Glass Float - Dispersion

Dispersion

Today most of the glass floats remaining in the ocean are stuck in a circular pattern of ocean currents in the North Pacific. Off the east coast of Taiwan, the Kuroshio Current starts as a northern branch of the western-flowing North Equatorial Current. It flows past Japan and meets the arctic waters of the Oyashio Current. At this junction, the North Pacific Current (or Drift) is formed which travels east across Pacific before slowing down in the Gulf of Alaska. As it turns south, the California Current pushes the water into the North Equatorial Current once again, and the cycle continues. Although the number of glass floats is decreasing steadily, many floats are still drifting on these ocean currents. Occasionally storms or certain tidal conditions will break some floats from this circular pattern and bring them ashore. They most often end up on the beaches of Alaska, Washington or Oregon in the United States, Taiwan or Canada. It is estimated that floats must be a minimum of 7–10 years old before washing up on beaches in Alaska. Most floats that wash up, however, would have been afloat for 10 years. A small number of floats are also trapped in the Arctic ice pack where there is movement over the North Pole and into the Atlantic Ocean.