The distribution of the Earth's water
About 97% is salt water; only about 3% is fresh, and most of that is frozen or deep underground.
The Earth is often called the "blue planet", but very little of its water is usable fresh water. About 97% of the Earth's water is salt water in the oceans, and only about 3% is fresh water. Crucially, most of that fresh water is not easily accessible: the large majority is locked up in ice sheets and glaciers or stored deep underground as groundwater, leaving only a very small fraction in the lakes and rivers we most easily use.
The syllabus groups water into four stores:
- Salt water — the oceans, holding about 97% of all water; too saline to drink or irrigate with directly.
- Surface fresh water — ice sheets, glaciers, lakes, rivers, swamps and marshes, and permafrost. The ice and glaciers hold most of the fresh water, while lakes and rivers (the water we use most) are a tiny share.
- Sub-surface fresh water — soil moisture, ground water (water held in rocks called aquifers), and permafrost. Groundwater is a major store and the source of borehole and well water.
- Atmospheric water — water vapour and clouds in the air; a small store but vital because it drives the water cycle and rainfall.
The big idea: although water seems abundant, the share that is fresh, liquid and accessible is tiny — which is why fresh water is a limited resource and water security matters.
- About 97% of the Earth's water is salt water in the oceans; only about 3% is fresh.
- Surface fresh water = ice sheets, glaciers, lakes, rivers, swamps, marshes, permafrost.
- Sub-surface fresh water = soil moisture, ground water (aquifers), permafrost.
- Atmospheric water (vapour and clouds) is small but drives the water cycle.
- Most fresh water is frozen or deep underground; accessible lake/river water is tiny.