Wicklow, Leinster 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 23:00 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 Europe/Dublin local. Folk tradition, not a scientific forecast.

Next spring tide on Sat 09 May (range 1.1m). Next neap on Thu 07 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.

Wicklow town faces east onto the Irish Sea, 50 kilometres south of Dublin Harbour. The Vartry river reaches the sea here through a small harbour that has served the town since medieval times. What surprises most visitors comparing Wicklow to Dublin Bay is the tidal range — mean spring range at Wicklow is only 1.0 to 1.5 metres, compared to 3.5 to 4.0 metres at Howth, just 50 kilometres north. This is not a quirk of local geography. It reflects something fundamental about the dynamics of the Irish Sea. The Irish Sea is a semi-enclosed basin, roughly 220 kilometres long and 100 kilometres wide at its broadest point. The Atlantic tidal wave enters from the south, between Wexford and Pembrokeshire, and also from the north, between County Antrim and the Mull of Kintyre. These two waves travel toward each other and interact. A tidal amphidrome — a point of near-zero tidal range around which the tidal wave rotates — sits in the central Irish Sea, roughly east of the Isle of Man. Wicklow lies relatively close to this amphidromic point, which suppresses its tidal range dramatically. The physics are the same reason that certain points in the North Sea, off the Dutch coast, have almost no tide at all: they sit near their own tidal node. For practical purposes, Wicklow's 1.0 to 1.5 metre spring range means the harbour entrance dries at low water but the drying height is modest compared to harbours further north. The Vartry river outflow complicates the harbour at low water — the shallow bar across the entrance accumulates river-borne sediment and is the feature that most constrains vessel access. Local fishing vessels know the timing precisely; occasional visitors need to check predictions before entry. Black Castle headland marks the southern boundary of Wicklow Bay. The ruins of a Norman castle from the 12th century occupy the rocky promontory; access from the town is by a path that rounds the base of the headland. At lower states of tide, the path is clear of the sea and gives access to the wave-cut rocks around the headland's eastern face. At high water, particularly with any southerly swell running, the rocks at the base of the headland are washed, and the path is impassable. The ruin itself sits above the highest tide mark and is accessible at all states, but the circuit around the base requires a falling or low tide. Wicklow Head lighthouse, 4 kilometres south of town, stands on a headland that drops sharply to the sea. The lighthouse was established in 1781 and the current tower dates from 1818. The head is a seabird watchpoint; offshore movements of gannets, skuas, and Manx shearwaters are visible on appropriate wind and season combinations. The tidal range at the head is similar to Wicklow town — the rocks below the cliff expose a modest intertidal zone at low water. Brittas Bay, 10 kilometres south of Wicklow, is one of the most popular swimming beaches on the east coast of Ireland. It is a long, east-facing sandy beach backed by a dune system. The small tidal range at this latitude means the beach character is relatively consistent — the water does not retreat far on the ebb, and the bathing area does not move dramatically over the tidal cycle. Families with small children find this predictability useful; there are no large sand banks that appear and disappear with the tide, and the foreshore slope is gentle throughout. Summer weekends bring significant numbers from Dublin. Sea anglers fish the rocks around Black Castle and from the pier arms at Wicklow Harbour. Bass and flounder are the main winter targets; mackerel and pollock from summer onward. The Vartry outflow on the ebb creates a modest current plume that attracts flatfish — anglers positioning themselves to fish the edge of this plume on a falling tide do consistently better than those working the static pier. Tide data for Wicklow, Leinster comes from the Open-Meteo Marine API, a gridded model product. Timing accuracy is ±45 minutes, height accuracy ±0.3 m — usable for trip planning, not for navigation.