Ursula Meer
· 09.09.2026
The North Sea and the Baltic Sea remain too warm. As recently as last year, the Federal Maritime and Hydrographic Agency (BSH) had classified the summer of 2025, with an average temperature of 15.7 degrees Celsius, as the warmest in the North Sea since records began in 1969. This figure was not reached in 2026. Nevertheless, according to a new report from the BSH, temperatures this summer were also just under one degree above the long-term average. Off the coast of Heligoland, a new record was set with 66 days of marine heatwaves.
The Water temperatures in the North Sea and the Baltic Sea From June to August 2026, temperatures were just under one degree above the average for the years 1997 to 2021. In the North Sea, the average surface temperature reached 15.6 degrees Celsius. This was the fifth-warmest summer since 1997. The Baltic Sea reached 17.2 degrees Celsius, ranking seventh amongst the summers recorded since 1997.
The figures are taken from the latest summer report by the Federal Maritime and Hydrographic Agency. They are slightly lower than last year’s figures, when new temperature records were set in the North Sea and the Baltic Sea.
The waters around Heligoland were among the regions of the North Sea that had warmed the most. On 1 July 2026, the surface temperature at the measuring station there was in fact almost four degrees above the average for that day since the station began operating in 2009.
But it is not just this one peak value that is remarkable: at the monitoring station off Heligoland, the BSH recorded 66 days of marine heatwaves – that is, periods of at least five days with water temperatures that were unusually warm for the location and time of year. By way of comparison: in the spring of 2025, the BSH’s ‘Leuchtturm Kiel’ measuring station in the Baltic Sea had recorded 55 days as the previous record.
According to forecasts, marine heatwaves are set to become more frequent in all the world’s oceans. As warmer water can dissolve less oxygen, living conditions for marine life may deteriorate. This will have particularly serious consequences for the Baltic Sea: on the seabed of this already ailing inland sea, oxygen-depleted ‘dead zones’ may also become more common.
The southern North Sea was the warmest. There, and in the English Channel, temperature anomalies reached two degrees or more, with some areas recording their highest temperatures since 1997. For around a quarter of the North Sea, temperatures were among the three highest of the last 30 years.
Tim Kruschke, Head of the Marine Climate Issues Unit at the BSH, emphasised that the new record highs in the southern North Sea and the 66 days of marine heatwaves off Heligoland indicate that extreme heat events are also becoming increasingly noticeable in German waters. Although the North Sea and the Baltic Sea are not affected to the same extent as, for example, the Mediterranean or the north-east Atlantic, temperatures in many places were among the highest recorded in recent decades.
Temperatures in the Baltic Sea were not consistent. June, in particular, stood out, being almost three degrees above the long-term average; according to the BSH, it was the third-warmest June since records began. In July and August, however, temperatures were generally within the average range.
The greatest positive anomalies were measured off the east coast of Sweden, along the German and Polish coasts, and in the far north of the Baltic Sea. IIn late summer, this could even be seen with the naked eye: large patches of blue-green algae were floating in the southern and western parts of the Baltic Sea, and in some cases also in harbours around Bornholm.
Warmer seas do not necessarily lead to severe weather. However, they can contribute to “rising sea levels, because warm water expands and glaciers and ice sheets melt. This also causes water levels to rise during storm surges.”A warm summer does not, therefore, automatically lead to a stormy autumn or winter. Many factors interact in the formation and intensification of low-pressure systems, including air pressure distribution, high-altitude winds and the temperature difference between air masses.
Warming also supplies additional energy and moisture to the atmosphere. The European climate service Copernicus points out that high sea surface temperatures can increase evaporation and, consequently, the potential for heavy rainfall. It is not possible to determine from this how significantly this affects any individual weather event. The current forecasts, radar data and warning information prior to setting sail remain crucial.
Warmer seas are more than just a meteorological observation. The warming of the seas can have far-reaching consequences. For instance, warmer water alters habitats and food chains. Whilst some species are losing habitat at a drastic rate, others are migrating to cooler waters. Furthermore, non-native species are spreading, which can lead to an increase in harmful algal blooms and a lack of oxygen.
This is particularly critical for the Baltic Sea: when large quantities of dead algae sink to the seabed, microorganisms consume oxygen as they break them down, until there is hardly any left dissolved in the deep water. Other substances, such as ammonium, increase in concentration, and with them microorganisms that can carry out their metabolic processes without oxygen. In doing so, they produce hydrogen sulphide, which is toxic to many organisms – this results in ‘dead zones’ where higher life forms can no longer survive on the seabed.
The persistently high temperatures are also fuelling the growth of blue-green algae in coastal regions. Blue-green algae can produce toxins and are not entirely harmless to humans and animals: if swallowed or if there is contact with contaminated water, they can cause skin irritation, gastrointestinal complaints and, in severe cases, liver or nerve damage. Sailors out on the Baltic Sea in summer are advised to check the latest algae reports – swimming bans may be imposed at short notice.
Heavy-weather sailing explains how sailing yachts, motor yachts, monohulls and multihulls behave in heavy seas. The theory and technical section covers, amongst other things, equipment, trysails, and sea anchors and drift anchors. In the practical section, reports on heavy-weather situations are analysed and translated into specific tactics. This ties in with the article, as reliable preparation and the correct response to the current weather conditions are more important than drawing a sweeping conclusion based on warm seawater.
Weather at sea covers the basics of meteorology for cruising and regatta sailors. The book covers low- and high-pressure systems, local and regional weather events, sea states, currents and meteorological trip planning. It thus complements the ‘Summer Review’ by addressing the practical question of how skippers can interpret weather information and use it to make their own route decisions.
How did you find the unusually warm water temperatures in the North Sea or the Baltic Sea this summer?

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