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Hakuba vs Glasgow

Cfa Humid subtropicalCfb Oceanic / temperate

Comparing Hakuba change · Glasgow change

Bottom line

Hakuba and Glasgow have nearly identical year-round temperatures; Hakuba is the wetter, with 175 mm more rain a year.

Year-round temp About the same within 1°C on the year
Wetter Hakuba 175 mm more a year
Sunnier About the same similar amount of sun
Colder winters Hakuba 9°C colder nights

How the seasons compare

The differences between Hakuba and Glasgow, in everyday terms.

Summers

Hakuba has far hotter summers

Hakuba: Warm
Glasgow: Mild

Winters

Glasgow has much milder winters

Hakuba: Very cold
Glasgow: Chilly

Rain & snow

Hakuba is wetter

Hakuba: Wet
Glasgow: Wet

Sky

Similar amounts of sun

Hakuba: Often grey
Glasgow: Often grey

Month-by-month charts

Temperature

Hakuba and Glasgow run remarkably close all year.

-20°20°40° JanAprJulOct HakubaGlasgow

Precipitation

Hakuba is the wetter — about 175 mm more across the year.

PRECIPITATION (mm) 0100200 JanAprJulOct HakubaGlasgow

Clear skies

The two cities see a similar amount of sun.

0%25%50%75%100% JanAprJulOct HakubaGlasgow

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) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba23715212427292418125
Glasgow781013161820191713107
Difference+6+5+3-2-5-5-7-9-7-5-2+2
Jan – JunJanFebMarAprMayJun
Hakuba237152124
Glasgow7810131618
Difference+6+5+3-2-5-5
Jul – DecJulAugSepOctNovDec
Hakuba27292418125
Glasgow20191713107
Difference-7-9-7-5-2+2
Avg low (°C) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba-8-7-3281317181471-4
Glasgow2235710121210741
Difference+9+9+7+3-1-3-5-6-4+3+5
Jan – JunJanFebMarAprMayJun
Hakuba-8-7-32813
Glasgow2235710
Difference+9+9+7+3-1-3
Jul – DecJulAugSepOctNovDec
Hakuba17181471-4
Glasgow121210741
Difference-5-6-4+3+5
Precipitation (mm) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba8578100981121591951361651297079
Glasgow1471111017263677790100134133136
Difference+62+33+1-26-48-92-118-46-65+5+63+57
Jan – JunJanFebMarAprMayJun
Hakuba857810098112159
Glasgow147111101726367
Difference+62+33+1-26-48-92
Jul – DecJulAugSepOctNovDec
Hakuba1951361651297079
Glasgow7790100134133136
Difference-118-46-65+5+63+57
Cloud cover (%) Varies through the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba787573697180797076717277
Glasgow777575737178787774757575
Difference-2-1+3+4+1-2-1+7-2+4+3-2
Jan – JunJanFebMarAprMayJun
Hakuba787573697180
Glasgow777575737178
Difference-2-1+3+4+1-2
Jul – DecJulAugSepOctNovDec
Hakuba797076717277
Glasgow787774757575
Difference-1+7-2+4+3-2
Relative humidity (%) Glasgow runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Hakuba908782767579818183848588
Glasgow959491888484868789929495
Difference+5+7+10+12+10+5+4+7+6+8+9+7
Jan – JunJanFebMarAprMayJun
Hakuba908782767579
Glasgow959491888484
Difference+5+7+10+12+10+5
Jul – DecJulAugSepOctNovDec
Hakuba818183848588
Glasgow868789929495
Difference+4+7+6+8+9+7

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 → · Glasgow 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.

Glasgow

Temperature & precipitation — 1991–2020 normals computed from 20 years of daily observations at Paisley, a weather station, about 11 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 →