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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 758 mm more rain a year, and Malmö the sunnier.

Year-round temp About the same within 1°C on the year
Wetter Hakuba 758 mm more a year
Sunnier Malmö 6 pp less cloud
Colder winters Hakuba 7°C 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°20°40° JanAprJulOct HakubaMalmö

Precipitation

Hakuba is the wetter — about 758 mm more across the year.

PRECIPITATION (mm) 0100200 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 (°C) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba23715212427292418125
Malmö4471216192222171274
Difference+2+2-1-3-4-5-5-7-7-5-4
Jan – JunJanFebMarAprMayJun
Hakuba237152124
Malmö447121619
Difference+2+2-1-3-4-5
Jul – DecJulAugSepOctNovDec
Hakuba27292418125
Malmö2222171274
Difference-5-7-7-5-4
Avg low (°C) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba-8-7-3281317181471-4
Malmö-0-014812141411741
Difference+7+7+4+2-1-3-4-3+3+5
Jan – JunJanFebMarAprMayJun
Hakuba-8-7-32813
Malmö-0-014812
Difference+7+7+4+2-1
Jul – DecJulAugSepOctNovDec
Hakuba17181471-4
Malmö141411741
Difference-3-4-3+3+5
Precipitation (mm) Hakuba runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba8578100981121591951361651297079
Malmö5737324042575256103486658
Difference-28-41-68-58-70-102-143-80-62-81-4-20
Jan – JunJanFebMarAprMayJun
Hakuba857810098112159
Malmö573732404257
Difference-28-41-68-58-70-102
Jul – DecJulAugSepOctNovDec
Hakuba1951361651297079
Malmö5256103486658
Difference-143-80-62-81-4-20
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 →