Visakhapatnam 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/Kolkata local. Folk tradition, not a scientific forecast.

Last spring tide on Sat 02 May (range 1.3m). 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.

Visakhapatnam — Vizag to almost everyone who lives here — sits on the north Andhra Pradesh coast where the Eastern Ghats come down close to the sea and the Bay of Bengal pushes west into a natural harbour backed by the Kailasa and Dolphin's Nose headlands. The result is one of the few naturally sheltered deepwater anchorages on India's east coast, which is why this has been a working port for two millennia and why it now hosts India's Eastern Naval Command, one of the country's largest commercial ports, and a growing shipbuilding industry. The headlands also mean the city's beaches — Ramakrishna Beach, RK Beach, Rishikonda — face east into the open bay, taking the full fetch of the Bay of Bengal. The tidal regime is semidiurnal: two high tides and two low tides per day, roughly six hours between each turn. Mean spring range along this coast runs approximately 1.0 to 1.5 m — moderate, in the low mesotidal bracket. The Bay of Bengal here is not a dramatically tidal sea; the range does not transform the visible shoreline the way a 4 m tide does. What it does is set the rhythm for the fishing fleet working out of Visakhapatnam's fishing harbour at Bheemunipatnam and the smaller landing stations along the coast: departure on the outgoing ebb, return on the flood, the boat-handling window at the harbour mouth governed by tide state. The offshore geography is worth understanding for anyone reading tide times here. The Visakhapatnam Canyon is a deep submarine trench running broadly perpendicular to the coast, an underwater valley that starts just a few kilometres from the shore and drops into abyssal depths well offshore. Submarine canyons influence how oceanic swell propagates into the nearshore — the canyon acts as a waveguide that concentrates energy along its axis, which means that incoming swell from the northeast can arrive with more amplitude along certain approach angles than the surrounding coast would see. This is largely invisible in calm weather but becomes relevant when northeast monsoon swell and cyclone-generated seas are propagating from the same direction. The cyclone context is the part that any honest tidal resource has to address on this coast. The Bay of Bengal's northern end is statistically one of the most cyclone-active bodies of water in the world. The sea surface temperature stays warm enough to support cyclone intensification late into the season, the funnel shape of the bay concentrates surge energy toward the coast, and the flat deltaic terrain further south offers little natural protection. Visakhapatnam has been hit by significant cyclones multiple times in recent decades — Cyclone Hudhud in October 2014 made landfall almost directly on the city, causing widespread damage and a storm surge that overwhelmed the coastal zone. During a severe cyclone event, sea levels at Visakhapatnam can exceed 3 to 5 m above the predicted astronomical tide: a number that makes the 1.0 to 1.5 m tidal range essentially irrelevant as a planning variable. The India Meteorological Department's cyclone warning system, which issues advisories at 72, 48, 24, and 12 hours before landfall, is the instrument that coastal residents, fishers, and port operators respond to during the active season. Ramakrishna Beach, the main urban beach running south from the Submarine Museum, is the coast most residents interact with daily: a long east-facing strand with the Kailasa Hills visible to the south and the port cranes on the northern horizon. The beach is busiest in the early morning and evening, when the sea breeze that builds through the afternoon has dropped. Shore fishing from the groynes and rock points here produces queenfish, sardines, and small sharks on the ebb; the local handline fishers know the tidal rhythm as a matter of daily habit. Rishikonda Beach, 15 km north of the city, is a cleaner and less developed alternative with a government beach resort and calmer surf most of the year. For kayakers and divers, the rocky headlands at Dolphin's Nose and the offshore reef structures near Bheemunipatnam offer the most interesting water. The submarine canyon approach to the coast concentrates both pelagic fish species and nutrient upwelling, which supports the reef life in the nearshore zone. Dive visibility and sea state are best between February and May, after the northeast monsoon has subsided and before the southwest monsoon builds. Predictions on this page come from Open-Meteo Marine, a gridded global ocean model — typically within plus or minus 45 minutes on timing and 0.2 to 0.3 m on height under normal conditions. These are astronomical tide predictions only. Storm surge is a separate and potentially far larger water-level event that these predictions do not capture. For storm surge warnings and cyclone advisories on this coast, the India Meteorological Department's official bulletins apply. The National Centre for Coastal Research (NCCR) in Chennai publishes tide tables for Andhra Pradesh gauge stations.