Roughly 36 hours later, the remnants of Genevieve regenerated into a tropical depression to the southeast of the main Hawaiian Islands. The system briefly became better organized on July 30, prompting the CPHC to forecast the storm would re-intensify into a tropical storm. However, by the end of the day, the low-level circulation center had become displaced to the east of the deep convection due to increased southeasterly shear and infiltration of dry air. By 21:00 UTC July 31, the CPHC reported that Genevieve had once again weakened into a remnant low, as only an isolated area of deep convection remained west of the center.