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🇸🇰Slovakia

3 cities

Climate overview

Slovakia (49,035 km²) lies in Central Europe between 47°44′–49°37′N and 16°50′–22°34′E, encompassing a diverse topography that profoundly shapes its temperate continental climate. The Carpathian mountain arc dominates the northern half, with the High Tatras reaching 2,655 m at Gerlachovský štít (the highest peak in the Carpathians), creating steep altitudinal climate gradients and orographic precipitation exceeding 1,400 mm annually on windward slopes.

The southern lowlands—primarily the fertile Danube basin and East Slovak Lowland—descend to 94 m at the Bodrog River, experiencing warmer, drier conditions with 500–650 mm annual precipitation concentrated in summer convective storms. Slovakia's continental position produces marked seasonal extremes: mean January temperatures range from -3°C in valleys to below -10°C at high elevations, while July averages 19–21°C in lowlands.

The Köppen classification is predominantly Dfb (warm-summer humid continental) in lowlands transitioning to Dfc (subarctic) above 1,200 m and ET (tundra) on High Tatras summits. Blocking high-pressure systems over Eastern Europe drive winter cold spells with temperatures plunging below -30°C, while Mediterranean air masses occasionally push summer maxima above 38°C in the Danube basin.

Bratislava (Danube lowland, 134 m elevation) averages 0°C in January and 21°C in July with 565 mm annual precipitation, experiencing a moderating western Atlantic influence. Košice (eastern valleys, 206 m) records -2°C in January and 20°C in July with 600 mm, showing slightly more continental character with colder winters.

The November 2004 High Tatras windstorm caused winds exceeding 200 km/h, flattening 12,000 hectares of forest (2.5 million cubic meters of timber) and triggering bark beetle outbreaks. The July 2010 Eastern Slovakia floods killed seven people and displaced 15,000 when 150–200 mm fell in 48 hours across the Hornád and Bodrog basins, causing €280 million in damages.

The June–August 2022 Central European heatwave saw Hurbanovo reach 39.3°C (equaling Slovakia's 2007 record), while Bratislava recorded 21 consecutive tropical nights (>20°C minimum). Accelerating climate change has driven rapid snowpack decline in the Tatras—April snow depth at Lomnický štít decreased 35% between 1961 and 2020, shortening the ski season by three weeks and threatening alpine ecosystems. Observations document mean annual temperatures rising 2.1°C since 1951, exceeding the global average rate.

Our archive covers 3 Slovak cities with daily ERA5 reanalysis data going back to 1940. The warmest July averages occur in Petržalka, around 26.3°C, while Košice records the coldest January nights near −5.8°C. Comparing the last decade against the 1940–1970 baseline, mean temperatures across these cities have risen by about 2.2°C.

Sources:Climate Change 2022: Impacts, Adaptation and Vulnerability - Chapter 13: EuropeClimate of Slovakia - SHMU Climate AtlasEuropean State of the Climate 2022 - Central Europe2004 High Tatras windstormClimate change in Slovakia: Observed and projected changes

How the climate has shifted in Slovakia

Average across 3 cities with full ERA5 coverage — 1940–1970 baseline vs the last decade (2016–2025).

+2.2°Cwarmer than the 1940–1970 baseline
Annual mean temperature
9.5°C11.8°C
Days above 30°C per year
9 days26 days+17
Frost days per year
98 days66 days−32
Tropical nights (≥20°C) per year
2 nights7 nights+5

Warmest year in the record so far: 2024.

What's unusual right now

From a snapshot of the world's largest cities updated each hour. Today's mean temperature compared with each city's long-term average for the same calendar date (ERA5 climatology, 1940 onward). Last 30 days uses each city's rolling daily-mean vs its monthly average. Not a global ranking.

Coolest in Slovakia right now

From a snapshot of the world's largest cities updated each hour. Not a global ranking.

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