa Humid subtropical

Comparing Grindelwald change · Hakuba change

Bottom line

Grindelwald and Hakuba have nearly identical year-round temperatures; Hakuba is the wetter, with 228 mm more rain a year, and Grindelwald the sunnier.

Year-round temp About the same within 1°C on the year
Wetter Hakuba 228 mm more a year
Sunnier Grindelwald 8 pp less cloud
Colder winters Hakuba 5°C colder nights

How the seasons compare

The differences between Grindelwald and Hakuba, in everyday terms.

Summers

Hakuba has much hotter summers

Grindelwald: Mild
Hakuba: Warm

Winters

Grindelwald has milder winters

Grindelwald: Cold
Hakuba: Very cold

Rain & snow

Hakuba is wetter

Grindelwald: Wet
Hakuba: Wet

Sky

Grindelwald is sunnier

Grindelwald: Often cloudy
Hakuba: Often grey

Month-by-month charts

Temperature

Grindelwald and Hakuba run remarkably close all year.

-20°20°40° JanAprJulOct GrindelwaldHakuba

Precipitation

Hakuba is the wetter — about 228 mm more across the year.

PRECIPITATION (mm) 0100200 JanAprJulOct GrindelwaldHakuba

Clear skies

Grindelwald has the clearer skies — the higher line.

0%25%50%75%100% JanAprJulOct GrindelwaldHakuba

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
Grindelwald35111519222424191484
Hakuba23715212427292418125
Difference-2-3-3+2+1+3+5+5+4+4+1
Jan – JunJanFebMarAprMayJun
Grindelwald3511151922
Hakuba237152124
Difference-2-3-3+2+1
Jul – DecJulAugSepOctNovDec
Grindelwald2424191484
Hakuba27292418125
Difference+3+5+5+4+4+1
Avg low (°C) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Grindelwald-3-31481214141061-2
Hakuba-8-7-3281317181471-4
Difference-5-5-4-2+1+4+4+4+1-2
Jan – JunJanFebMarAprMayJun
Grindelwald-3-314812
Hakuba-8-7-32813
Difference-5-5-4-2+1
Jul – DecJulAugSepOctNovDec
Grindelwald14141061-2
Hakuba17181471-4
Difference+4+4+4+1-2
Precipitation (mm) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Grindelwald7267738212212714614694808091
Hakuba8578100981121591951361651297079
Difference+13+12+27+16-10+33+50-10+71+49-10-12
Jan – JunJanFebMarAprMayJun
Grindelwald72677382122127
Hakuba857810098112159
Difference+13+12+27+16-10+33
Jul – DecJulAugSepOctNovDec
Grindelwald14614694808091
Hakuba1951361651297079
Difference+50-10+71+49-10-12
Cloud cover (%) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Grindelwald686968697265595961667171
Hakuba787573697180797076717277
Difference+10+7+4-1+15+19+11+15+5+1+6
Jan – JunJanFebMarAprMayJun
Grindelwald686968697265
Hakuba787573697180
Difference+10+7+4-1+15
Jul – DecJulAugSepOctNovDec
Grindelwald595961667171
Hakuba797076717277
Difference+19+11+15+5+1+6
Relative humidity (%) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Grindelwald868687848178777881838786
Hakuba908782767579818183848588
Difference+4+1-6-8-6+1+4+3+2+1-2+2
Jan – JunJanFebMarAprMayJun
Grindelwald868687848178
Hakuba908782767579
Difference+4+1-6-8-6+1
Jul – DecJulAugSepOctNovDec
Grindelwald777881838786
Hakuba818183848588
Difference+4+3+2+1-2+2

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. Grindelwald trends → · Hakuba trends →

Methodology & sources

Grindelwald

Temperature & precipitation — the official 1991–2020 climate normals from a national meteorological service, measured at Interlaken, about 14 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.

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 →