Theory

Marine meteorology: what you need for the exam

Shkiper AI team · 12 April 2026 · 7 min read

Atmospheric pressure and isobars

Standard atmospheric pressure at sea level is 1013 hPa (mbar). On a synoptic chart, pressure is shown by isobars — lines of equal pressure, usually at 4 hPa intervals. The wind blows parallel to the isobars (in the northern hemisphere with a slight inflow toward low pressure) and the closer they are, the stronger it is.

Buys-Ballot’s law (a practical rule for the northern hemisphere): stand with your back to the wind — the centre of low pressure is on your left. A quick way to gauge where a cyclone is moving relative to you.

A low-pressure area (L, cyclone) — bad weather: clouds, precipitation, strong winds. A high-pressure area (H, anticyclone) — usually clear, weak winds in summer, cold and fog in winter.

Fronts and cyclones

A mid-latitude cyclone is a structure with warm and cold fronts:

For the sailor, the key sign of imminent worsening is a pressure drop of more than 2 hPa in 3 hours and a wind shift. A fast drop (4+ hPa in 3 hours) is a sign of an active cyclone — head for shelter.

Breezes and local winds

On clear summer days near the coast, breezes — daily-circulation winds — are at work:

Knowing the breezes helps plan departures and returns: with a sea breeze it is easy to head out, with a land breeze — to come back.

Katabatic winds — cold air flowing down a high coast or mountain. They suddenly intensify at night and can reach 15–25 m/s. Typical in fjords, Adriatic straits (bora) and the Mediterranean (mistral, tramontane).

The Beaufort scale

The Beaufort scale (0–12) describes wind force by visual cues — useful when no instrument is at hand. Key points for the sailor:

Forecasting from clouds and signs

Without internet, a sailor reads the weather from the sky:

Working forecast sources: NAVTEX (automatic reception of storm warnings), GRIB files via a satellite terminal, national marine services (Météo France, UK Met Office, Russian Roshydromet).

Tides

Tides are caused by the gravitational pull of the Moon (the main contribution) and the Sun. Key concepts for the exam:

For the sailor, tides decide whether you can enter a port, how much chain to pay out at anchor, and how to set course relative to the current. An hour’s mistake can land you on a sandbank.

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