A MECHANISM FOR THE ACCUMULATION OF FLOATING MARINE DEBRIS NORTH OF HAWAII

A mechanism for the accumulation of floating marine debris in the Nort h Pacific, especially north of the Hawaiian Islands, is investigated. First, about 50 pseudo marine debris markers floating at the sea surfa ce are arranged in the North Pacific. Their trajectories are simulated by surface currents consisting of Stokes drift, Ekman drift, and geos trophic currents. The simulation by Ekman drift alone shows remarkable convergence at midlatitudes and moderate convergence north of the Haw aiian Islands. On the other hand, that by Stokes drift or geostrophic currents does not present any remarkable high-density area and shows b asin-scale movement of marine debris. However, from the simulation by combined surface currents, marine debris gathers north of the Hawaiian Islands. This can be explained by a simple mechanism consisting of a three-step process. First, marine debris accumulates in the Ekman conv ergence zone related to westerly and trade winds. Second, the debris m oves eastward by geostrophic currents. Finally, the debris accumulates north of the Hawaiian Islands by Ekman drift due to the atmospheric N orth Pacific subtropical high.