Fossil fuel combustion is leading to higher temperatures worldwide. Local conditions on land and sea are determining which regions experience the most rapid warming.
Recently, Western Europe faced its second unprecedented heat wave in a month. This aligns with a concerning trend: Europe has been warming more rapidly than any other continent over the past 30 years.
Since the mid-1990s, the average temperatures in Europe have increased by about 1 degree Fahrenheit (0.56 degrees Celsius) per decade. This rate is more than twice the global average, according to data from Copernicus, the European Union’s climate monitoring service.
Human activities, including the emission of carbon dioxide and other greenhouse gases, are contributing to the long-term rise in global temperatures. These actions are intensifying the extremes in heat waves, affecting their severity and duration.
Several local factors influence the distribution of the excess heat and why some places warm faster than others. For example, in Europe’s northern regions, the warming atmosphere is causing the sea ice in the Arctic to melt. This exposes more of the ocean’s dark surface, which absorbs more solar energy and leads to additional warming in the Arctic area.
Pollution controls also play a role in Europe’s rapid heating. While the reduction of industrial emissions benefits air quality, it also reduces the concentration of aerosols—particles that help reflect solar radiation back into space.
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