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Hakuba vs Malmö

Cfa Humid subtropicalCfb Oceanic / temperate

Comparing Hakuba change · Malmö change

Bottom line

Hakuba and Malmö have nearly identical year-round temperatures; Hakuba is the wetter, with 30 in more rain a year, and Malmö the sunnier.

Year-round temp About the same within 2°F on the year
Wetter Hakuba 30 in more a year
Sunnier Malmö 6 pp less cloud
Colder winters Hakuba 13°F colder nights

How the seasons compare

The differences between Hakuba and Malmö, in everyday terms.

Summers

Hakuba has much hotter summers

Hakuba: Warm
Malmö: Mild

Winters

Malmö has much milder winters

Hakuba: Very cold
Malmö: Cold

Rain & snow

Hakuba is wetter

Hakuba: Wet
Malmö: Moderate rainfall

Sky

Malmö is sunnier

Hakuba: Often grey
Malmö: Often cloudy

Month-by-month charts

Temperature

Hakuba and Malmö run remarkably close all year.

20°40°60°80° JanAprJulOct HakubaMalmö

Precipitation

Hakuba is the wetter — about 30 in more across the year.

PRECIPITATION (in) 048 JanAprJulOct HakubaMalmö

Clear skies

Malmö has the clearer skies — the higher line.

0%25%50%75%100% JanAprJulOct HakubaMalmö

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
Malmö394044536266717163544540
Difference+4+3-1-6-8-9-10-12-12-10-8-1
Jan – JunJanFebMarAprMayJun
Hakuba353745596975
Malmö394044536266
Difference+4+3-1-6-8-9
Jul – DecJulAugSepOctNovDec
Hakuba818375645341
Malmö717163544540
Difference-10-12-12-10-8-1
Avg low (°F) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba191926364756636457453425
Malmö323134404754585852453934
Difference+13+13+8+4+1-2-5-6-5+6+9
Jan – JunJanFebMarAprMayJun
Hakuba191926364756
Malmö323134404754
Difference+13+13+8+4+1-2
Jul – DecJulAugSepOctNovDec
Hakuba636457453425
Malmö585852453934
Difference-5-6-5+6+9
Precipitation (in) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba3.33.13.93.94.46.37.75.46.55.12.73.1
Malmö2.31.51.31.61.62.32.12.241.92.62.3
Difference-1.1-1.6-2.7-2.3-2.8-4-5.6-3.1-2.5-3.2-0.1-0.8
Jan – JunJanFebMarAprMayJun
Hakuba3.33.13.93.94.46.3
Malmö2.31.51.31.61.62.3
Difference-1.1-1.6-2.7-2.3-2.8-4
Jul – DecJulAugSepOctNovDec
Hakuba7.75.46.55.12.73.1
Malmö2.12.241.92.62.3
Difference-5.6-3.1-2.5-3.2-0.1-0.8
Cloud cover (%) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba787573697180797076717277
Malmö767569616062626366707677
Difference-3-1-4-8-11-18-17-7-10-1+4
Jan – JunJanFebMarAprMayJun
Hakuba787573697180
Malmö767569616062
Difference-3-1-4-8-11-18
Jul – DecJulAugSepOctNovDec
Hakuba797076717277
Malmö626366707677
Difference-17-7-10-1+4
Relative humidity (%) Malmö runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba908782767579818183848588
Malmö929188838180798083879193
Difference+3+4+6+7+6+1-2+3+6+5
Jan – JunJanFebMarAprMayJun
Hakuba908782767579
Malmö929188838180
Difference+3+4+6+7+6+1
Jul – DecJulAugSepOctNovDec
Hakuba818183848588
Malmö798083879193
Difference-2+3+6+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. Hakuba trends → · Malmö 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.

Malmö

Temperature & precipitation — 1991–2020 normals computed from 10 years of daily observations at Koebenhavn: Landbohojskolen-1, a weather station, about 31 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 →