
A significant heatwave is forecasted to impact Central Europe around 15 June 2025, with the GFS model from 00Z on 2 June 2025 indicating potential temperatures reaching +41°C at the tri-border area of Hungary, Slovakia, and Austria. This early summer event could rival or surpass historical records, posing substantial health and infrastructure risks.
As Central Europe faces a potentially historic early summer heatwave, the GFS forecast for 15 June 2025 highlights a critical synoptic setup dominated by a persistent blocking high-pressure ridge over Southwestern and Central Europe. This ridge facilitates the advection of intensely hot, dry Saharan air masses northward, producing 850 hPa temperatures exceeding +25°C, a hallmark of extreme continental heat.
The combination of strong atmospheric stability, clear skies, and adiabatic compression as the air descends into low-lying basins such as the Vienna Basin, Danubian Lowland, and Little Hungarian Plain is expected to amplify surface temperatures, with forecasts reaching 40–41°C—well above historical June records.
Early summer heatwaves have intensified across Central Europe in recent decades, pushing national June temperature records to unprecedented levels. Hungary currently holds a June record of 39.9°C, measured in Kiskunhalas on 20 June 2021, during a powerful early-season heatwave. Budapest also frequently records temperatures above 37°C in similar conditions, reflecting a broader warming trend.
In neighboring Slovakia, the June temperature record stands at 38.8°C, registered in Hurbanovo on the same day—20 June 2021. Western and southern parts of the country are particularly vulnerable to early summer heat, with frequent highs above 36°C during events in June 2012, 2019, and 2021. These extremes challenge infrastructure and public health systems even before the peak summer season begins.
Austria reached its highest June temperature of 38.6°C in Bad Deutsch-Altenburg, again on 20 June 2021. This city also holds Austria’s overall national record of 40.5°C (from August 2013), underlining its status as a national heat hotspot. The June 2019 and 2021 heatwaves affected large swaths of the country, especially the eastern lowlands.
Czechia’s June record was set in Doksany, where the mercury hit 38.9°C on 26 June 2019. That year marked the hottest June in Czech history. Cities like Prague and Brno also approached or exceeded 37°C, with widespread agricultural and ecological stress reported due to prolonged heat and drought.
Poland recorded its highest June temperature—38.2°C—in Radzyń on 26 June 2019, part of the same continental heatwave that gripped much of Europe. Numerous Polish cities, including Warsaw and Kraków, reported temperatures in the 36–37.5°C range, illustrating how early heat extremes are becoming more common even in traditionally milder climates.
In Germany and Switzerland, the same June 2019 heatwave set national records of 39.6°C in Coschen (Germany) and 37.0°C in Beznau/Sion (Switzerland). These extremes occurred during one of the most intense early summer heat events in European history, surpassing many July and August records in some regions. If current forecasts for mid-June 2025 prove accurate, many of these national records—especially in the Danube basin—could be under serious threat.
Here are more June temperature records for the countries mentioned, highlighting extreme early-summer heat events across Central Europe in recent decades:
Here is a clear and compact table of national June temperature records for Central European countries:
Country | June Record Temp | Location | Date |
---|---|---|---|
Hungary | 39.9°C | Kiskunhalas | 20 June 2021 |
Slovakia | 38.8°C | Hurbanovo | 20 June 2021 |
Austria | 38.6°C | Bad Deutsch-Altenburg | 20 June 2021 |
Czechia | 38.9°C | Doksany | 26 June 2019 |
Poland | 38.2°C | Radzyń | 26 June 2019 |
Germany | 39.6°C | Coschen (Brandenburg) | 30 June 2019 |
Switzerland | 37.0°C | Beznau / Sion | 27–28 June 2019 |
Hypothetical Maximum Temperatures on 15 June 2025
Assuming the GFS forecast materializes, the following are projected maximum temperatures for major cities with populations over 100,000:
Country | City | Projected Max Temp |
---|---|---|
Hungary | Budapest | 41°C |
Slovakia | Bratislava | 40°C |
Austria | Vienna | 40°C |
Czechia | Brno | 39°C |
Poland | Kraków | 38°C |
Germany | Munich | 37°C |
Switzerland | Zurich | 36°C |
These temperatures would represent unprecedented early summer highs for many of these locations.

Abnormal heat for Hungary / Slovakia / Austria for 15. June 2025 from GFS. Source: https://www.wetterzentrale.de/en/topkarten.php?map=3&model=gfs&var=5&time=324&run=0&lid=OP&h=0&mv=0&tr=6

Temperature in 850 hPa in the region. Source: https://www.wetterzentrale.de/en/topkarten.php?map=3&model=gfs&var=2&time=324&run=0&lid=OP&h=0&mv=0&tr=6
Synoptic Evolution (1–15 June 2025)
- 1–5 June 2025: The GFS model shows relatively normal conditions across Central Europe, with alternating weak troughs and ridges. The pattern is progressive, allowing some Atlantic influence to bring cooler interludes.
- 6–10 June: A persistent upper-level ridge begins to build over Southwestern Europe, centered over Spain, France, and Northern Africa. This ridge cuts off Atlantic lows from entering the continent and begins drawing hot Saharan air northward via southerly and southeasterly winds.
- 11–13 June: The ridge strengthens and expands northeastward over Italy, the Balkans, and the Carpathian Basin. At the same time, a cut-off low over the eastern Atlantic creates a pressure gradient that intensifies southerly wind flow. This accelerates the transport of hot air masses from the Sahara through the Mediterranean, across the Adriatic and Pannonian Basin, directly into Austria, Hungary, and Slovakia.
- 14–15 June: The heat dome becomes fully established, with 850 hPa temperatures exceeding +25°C across the region. These values, unusually high for mid-June, are more typical of July–August heatwaves. Surface temperatures are projected to reach 40–41°C in lowland areas, especially along the Danube and the Vienna–Bratislava–Győr corridor.
The imported Saharan air should be:
- Extremely dry at mid and upper levels, which prevents cloud formation and allows maximum solar heating of the ground.
- Warm at 850 hPa, ensuring that the warmth is not just surface-based but deeply rooted.
- Often associated with a dusty component, though the degree of dust transport depends on the wind trajectories across the Mediterranean.
As the air crosses the Alps and Carpathians, it undergoes adiabatic compression (warming by sinking), which enhances temperatures further in valleys and basins like:
- The Vienna Basin
- The Little Hungarian Plain
- The Danubian Lowland
These regions are historically prone to heat extremes due to geographic and climatic factors that amplify hot air stagnation.
Such extreme thermal anomalies pose severe risks including heat-related morbidity and mortality, energy grid stress due to peak cooling demands, agricultural drought stress, and water resource depletion. The urban heat island effect may further exacerbate impacts in major population centers.
This event exemplifies the influence of blocking patterns and persistent ridges in driving prolonged heatwaves, phenomena that are increasing in frequency and intensity under anthropogenic climate change.
Urgent meteorological monitoring, early warning dissemination, and implementation of heat mitigation strategies—including public health advisories and infrastructure resilience—are imperative to reduce adverse impacts.
This forecast serves as a clear meteorological signal: extreme early summer heatwaves are becoming more common, demanding enhanced preparedness and adaptive capacity across (not only) Central Europe.