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 →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.
NOAA LSA · regional trend · millimetres per year
The map is the NOAA Laboratory for Satellite Altimetry regional sea-level trend for 1992.96-2025.10, from the TOPEX, Jason, and Sentinel-6 reference series. The colour is millimetres per year. The global mean used on this site, about 3.7 millimetres per year in 2006-2018, is the IPCC AR6 figure. The NASA Sea Level Change Portal publishes that global mean as a time series, with the Sea Level Explorer and the AR6 projection tool.
One global number hides the places where the surface is rising faster or falling. Sea level is separate from surface temperature, salinity, and pollution.
Red is a faster rise. Blue is a slower rise or a fall. Currents, winds, and the vertical motion of the land make regional rates differ from the global mean. The NASA time series is the global average. This map is the regional rate over the altimeter record, not a single tide-gauge day and not a map of a future coastline.
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 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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