Ocean acidification
How much surface-ocean pH changed from the late 1980s to the early 2020s. A carbonate-chemistry trend, not temperature and not a pollution map.
Read the card →Heat stored in the upper 700 metres in 2025, as an anomaly in each 1° cell, from NOAA NCEI.
NOAA NCEI · 0-700 m anomaly · 2025
The map is the NOAA NCEI yearly ocean heat content anomaly for 0-700 m in 2025. The number is 10¹⁸ joules in each 1° cell, calculated from temperature profiles. NCEI also publishes a 0-2000 m series. NASA and Climate.gov explain the global total over time. Mercator Ocean offers a European view of the same idea.
About 90 percent of the excess heat in the climate system is stored in the ocean (IPCC AR6). Sea-surface temperature describes only the top. This map shows where the upper 700 metres held more or less heat than the long-term reference in 2025.
The colour is the 2025 anomaly in the upper 700 metres. It is not sea-surface temperature and not the 0-2000 m layer. Deeper layers have been measured well for a shorter time, with the strongest coverage since the Argo float era. NASA and Climate.gov show the global total as a time series.
How much surface-ocean pH changed from the late 1980s to the early 2020s. A carbonate-chemistry trend, not temperature and not a pollution map.
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The lowest dissolved oxygen between 100 and 1000 metres in the World Ocean Atlas 2023 climatology. Open-ocean oxygen, not the coastal dead-zone pins on Pollution.
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Sea-ice concentration for a recent Arctic March and Antarctic September, side by side. Frozen ocean cover, not surface temperature and not land ice.
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Where the ocean surface is rising faster or more slowly, in millimetres per year. The global average cited on this site comes from the NASA Sea Level Change Portal.
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Where the sea surface was warmer or cooler than usual on 25 September 2026. A temperature anomaly from NOAA Coral Reef Watch, not a classified heatwave category.
Read the card →Where hard coral cover stands today and how heat stress bleaches reefs, based on global monitoring and satellite observations.
Read the card →How assessed marine fish stocks are doing worldwide, according to FAO’s global stock-status figures.
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Surface currents and the great gyres that steer heat, salt, and life.
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How salty the sea is, and why that density helps drive the overturning circulation.
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The temperature of the sea surface: the standing climate, and years that run warmer or cooler.
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Five subtropical garbage patches, oil, phytoplankton blooms, and coastal dead zones.
Read the card →Heat, acidity, plastic, and hypoxia, each from a named paper.
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