Question

What is a carbon sink, and how much CO₂ do the oceans absorb?

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Answer

A carbon sink is any reservoir absorbing more carbon than it releases. The two dominant natural sinks are the ocean and land vegetation and soils, and together they absorb roughly half of human CO₂ emissions each year.

The ocean sink takes up around a quarter of annual emissions. It works through two mechanisms:

The solubility pump. CO₂ dissolves in seawater, more readily in cold water. Cold, dense water sinking at high latitudes carries dissolved carbon into the deep ocean, where it can remain for centuries.

The biological pump. Phytoplankton take up CO₂ through photosynthesis. When they die, a fraction sinks as particulate matter, transporting carbon to depth.

The land sink absorbs a further quarter or so, through forest growth, soil carbon and the CO₂ fertilisation effect — plants growing somewhat faster in a higher-CO₂ atmosphere.

Why this matters enormously. Without these sinks, atmospheric CO₂ would be rising roughly twice as fast. They are doing an unpaid service of extraordinary scale.

The costs and the concerns:

Ocean acidification is the direct chemical consequence. Dissolved CO₂ forms carbonic acid, and ocean pH has fallen measurably since industrialisation — a roughly 30% increase in hydrogen ion concentration. This impairs organisms building calcium carbonate shells and skeletons: corals, molluscs, and some plankton at the base of marine food webs. It is sometimes called the other CO₂ problem, and it proceeds regardless of temperature.

Sinks may weaken. Warmer water holds less dissolved gas. Forests stressed by drought, fire and pests absorb less, and can become net sources — parts of the Amazon have been measured emitting more than they absorb in some years. Thawing permafrost releases stored carbon.

Saturation. The fraction of emissions absorbed is not guaranteed to hold.

Blue carbon — mangroves, saltmarsh and seagrass — stores carbon very densely per hectare.

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