Galle 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 09:30 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 Asia/Colombo local. Folk tradition, not a scientific forecast.

Last spring tide on Sat 02 May (range 0.6m). Next neap on Fri 08 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.

Galle sits at Sri Lanka's southwestern corner, 120 kilometres south of Colombo, where a broad harbour opens into the Indian Ocean just north of the island's last major headland before Dondra Point. The Dutch-built fort on the headland — ramparts, cannon platforms, and the lighthouse visible for miles offshore — has enclosed the old town since the 17th century and is the most intact colonial-era fortification in Asia. The harbour operates inside the fort's protected northern face, the fish market runs every morning, and the outer bay to the south is where the ocean conditions shift between monsoon seasons in a way that the two places on this page — Galle and Colombo — experience quite differently despite being on the same coast. The tidal regime at Galle is mixed diurnal. Some days you get two clear highs and two clear lows, roughly 12 hours apart. Other days the pattern collapses to a single dominant high and a long, flattish low phase as the moon's declination shifts the balance between the Arabian Sea and Bay of Bengal forcing. Mean astronomical range is roughly 0.3 to 0.6 metres — this is a microtidal coast. Spring tides around new and full moons push toward the upper end; neap tides can bring the total swing under 0.2 metres. That is small, but not irrelevant on a coral-reef coast: the difference between a spring low and a neap high can change whether you're snorkelling over a reef table in a metre of water or wading over it on your ankles. The fringing reefs off Unawatuna, six kilometres northeast along the coast, are the most visited dive and snorkel ground in the area. The bay at Unawatuna is partially sheltered by a reef arc that runs across its mouth; the inner lagoon stays calm enough for confident swimmers even when the outer bay is messy. Low tide exposes the inner reef to knee depth in places, which matters for beach entry. High water — roughly 0.3 to 0.4 metres above low in mean conditions — deepens the inner reef to a swimmable 0.8 to 1.0 metres and opens the entire bay floor for snorkelling. The reef at Jungle Beach, the small cove on the western headland of the bay, is accessible as a shore dive only on the higher half of the tide; the entry channel at low water is too shallow to fin through without damaging coral. Sea turtles — mostly green turtles, some hawksbills — are resident on the reefs near Galle and at the nesting beach at Rekawa, 50 kilometres east. The turtle population is more active in the early morning hours, regardless of tidal phase. Anglers working the rocky points south of the fort, and around the outer breakwater of the harbour, target trevally, snapper, and queenfish on the incoming tide as baitfish push against the structure. Kayaking in Galle Harbour is feasible on calm days but the harbour is active — fishing boats enter and exit from before dawn, and the ferry and commercial traffic has priority in the main channel. The southwest monsoon (May through September) brings consistent southwesterly swells to the outer bay and makes the headland paddle around the fort uncomfortable for most sea kayaks. November through March is the workable window for coastal paddling in the south. The Southwest Monsoon is the dominant seasonal factor for this coast. During the monsoon, May through September, the outer bay at Galle is exposed and rough, the harbour bar can get confused sea states when the swell meets the outgoing boat traffic, and the beach at Unawatuna is not safe for casual swimming. The Northeast Monsoon season, October through March, is when this coast opens up: flat mornings, consistent swell at Hikkaduwa (30 kilometres north), and the kind of visibility underwater that justifies the dive trips. Photographers working this coast should plan dawn shoots at the fort ramparts from October onward — the early sun hits the Dutch-era lighthouse and the rampart cannon from a clean angle and the sea is calm enough that the reflections in the harbour water hold. Tide predictions on this page come from Open-Meteo Marine, a global ocean model. The data is model-derived rather than from a calibrated local gauge — accuracy is typically within plus or minus 45 minutes on timing and 0.2 to 0.3 metres on height. On a coast with a mean range of 0.3 to 0.6 metres, that height uncertainty is a substantial fraction of the total signal. The National Aquatic Resources Research and Development Agency (NARA) in Colombo maintains the official gauge network for Sri Lanka. For any commercial harbour scheduling, reef navigation, or activity that depends on precise water-level data, NARA is the source to consult.