barometric pressure of 995 mb (hPa; 29.39 inHg) a day later, the storm tracked over progressively cool waters, causing it to weaken. At 0600 UTC on July 27, Dalila weakened to a tropical storm, and by 1800 UTC, the system no longer retained enough organization to be considered a tropical cyclone. The remnant low tracked west, southwest, and eventually south prior to dissipation at 1200 UTC on July 30. Though the center of the storm remained offshore, outer rainbands led to heavy rainfall that triggered substantial flooding. In Michoacán, Dalila flooded ten municipalities with at least 15 in (380 mm) of precipitation, destroying dozens of wooden structures. Heavy rains in Jalisco killed eleven, many of whom occurred in automobile crashes. Flood waters covered numerous roads, causing many accidents, while approximately 50 homes were damaged. Rough seas and heavy rain affected Baja California Sur, though no damage or fatalities were reported. Tropical Storm Erick A tropical wave emerged off the western coast of Africa on July 16. Tracking westward, intermittent bursts of deep convection occurred as it crossed the Leeward Islands on July 22, but associated activity remained disorganized. The wave crossed Central America three days later, emerging into the eastern Pacific Ocean shortly thereafter. On July 28, a broad area of low pressure formed along the wave axis; easterly shear, however, prevented thunderstorms from developing over the center. Convective activity increased by July 31, leading to the formation of a tropical depression at 1200 UTC that day. Despite the unfavorable environment, satellite intensity estimates increased to tropical storm intensity, prompting the National Hurricane Center to upgrade the depression to such. After attained a peak intensity with winds of 40 mph (65 km/h) and a minimum barometric pressure of 1004 mb (hPa; 29.65 inHg) at 0600 UTC on August 1, continued wind shear caused Erick to weaken to a tropical depression. The low-level center became lost organization as it became elongated northeast to southwest on August 2, leading to degeneration into a tropical wave by 0600 UTC. The remnants of the system dissipated six hours later. Hurricane Flossie An ill-defined tropical wave entered the eastern Pacific on August 1 and steadily organized to attain tropical depression intensity eight days later. Within an environment of light shear, the depression intensified into Tropical Storm Flossie at 0000 UTC on August 9 and continued to organize to attain Category 1 hurricane intensity by 1200