Kakinada, Andhra Pradesh 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 03:30 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.

Kakinada sits on the Bay of Bengal coast at the eastern fringe of the Godavari delta, one of India's most productive and ecologically significant river systems. The city is Andhra Pradesh's second-largest port, and the tidal rhythms of Kakinada Bay shape almost every aspect of life along this stretch of coast — from the mechanised trawler fleet to the mangrove corridors that buffer the delta from monsoon storm surge. The Bay of Bengal produces a semidiurnal tidal pattern here — two high waters and two low waters every 24 hours and 50 minutes. Mean tidal range at Kakinada runs 1.2 to 2.0 m, with the larger ranges during spring tides in the post-monsoon period. Because the bay opens to the south and southwest rather than directly to the open ocean, tidal heights are moderated by comparison with more exposed stretches of the Coromandel Coast. Low water typically exposes 80–120 m of flat sand and mud along the harbour foreshore. Hope Island is the defining geographic feature of Kakinada Bay. This 25 km barrier spit runs roughly north–south, separating the sheltered bay from the open Bay of Bengal. The harbour entrance sits at Hope Island's southern tip, where the channel maintains enough depth for vessel traffic for roughly 3 hours either side of high water at spring tides. At neap tides, the window is wider but the approach requires more care. Captains of the mechanised trawler fleet know this channel by instinct — most departures happen on the ebb tide in the early hours of the morning, and return runs are timed to catch the evening flood so vessels arrive at the unloading jetty with a favourable current and sufficient water beneath the keel. The harbour handles a large fleet of mechanised trawlers targeting prawn, croaker, and ribbon fish. The unloading sequence at Kakinada is tide-dependent: boats that miss the evening flood either wait offshore or accept additional harbour dues for a delayed berth. The morning market at Kakinada fish landing centre prices product that came in the previous evening — freshness is pegged directly to tidal timing. East and south of the harbour, the Godavari delta spreads across roughly 5,700 square kilometres before reaching the sea. The delta's distributary channels — the Vasishta Godavari, Gautami Godavari, and several smaller branches — discharge into the Bay of Bengal across a 70 km front. Tidal influence penetrates the lower reaches of these channels, creating brackish zones that support one of the most extensive mangrove systems in Asia. The Coringa Wildlife Sanctuary, covering approximately 235 square kilometres along the Gautami Godavari estuary southeast of Kakinada, contains around 24 of India's 35 mangrove species. Coringa is typically ranked as India's second-largest mangrove forest by area. The mangroves function as both nursery habitat for the prawns and fish that sustain Kakinada's fishing economy, and as a physical buffer against cyclone storm surge — a significant function on a coast that sits in the Bay of Bengal cyclone belt. High water in mangrove channels can exceed 2.5 m above low water during spring tides, with additional surge during cyclonic events temporarily pushing levels 1–2 m above the normal high-water mark. For anglers, Kakinada's estuary system offers productive fishing across most of the tidal cycle. Mud crab are most effectively worked at low water on the mangrove creek edges; barramundi and mullet move into the delta channels on the flood. Shore-based fishing from the Hope Island spit is possible when the channel is calm, though access requires a boat across the bay entrance. The trawler fleet targets deeper-water species offshore, but local boat operators run trips from the harbour for recreational anglers targeting prawns and croaker in the near-shore zone during the flood tide. Kayakers and canoeists exploring the Coringa mangrove channels should plan their passage carefully. The creek network is extensive but the channels shallow out quickly at low water — a transit through the inner sanctuary needs to be timed to depart with the flood and turn back before the ebb leaves less than 0.5 m of water in the minor channels. The sanctuary entry point near Corur village gives access to the core mangrove area. The Konaseema region, visible across the Godavari distributaries to the south from Kakinada's harbour waterfront, is a network of delta islands and paddy fields that sits barely above sea level. Coconut palms mark every island boundary; during spring high tides the road banks and bunds that separate paddy from water are easily overtopped. Residents here read the tide tables as much for flood management as for fishing access. For beach visitors, the area immediately north of the harbour along the Hope Island spit provides the most accessible strand. The beach widens by 60–80 m between high and low water at spring tides — sufficient to find firm sand for a walk during mid-ebb, with the sand returned to water by the following high. The sea temperature along this coast runs 26–29°C for most of the year, dropping to around 23°C in January. Tide data for Kakinada 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.