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Bormio vs Bergen

Dfb Warm-summer humid continentalCfb Oceanic / temperate

Comparing Bormio change · Bergen change

Bottom line

Bergen is the warmer of the two — about 3°C on the annual average; Bergen is the wetter, with 2039 mm more rain a year, and Bormio the sunnier.

Warmer Bergen 3°C on the year
Wetter Bergen 2039 mm more a year
Sunnier Bormio 10 pp less cloud
Colder winters Bormio 7°C colder nights

How the seasons compare

The differences between Bormio and Bergen, in everyday terms.

Summers

Summers are nearly the same

Bormio: Mild
Bergen: Mild

Winters

Bergen has much milder winters

Bormio: Very cold
Bergen: Chilly

Rain & snow

Bergen is much wetter

Bormio: Fairly dry
Bergen: Very wet

Sky

Bormio is sunnier

Bormio: Often cloudy
Bergen: Often grey

Month-by-month charts

Temperature

Bergen is the warmer of the two — about 3°C on the annual average.

-20°-10°10°20°30° JanAprJulOct BormioBergen

Precipitation

Bergen is the wetter — about 2039 mm more across the year.

PRECIPITATION (mm) 0145290 JanAprJulOct BormioBergen

Clear skies

Bormio has the clearer skies — the higher line.

0%25%50%75%100% JanAprJulOct BormioBergen

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
Bormio2371114192020161262
Bergen5571115182019161285
Difference+3+2+1+1-1-1-1+2+3
Jan – JunJanFebMarAprMayJun
Bormio237111419
Bergen557111518
Difference+3+2+1+1-1
Jul – DecJulAugSepOctNovDec
Bormio2020161262
Bergen2019161285
Difference-1-1+2+3
Avg low (°C) Bergen runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Bormio-7-6-3159101073-1-5
Bergen1014710121210631
Difference+7+7+4+3+2+2+2+2+3+3+4+6
Jan – JunJanFebMarAprMayJun
Bormio-7-6-3159
Bergen1014710
Difference+7+7+4+3+2+2
Jul – DecJulAugSepOctNovDec
Bormio101073-1-5
Bergen121210631
Difference+2+2+3+3+4+6
Precipitation (mm) Bergen runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Bormio201519203254727450453422
Bergen252209202138109132158208251275272288
Difference+232+195+183+118+77+78+86+134+201+230+238+266
Jan – JunJanFebMarAprMayJun
Bormio201519203254
Bergen252209202138109132
Difference+232+195+183+118+77+78
Jul – DecJulAugSepOctNovDec
Bormio727450453422
Bergen158208251275272288
Difference+86+134+201+230+238+266
Cloud cover (%) Bergen runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Bormio626568727470646364646664
Bergen817978726873777677788081
Difference+19+14+10-1-5+2+13+13+13+14+14+17
Jan – JunJanFebMarAprMayJun
Bormio626568727470
Bergen817978726873
Difference+19+14+10-1-5+2
Jul – DecJulAugSepOctNovDec
Bormio646364646664
Bergen777677788081
Difference+13+13+13+14+14+17
Relative humidity (%) Bergen runs higher most of the year
JanFebMarAprMayJunJulAugSepOctNovDec
Bormio889090837979798183848888
Bergen949491848080828487909395
Difference+7+4+1+1+1+3+3+4+6+5+7
Jan – JunJanFebMarAprMayJun
Bormio889090837979
Bergen949491848080
Difference+7+4+1+1+1
Jul – DecJulAugSepOctNovDec
Bormio798183848888
Bergen828487909395
Difference+3+3+4+6+5+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. Bormio trends → · Bergen trends →

Methodology & sources

Bormio

Temperature & precipitation — the official 1991–2020 climate normals from the WMO's CLINO 1991–2020 collection, measured at San_valentino_alla_muta, about 38 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.

Bergen

Temperature & precipitation — 1991–2020 normals computed from 30 years of daily observations at Bergen Florida, a weather station, about 1 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 →