Barra Beach tide times

Predictions: Open-Meteo Marine (MeteoFrance SMOC, 0.08° grid) — heights relative to MSL (not chart datum / LAT). Model-derived.

Model-derived from a global ocean grid. Useful indication; expect about ±45 minutes on average vs. a local harmonic gauge, individual stations vary widely. See /methodology for per-region detail. Not for navigation.

Conditions as of 00:00 local time. Refreshes daily.

Predictions: Open-Meteo Marine (MeteoFrance SMOC, 0.08° grid) — heights relative to MSL (not chart datum / LAT). Model-derived. · Not for navigation.

The angler tradition for major/minor fishing windows: major ≈3-hour windows around moon transit and opposition; minor ≈2-hour windows around moonrise and moonset. Times are Africa/Maputo local. Folk tradition, not a scientific forecast.

Last spring tide on Thu 07 May (range 1.5m). Next spring tide on Wed 13 May (range 1.9m). Next neap on Sun 10 May.

Spring tides cluster around new and full moons (biggest swings). Neap tides land on quarter moons (smallest swings). See the spring tide and neap tide glossary entries for the why.

Barra Beach sits 15 km north of Tofo on the Inhambane Peninsula, at a point where the peninsula narrows to less than 500 m between the Indian Ocean-facing eastern coast and the Inhambane Bay-facing western coast. Barra Point, the northernmost tip of the beach, is within sight of both water bodies simultaneously — the open-ocean swell running in from the southeast on one side and the flat calm of the bay on the other. The two coastlines are functionally different beaches accessed from the same narrow piece of land. The eastern, ocean-facing beach at Barra is exposed, with consistent southeast swell and the full macrotidal range of approximately 3.5 m on springs. At spring low water the beach widens by 150 to 200 m and the outer sandbar, which generates a shore-break on swell days, becomes exposed on its crest. The western, bay-facing shore is sheltered — mangrove fringe, calm water, soft bottom — with the same 3.5 m spring range but expressed across a shallow intertidal flat rather than a surf beach. At spring low the bay flat around the mangrove edge exposes several hundred metres of mudflat. The dhow crossing from Maxixe to Inhambane town — across the 3 km of Inhambane Bay that separates the mainland from the peninsula — is one of the most atmospheric short passages on the Mozambique coast. Traditional ngalawa sailing dhows make the crossing through the day, timing departures with the tide and the wind. The bay is shallow over most of its extent; the dhows draw less than 0.5 m on flat water and can cross on almost any tidal state, but the operators prefer the flood and the slack high for ease of navigation through the sandbank channels. The crossing from Maxixe market on the mainland to Inhambane town is the practical transport link for most visitors arriving by bus from Maputo; the motorised ferry supplements the dhows on the busier morning runs. Barra Lodge, at the northern end of the beach, is the main resort accommodation. The lodge sits on a prominent dune overlooking the beach with views north to Barra Point and south toward Tofo. Access from Inhambane town is by road around the peninsula — approximately 20 minutes by vehicle — or by boat across the bay and then by road to the lodge. Shore fishing from the ocean-facing beach at Barra is consistent for the same species as Tofo: kingfish, barracuda, garrick, snapper, and queenfish from the beach gutters and the rocky headland at Barra Point. The headland rocks are fishable from approximately mid-ebb through the first two hours of the flood; spring high water submerges the ledge fishing positions. The bay side at Barra also produces flatfish and smaller reef species from the exposed mudflat edges at low water. Kayakers and paddleboarders on the bay side find a protected flat-water environment with consistent conditions across most tidal states — the bay is navigable throughout the range, though the shallow inner flat near the mangrove edge is inaccessible at low spring. The ocean side is suitable for experienced paddlers on calm days when swell is below 1.5 m. Beach-walkers at Barra on a spring low find one of the widest and most varied stretches of shore on the Inhambane Peninsula. The 150 to 200 m of firm wet sand that emerges on the ocean side at spring low runs south from the lodge to Barra Point without obstruction; the equivalent low-water bay-side exposure on the mangrove edge is a different landscape entirely — dark mud, crab burrows, and the clicking of fiddler crabs working the exposed flat. Photographers with early morning access to the spring low find both environments within a 10-minute walk of each other and both lit by the same low eastern light. Kayakers departing from the bay side at Barra should avoid the mangrove drainage channels on the spring ebb: the flow through narrow mangrove channels can reach 1.5 knots as the flat drains, and paddling against it wastes energy that is better conserved for open-bay crossing. Predictions for Barra Beach come from Open-Meteo Marine, a gridded global ocean model; accuracy is typically within plus or minus 45 minutes on timing and 0.2 to 0.3 m on height above chart datum. The authoritative Mozambican tide tables are published by Instituto Nacional de Hidrografia e Navegação (INAHINA). These predictions are not for navigation.