What Is an Outgoing Tide? Definition and Effects

Tides are a powerful natural phenomenon, shaping coastlines and influencing marine environments globally. These rhythmic rises and falls of ocean water are fundamental to coastal dynamics, impacting navigation and marine life. Understanding the outgoing tide offers valuable insights into the ocean’s behavior and its daily interactions with land.

Defining the Outgoing Tide

An outgoing tide, also known as an ebb tide, is the period when sea levels fall between high and low tide. During this phase, water recedes from the shoreline, moving seaward. This movement is the opposite of an incoming, or flood, tide, which sees water levels rising. The ebb tide marks the transition from high to low tide.

This process involves a horizontal movement of water, creating an ebb current. This current flows away from the land and towards the sea, emptying bays, estuaries, and tidal rivers. From shore, an outgoing tide is observed as the water’s edge visibly moves outward, exposing more of the beach or seafloor.

The Forces That Drive Tides

Tides are primarily generated by the gravitational pulls of the Moon and Sun on Earth’s oceans. The Moon exerts the most significant influence due to its proximity, despite being smaller than the Sun. The Moon’s gravity creates bulges of water on both the side of Earth facing it and on the opposite side.

The bulge closest to the Moon results from direct gravitational attraction. On the far side, a bulge forms because the Moon’s gravity pulls the Earth more strongly than the water, causing the water to bulge outwards due to inertia. As Earth rotates through these two bulges over approximately 24 hours and 50 minutes, coastal areas experience two high tides and two low tides daily. The Sun also contributes to tidal forces, though its influence is about half that of the Moon, creating stronger or weaker tides depending on its alignment with the Moon and Earth.

Practical Considerations for Outgoing Tides

Outgoing tides create distinct conditions important for coastal activities and safety. Strong currents frequently accompany ebb tides, particularly in constricted areas like inlets, harbors, and river mouths. These powerful currents can pose safety hazards for swimmers, boaters, and paddleboarders, as they can quickly pull people away from shore or make navigation challenging. The strongest ebb currents typically occur before or near low tide.

The receding water during an outgoing tide also exposes more shoreline, benefiting activities like beachcombing and collecting shells. This exposure allows observation of marine life that might otherwise be submerged. For fishing, outgoing tides are advantageous, as currents often carry baitfish and other food sources out of shallower areas into deeper channels or towards offshore structures. Many fish species feed more actively during moving tides, making the ebb an opportune time for anglers, especially near inlets where prey is swept out.