The daily global average sea surface temperature for extra-polar oceans reached 21.1 degrees Celsius on 21 and 22 August 2026, the highest on record.
Extra-polar oceans are defined as waters between 60 degrees South and 60 degrees North, excluding the polar seas.
The previous record was 21.09 degrees Celsius, set on 1 March 2024.
Global sea surface temperatures normally peak in March or April, making an August record unusual.
A strengthening El Nino, on top of decades of greenhouse-gas-driven warming, is driving the anomaly.
Sea surface temperature (SST) is the temperature of the uppermost layer of the ocean, measured by satellites, moored and drifting buoys, and ship-based observations. Global SST records are usually quoted for the extra-polar belt — waters between 60 degrees South and 60 degrees North — because the polar seas are ice-covered for much of the year and their seasonal swings would otherwise dominate the global average and mask the trend in the open ocean. That belt still contains most of the world's major marine ecosystems and fisheries, so it is the meaningful measure for ecological impact.
Simple Analogy: It is like reporting a country's average temperature while leaving out its two ice caps — the number then reflects where people and crops actually are.
The European Union's climate monitoring programme, which produces the reanalysis datasets used to identify global temperature records
The United States federal agency responsible for oceanic and atmospheric monitoring and forecasting
GS Paper I > Geography: Important geophysical phenomena; GS Paper III > Conservation and environmental degradation
General Awareness > Current Affairs > Environment
General Awareness > Current Affairs
Which of the following is not typically considered a weather element?
Answer: Soil pH
The temperature of the uppermost layer of the ocean, measured by satellites, buoys and ship-based observations.
Ocean waters between 60 degrees South and 60 degrees North, excluding the polar seas — the belt used for global SST records.
The warm phase of the El Nino-Southern Oscillation, a periodic warming of the central and eastern tropical Pacific Ocean.
A prolonged period of unusually high ocean temperatures over a given region.
The loss of symbiotic algae by corals under thermal stress, leaving them white and vulnerable to death.