A forecast for "the South West" covers a hundred miles of coastline, three headlands and a dozen microclimates. The clouds above your own stretch of water do not. They are the raw data — the actual air, right there, right now — and learning to read them is the difference between a pleasant afternoon afloat and a wet, windy dash for the slipway. You do not need instruments. You need the habit of looking up every twenty minutes and noticing what has changed since last time. Change is the whole story: a sky that is evolving is telling you something, while a sky settled into a pattern is telling you it will stay that way for a while yet.
Most fair days on the coast begin with cumulus humilis — small, flat-bottomed, wider than they are tall, with crisp edges and plenty of blue between them. These are the classic fair-weather clouds and they mean nothing worse than a spell of shade. Watch their tops. As the morning warms, a cumulus that starts to puff upwards into cumulus mediocris is one to keep an eye on; when it becomes cumulus congestus, a cauliflower tower with hard, bright edges and a flat dark base, showers are usually one to two hours away. The tell-tale is vertical growth. A cloud building upwards faster than it spreads out is a cloud with energy to spend, and sooner or later it will spend it on you.
Here is the single most useful trick for coastal walking and sailing: the height of the cumulus base is a rough measure of how humid the air is near the surface. On a dry, settled day the bases sit high — 3,000 feet or more — and the clouds look distant and neatly stacked. As moisture builds, the base drops: 2,500, then 2,000, then 1,200 feet. A lowering base is a warning. It means the air is closer to saturation, that any shower will be heavier and longer-lived, and that cloud tops will reach higher before they stop growing. If the base falls below the height of the cliffs you are walking beneath, or below the mast of the boat you are sailing, it is time to be thinking about shelter rather than whether to turn back.
The dangerous stage is cumulonimbus: a towering cloud whose top has flattened into an anvil or a broad, fibrous canopy. The base goes very dark, often with a ragged, lowering shelf of cloud at the leading edge, and the first gusts arrive before the rain does. Squall lines along the coast can shift the wind through 90 or even 180 degrees in a couple of minutes and push it from a gentle Force 3 to a spiteful Force 6 or 7. From the first clear anvil to the squall hitting your position you may have twenty to thirty minutes. If you are on the water, that is time to get the sails down, check lifejackets and head for the nearest safe harbour — not time to finish the beat.
Not all coastal weather arrives with drama. A warm front announces itself politely, often on a clear morning, with a few wisps of cirrus high up — the "mares' tails" that look like torn horsehair. Over the next few hours they thicken into a milky cirrostratus veil, and the sun develops a halo around it. Then the cloud lowers and thickens to altostratus, a flat grey sheet through which the sun becomes a dim, watery disc, and finally to nimbostratus: a low, featureless, uniformly dark layer that delivers steady, soaking rain for six hours or more. The sequence can take half a day from first cirrus to first drops, which is ample warning — if you have learned to spot the start of it.
Turn these into habits and you will rarely be caught out.
The sky is not a forecast — it is the weather itself, unfolding a few thousand feet above your head. Learn its habits over one season of coastal days and you will find you are checking the app less and trusting your own eyes far more.
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