Collection: Field Notes — Old Fashioned Seamanship

Series Hub: Traditional Navigation Techniques

Subject: Land signs at sea — birds, clouds, sound, and colour as indicators of invisible land; how Pacific navigators expanded their target zone far beyond visual range, and how the same signs work on a North Sea or Atlantic approach

Reading Land Signs at Sea — Birds, Clouds, Sound, and the Expanded Target Landfall

An atoll in the Pacific barely rises above sea level. From a small boat the visual range, the distance at which you could see the land itself, is perhaps ten miles. The zone in which the atoll announces its presence through birds, clouds, and water colour extends to thirty, forty, sometimes seventy miles. The target, in navigational terms, is not the island. It is the zone of signs that surrounds it.

This is the central insight of what David Lewis, in We, the Navigators, calls the expanded target landfall. The transformation of a tiny, low-lying objective into a much larger, multi-layered navigational target through the systematic reading of environmental signals that precede the island’s visual appearance by many miles. It is not a technique limited to the Pacific. The same physics that generates land clouds over a coral atoll generates them over Lundy, the Scillies, or any other piece of land warmed by the sun. The same biology that sends terns back to their roosting islands at dusk operates over every seabird colony in the North Atlantic. The signs translate. What requires work is learning to read them.

Birds: the most reliable indicators

Lewis documents a consistent understanding across multiple Pacific Island navigational traditions about the role of seabirds in landfall. Two navigators from entirely separate island groups, Teeta of the Gilbert Islands and Hipour of the Carolines, gave Lewis almost identical descriptions when asked about birds as navigational signs. Both identified terns and noddies as the most consistently useful species. Both gave the useful range as approximately twenty miles offshore, twice the sight range of a low atoll. Both emphasised that the directional information only comes at specific times. In the early morning when birds leave their roosting island to feed, and in the evening when they return.

During the day, a large number of noddies in the area confirms that land is somewhere within roughly twenty miles, but gives no indication of direction. It is only the morning departure flight and the evening return that indicate the bearing of the land. At dusk, Lewis records, frigatebirds abandon their random patrolling, climb higher, and set off in a single direction with purpose. Boobies leave their inquisitive circling and fly low and straight for the horizon. Noddies and terns follow with considerable directional precision. The navigator who wants to know where land lies heaves to at dusk and watches.

Boobies have a larger daily range than noddies. Hipour estimated roughly thirty miles, and this is consistent with other sources Lewis cites. Frigatebirds range further still, perhaps seventy-five miles, though their homing behaviour is less reliably directional and Lewis notes that Carolinian navigators regarded them as erratic land indicators despite their impressive range. A solitary frigatebird is interesting. A group of them in purposeful flight at dusk is considerably more so.

Lewis gives a direct demonstration of bird navigation in practice. On the return passage from Saipan toward Pikelot, Hipour aimed not at the tiny islet itself but at the bird zone extending around it. A twenty-mile radius circle of tern and noddy activity that made the effective target forty miles across rather than the few hundred yards of actual land. When two boobies appeared flying from a direction consistent with their expected etak island of Gaferut, Lewis took a bearing on them. Plotting his track in Australia afterward, he found Gaferut had indeed been in that direction at the time, about sixty to seventy miles off. The birds had provided a useful position confirmation.

The critical practical note Lewis emphasises is attention. He writes plainly that the number of birds a sailor on casual watch will log bears no relation to the number a trained navigator attending carefully will notice. This is not mystical. It is the difference between looking and specifically watching for something. A helmsman focused on sail trim, instrument readout, and watch-keeping routine will register seabird presence only when there are very many of them. A watch specifically tasked with noting bird species, numbers, and flight direction will record far more, including the kind of specific directional departure flight that provides a bearing.

For the North Sea and Atlantic sailor

The relevant bird species differ, but the principle transfers exactly. Gannets are the most useful bird for northern European waters. They are coastal and island breeders. Bass Rock, Hermaness, Ailsa Craig, Grassholm, and dozens of other colonies around the British Isles. Their daily feeding range from those colonies is considerable, up to several hundred kilometres in some studies. A gannet or a group of gannets flying with purpose in consistent direction at dusk is worth attending to. Puffins, razorbills, and guillemots all have a much more restricted range and are reliable indicators of proximity to breeding colonies, within roughly twenty to thirty miles of nesting cliffs. Seeing them in numbers on the water in July or August places you within that radius.

On a Biscay crossing, gannets and shearwaters can be treated as range indicators in the broad sense without directional precision. On a western approaches landfall after a Channel crossing or a return from Biscay, the density and species composition of the bird life changes with proximity to the Scillies, Cornwall, and the French coast in ways that are readable once you know what to look for. Tim Severin’s crossing of the North Atlantic in the replica sixth-century currach Brendan used exactly these signs for landfall confirmation. Bird behaviour, cloud character, and water colour all contributed to the approach to Newfoundland at the end of the crossing, as he describes in The Brendan Voyage.

Cloud signs and the stationary cumulus

The second major category of land signs Lewis documents is cloud behaviour. The physics is the same in any latitude. Land heats faster than sea, warm air over land rises, and as it rises it cools to the dew point and a cumulus cloud forms. Over a small island on a sunny afternoon, this produces a cumulus that sits over the island and stays there while other clouds drift past on the wind. The cloud above the island is anchored to its heat source. The surrounding clouds are not.

Lewis documents the Gilbertese navigator Teeta’s description of how this works in practice. The first sign, visible from roughly fifteen to twenty miles, is a persistent cloud formation that behaves differently from the surrounding cloud. It builds, breaks up slightly, and reforms. Its internal activity driven by the convection over the land while the clouds around it drift steadily downwind and dissipate. The shape Teeta particularly emphasised as diagnostic is what Lewis describes as a V-shaped cloud. Two branches that form above an invisible island as the convective cloud is split by internal dynamics and then carried downwind, with new cloud continually forming and replacing the dissipating arms. The cloud does not move. The arms reform as each successive cumulus is blown away.

