weaken; it degenerated into a remnant low at 18:00 UTC on the next day. The low drifted southwest and then west, before dissipating well east of Hawaii on September 21. Hurricane Javier A tropical wave entered the eastern Pacific in early September, organizing into a tropical depression at 18:00 UTC on September 10 south of the Gulf of Tehuantepec. Under light shear, the depression intensified into Tropical Storm Javier at 12:00 UTC the next morning and into a hurricane at 18:00 UTC on September 12. The cyclone soon began a period of rapid intensification as it alternated on a west-northwest to northwest course, ultimately peaking as a Category 4 hurricane with winds of 150 mph (240 km/h) at 00:00 UTC on September 14 as a distinct pinhole eye became evident on satellite imagery. Cooler waters, strong southwesterly shear, and an eyewall replacement cycle all weakened Javier thereafter; it fell to tropical depression intensity early on September 19 before crossing Baja California and degenerated into a remnant low at 18:00 UTC that day over the Gulf of California. The low crossed the state of Sonora before dissipating over mountainous terrain on September 20. As a tropical cyclone, Javier produced moderate rainfall peaking at 3.14 in (80 mm) in Bacanuchi, Mexico. Three fishermen went missing offshore the coastline due to high surf. As a post-tropical cyclone, the storm's remnant moisture overspread the Southwest United States, alleviating a multi-year drought. Accumulations peaked at 7 in (178 mm) in Walnut Creek, Arizona, with lighter totals across the Four Corners and upper Midwest. The remnants of Javier produced 2 in (51 mm) of rain in Wyoming, cementing its status as the wettest tropical cyclone in the reliable record there. Tropical Storm Kay An area of disturbed weather developed within the ITCZ well southwest of mainland Mexico, coalescing into a tropical depression at 18:00 UTC on October 4. The depression strengthened into Tropical Storm Kay twelve hours later, and it attained peak winds of 45 mph (75 km/h) at 12:00 UTC the next morning as suggested by satellite intensity estimates. Moderate northerly shear caused core convection to decrease as the system moved west-northwest, resulting in Kay degenerating into a remnant low at 12:00 UTC on October 6 over open ocean. The low-level swirl curved southwestward and dissipated the next day. Tropical Storm Lester An area of disturbed weather south of the Gulf of Tehuantepec organized into