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 →Sea-ice concentration for a recent Arctic March and Antarctic September, side by side. Frozen ocean cover, not surface temperature and not land ice.
NSIDC G02135 · concentration · Arctic March 2026 · Antarctic September 2025
The map is monthly sea-ice concentration from the NSIDC Sea Ice Index, dataset G02135 version 4. The left panel is the Arctic in March 2026. The right panel is the Antarctic in September 2025. The number is percent concentration. Sea Ice Today remains the public discussion of extent, which is the ocean area with at least 15 percent ice, set against a 1981-2010 median.
Surface temperature is a different measurement. Sea ice is frozen seawater. It reflects sunlight and follows its own calendar: the Arctic is near its maximum in March and its minimum in September, and the Antarctic is roughly the other way around. It is not glacier or ice-sheet mass on land.
Lighter colour is higher concentration. Dark blue is open water or very little ice. Land is the NSIDC mask. Extent, the area above 15 percent, is a separate summary in the Sea Ice Index time series. Read the Arctic and Antarctic panels as two seasons, not as one global average.
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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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.
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Heat stored in the upper 700 metres in 2025, as an anomaly in each 1° cell, from NOAA NCEI.
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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