general west-northwest track, the system became Tropical Storm Erick and simultaneously attained peak intensity with maximum sustained winds of and a minimum pressure of 1001 mbar (hPa; ) July 22. It then moved over relatively cooler waters and weakened as the deep convection quickly vanished. By July 24, it was just a non-convective and dissipating swirl of low clouds, although some showers re-developed intermittently. Hurricane Dalila Dalila's origin is a tropical wave that moved westward from Africa and over the eastern tropical Atlantic Ocean on July 10. It crossed northern South America and Central America on the July 15 through July 17 accompanied by vigorous thunderstorm activity, and then entered the Pacific basin on July 18 as an organized area of disturbed weather. Early on July 21, the system acquired a low-level circulation and became Tropical Depression Five-E, about south of the Gulf of Tehuantepec. Moving west-northwestward, it became Tropical Storm Dalila with winds 12 hours later. Dalila steadily tracked toward the west-northwest at forward speeds fluctuating between five and . The center of the cyclone reached its point of closest approach to the coast to the west coast of Mexico between Acapulco and Manzanillo on July 22 and July 23, when it came within about of the coast. With warm sea surface temperatures and minimal vertical shear, Dalila's winds increased from from the 22nd into the 23rd. The wind speed briefly reached an estimated on July 24, and Dalila became a hurricane. However, the system quickly weakened back to a strong tropical storm. Passing directly over Socorro Island on July 25, most of the associated deep convection with Dalila dissipated on July 27 as the storm moved over colder water. Reduced to a swirl of low clouds, Dalila dissipated as a tropical cyclone on July 28, while located about west of the southern tip of Baja California. Tropical Depression Six-E A westward moving tropical wave entered the Pacific from August 12 to 13 after crossing from the Atlantic and Caribbean. At 12:00 UTC on August 22, Tropical Depression Six-E developed from this wave. In addition to lowering sea surface temperatures, the system began to be affected by southerly wind shear, which displaced the mid-level circulation and deep convection from the low-level circulation. The National Hurricane Center later noted the disorganized state of the tropical depression as being only "... a swirl of low clouds with a few showers to