But the convection that was associated with the depression went away and the whole structure of the storm started to get worse. The depression stayed disorganized during the morning, in spite of curved banding traits forming, they stayed far from the center of circulation. In the late afternoon, the depression mooved onto the northern coastline of Honduras with winds still at 30 mph (45 km/h). Even though being over land and still being disorganized, the depression became a little bit more strong enough to reach its peak intensity of 35 mph (55 km/h) on the afternoon of October 15. This happened because of a mistake of a QuikSCAT satellite pass a ship, with the code H3VR, reporting 38 mph (61 km/h) sustained winds, and a buoy report. However, the winds were actually though to have been weaker than what was said because of the ridge of high pressure that was over the southern United States. The final advisory on the depression was given out the next morning as it turned back into a remnant low.