In overcast conditions, a different sign becomes visible. The overcast above an island’s position thickens and darkens while the surrounding sky remains lighter. There is also what the Gilbertese navigator Abera described to Lewis as the loom of invisible land. A faint brightening of the horizon above a sandy atoll that reflects the sun’s glare upward, visible from considerable distances and most easily seen when there is partial cloud to act as a reflecting surface.

Iotiebata, another Gilbertese navigator, demonstrated cloud colour changes for Lewis on a passage between two atolls. Approaching an island with a lagoon, the cloud base above it showed a greenish tint at around fifteen to sixteen miles, the reflected colour of the lagoon water being picked up in the cloud base. Above sandy or reef-dominant surfaces the cloud base brightens and whitens. Above forested land it darkens.

The Solent as a Pacific training ground

Tristan Gooley, in The Secret World of Weather, makes a direct connection between Pacific Island cloud-reading techniques and what any sailor can observe over the Isle of Wight on a settled summer afternoon. He describes watching from the South Downs above his home, with the Solent below and the Isle of Wight clearly visible across the water, and seeing the island produce exactly the cloud formations Pacific navigators used as landfall indicators. Cumulus clouds build over the island from early afternoon, differ noticeably in character from clouds over the surrounding water, and show the anchored, rebuilding behaviour that distinguishes a thermally-driven island cloud from a drifting sea cloud.

His point is explicit. The Solent on a sunny summer afternoon is a free training ground for this observational skill, with the significant advantage that you can see the island causing the cloud while you learn to recognise the signs. Once you have trained your eye on the Isle of Wight, or on Lundy from the Bideford Bay coast, or on any island visible from a vantage point, the same recognition transfers to islands you cannot yet see.

This is the most useful single training opportunity for cloud-reading in British waters and it requires nothing more than a sunny afternoon, a bit of height, and specific attention. I think Gooley’s framing is genuinely valuable here. He has done the work of translating an exotic Pacific technique into a practical exercise that anyone with a clear afternoon and the Isle of Wight in view can do.

Cloud signs on European approaches

On a western approaches passage from Biscay toward the Scillies, the islands will produce visible cloud effects well before the land itself appears above the horizon. Provided conditions are suitable, which means a settled afternoon with sufficient solar heating and a reasonable humidity level. The classic scenario is a southwesterly crossing from Ushant or the Brest approaches toward the Scillies. The Scillies rise only briefly above sea level, and their visual range from a small yacht’s deck is modest. But in settled conditions in summer, the cumulus building over the islands from early afternoon is visible at a considerable distance, stationary against a slowly drifting background of trade cumulus.

The same effect applies to the Orkney Islands approaching from the south, to Shetland from Orkney, to the Faroe Islands on a passage from Shetland, and to the Norwegian mountains on an approach from the North Sea. For high ground the effect is a slightly different phenomenon, orographic cloud forced up by the mountain, which is even more persistent and distinctive than the convective island cloud.

Sound as a land sign

Gooley covers this territory in How to Read Water in the context of freshwater, detecting a waterfall at range by careful listening. The same principle applies at sea in certain conditions. The sound of surf breaking on a rocky coast carries downwind for several miles in calm conditions. In fog on a quiet night, this is not a reassuring sound, but it is an informative one, and hearing it before seeing anything is considerably better than the alternative.

More practically, the distinctive character of shore-reflected sound in fog, the different acoustic quality of an echo off a cliff face versus open water, was used by coasting sailors for centuries. In the era before electronic fog detection this was a real navigation tool, and it remains available to any sailor who is paying attention and not drowning out the auditory environment with engine noise.

Integrating the signs

Lewis makes an observation about land sign navigation that is worth stating directly. These signs are not road signs. They do not produce unambiguous, permanent, readable information on demand. They are transient, variable, and require patient, sustained observation over an hour or more to become interpretable. He records the Gilbertese navigator Iotiebata’s instruction that when cloud signs are not visible, patience is required. They will reappear. A five-minute glance at the sky tells the untrained eye almost nothing. An hour of careful watching, attending to which clouds stay and which drift, which build and reform, which show a different colour at the base, begins to produce interpretable information.

This is, in microcosm, the same shift in observational practice that the whole of this navigation series describes. Not a matter of knowing more facts. A matter of attending differently, with sustained, specific, patient attention rather than a background awareness. The signs are present in the environment. They require observers who are actually watching for them.

The Dead Reckoning trainer covers the position-estimating process that tells you when to start looking for land signs in the first place. Knowing your approximate position is what makes the question “is that gannet flying from where my chart says Bass Rock is” meaningful. Land signs without dead reckoning are decoration. Land signs combined with a noon shot sextant or DR plot are confirmation.

The companion posts in this series. The Sidereal Compass covers the star-based direction framework that takes the navigator toward the target. Dead Reckoning Without Electronics covers the position-estimating process that tells you when to start looking for land signs. The full series index is at Traditional Navigation Techniques.

References

Lewis, D. (1994). We, the Navigators: The Ancient Art of Landfinding in the Pacific. University of Hawai'i Press.

Gooley, T. (2016). How to Read Water. Sceptre. 

Gooley, T. (2021). The Secret World of Weather. Sceptre.

Severin, T. (1978). The Brendan Voyage. Hutchinson.

Gooley, T. (2013). Nature's Radar. The Journal of Navigation, 66(2), 161–179. 

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