The remnants of Barbara continued west-northwest until being absorbed by a frontal zone near the International Date Line on June 30. Barbara was the first tropical cyclone in the Central Pacific during the month of June, the second being Tropical Storm Boris in 2020. Tropical Storm Cosme A tropical wave crossed Central America and emerged into the eastern Pacific basin on July 6. The wave moved slowly westward from July 6 – July 10. On July 10, the convective pattern began to show signs of organization about south of Acapulco, Mexico, and the system received its first Dvorak satellite classification. Over the next two days, the system moved generally west-northwestward as multiple competing low-level circulations developed within the broad area of low pressure associated with it. During this period, development of the disturbance was hindered by southerly shear from an upper-level trough to the west of the disturbance that caused the system to become elongated north–south. On July 12, the upper trough cut off southwest of the disturbance and the organization improved. By early on July 13, a single low-level circulation center had become established and Tropical Depression Three-E formed about southwest of Manzanillo, Mexico. The depression moved west-northwestward, and quickly became Tropical Storm Cosme on July 13, about south of Cabo San Lucas, Mexico. The forward motion then slowed over the next 12 hours. Cosme's development was hindered by easterly shear; its peak intensity of was reached late on July 13. By early on July 14, convection was limited and well removed from the center. Cosme weakened back to a tropical depression, when it was about southwest of Cabo San Lucas. Cosme produced no more significant convection after about on July 15, at which point the tropical cyclone became a non-convective low center. The low then moved slowly westward until it dissipated on July 18 about west-southwest of Cabo San Lucas. Tropical Storm Erick A poorly defined tropical wave traveled westward across the tropical Atlantic and reached the eastern North Pacific on July 16. The thunderstorm activity associated with the wave increased on July 18 when the disturbance was centered about south of the southern tip of the Baja California Peninsula. Thereafter, deep convection gradually developed around a large cyclonic gyre which accompanied the wave. It was not until July 20 that a well-defined center of circulation formed and satellite intensity estimates supported tropical depression status. Moving on a