Lovina, Bali 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 06:00 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 Asia/Makassar local. Folk tradition, not a scientific forecast.

Next spring tide on Wed 06 May (range 1.3m). Next neap on Mon 11 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.

Lovina sits on Bali's north coast, 10 km west of Singaraja on the shore of the Bali Sea. It faces north across the Buleleng Strait toward the island of Java rather than toward the open Indian Ocean, and that geographical fact changes everything about how the water behaves here compared with Kuta or Seminyak on the south coast. The island mass of Bali blocks virtually all Indian Ocean swell from reaching the north coast. Swells generated south of the island — the dominant swell source for Indonesian waters in the dry season — wrap fractionally around the eastern and western tips of Bali but lose almost all of their energy before reaching Lovina. The result is a north coast that is essentially flat year-round, with wave height rarely exceeding 0.3 m at Lovina beach itself. The Bali Sea generates small locally produced chop in strong winds, but even during the northwest monsoon in December and January this rarely rises above 0.5 m. The water surface off Lovina is calm in a way that is immediately noticeable to anyone arriving from a week on the south coast. The tidal regime in the Bali Sea is semidiurnal with a mean range of 0.5 to 1.5 m — significantly smaller than the Indonesian tidal systems further west or the Pacific-facing coasts. Diurnal inequality is present but less pronounced than at Kuta. At low water the beach extends 15 to 25 m further than at high, enough to change usable beach area but not enough to dramatically restructure the shoreline. The low-water period is the better time for snorkelling access: the reef edge is closer to a reasonable wading depth and the approach through the shallow near-shore zone is more manageable. The beach at Lovina is black volcanic sand, the product of volcanic geology in the Buleleng highlands immediately to the south. The sand absorbs heat faster than quartz and becomes notably hot underfoot in the midday hours — approaching temperatures that require footwear to cross comfortably. Morning and late afternoon are the comfortable windows. The black surface creates strong visual contrast with the turquoise Bali Sea water at the shoreline, particularly at low tide when the wet sand surface reflects light. A fringing reef runs along the Lovina coast at 100 to 300 m from shore, in 3 to 6 m of water. Visibility in the Bali Sea at Lovina typically runs 10 to 15 m — cleaner than the south coast surf zones, which carry suspended sand from wave action. The reef supports hard coral at moderate coverage levels and the fish communities typical of Indonesian reef systems: parrotfish, triggerfish, small reef sharks at the outer edge, and dense populations of damselfishes and wrasses in the coral heads. Snorkelling is accessible from the beach on foot: wade through the near-shore shallows, covering 100 to 200 m at knee to waist depth, and the reef slope begins. Boat access from the beach cuts the transit to under five minutes. Low to mid-tide is the better snorkelling window; at high water the extra depth over the shallower reef sections reduces visibility to the bottom. Spinner dolphins (Stenella longirostris) are present in the Buleleng Strait year-round. The dolphins feed in offshore deep water overnight and move into the shallower coastal water in the pre-dawn hours, surfacing frequently as they wind down their feeding activity. Dolphin-watching boats depart from Lovina beach at 05:30 to 06:00 — before sunrise — and return by 08:00. The timing is driven by dolphin behaviour, not tidal timing: the pre-dawn surface activity is not tied to the tidal cycle. Boats use small outboards and position upwind or up-current of the school to avoid disturbing the animals. Pod sizes vary from a handful of animals to fifty or more on productive mornings. The activity is not guaranteed — rough sea conditions from northwest winds can disperse the dolphins or push them further offshore — but the species is genuinely resident rather than seasonal, so the probability of an encounter is high on calm mornings. On the hillside above Lovina, Brahma Vihara Arama is a Theravada Buddhist monastery, the largest of its kind in Bali. The building is visible from the beach road and from the water on a clear day, its orange and white structures standing against the green hillside. The monastery overlooks the coast and gives context for the north Bali landscape — mountains rising sharply from the narrow coastal plain, the Bali Sea extending northward toward Java. Singaraja, 10 km east of Lovina, is Bali's second city and the former colonial capital of the Dutch East Indies' Bali administration. It has a functioning port on the Buleleng Strait; ferry traffic from Java docks here rather than at south Bali's Gilimanuk. The harbour activity adds occasional vessel traffic to the strait, visible from the Lovina waterfront. Tide data for Lovina, Bali 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.