The Marshallese recognized four main ocean swells: the
rilib,
kaelib,
bungdockerik and
bundockeing. Navigators focused on effects of islands in blocking swells and generating counterswells to some degree, but they mainly concentrated on
refraction of swells as they came in contact with undersea slopes of islands and the bending of swells around islands as they interacted with swells coming from opposite directions. The four types of ocean swells were represented in many stick charts by curved sticks and threads.
Rilib swells Rilib swells are the strongest of the four ocean swells and were referred to as "backbone" swells. They are generated by the northeast
trade winds and are present during the entire year, even when they do not penetrate as far south as the Marshall Islands. Marshallese considered the
rilib swells to come from the east, even though the angle of the winds as well as the impact of the ocean currents varied the swell direction.
Kaelib swells The
kaelib swell is weaker than the
rilib and could only be detected by knowledgeable persons, but it is also present year round.
Bungdockerik swells The
bungdockerik is present year round as well and arises in the southwest. This swell is often as strong as the
rilib in the southern islands.
Bundockeing swells The
bundockeing swell is the weakest of the four swells, and is mainly felt in the northern islands. ==Stick chart categories==