totaling to 200 million pesos (2007 MXN; $55 million). About a hundred residents were forced to evacuate after the storm destroyed a dozen palm huts in Guatemala. Tropical Depression Three-E On May 24, a tropical wave emerged off the western coast of Africa. The wave entered the eastern Pacific around June 6 and shower and thunderstorm activity began to increase shortly thereafter. A broad area of low pressure formed a few hundred miles south of Acapulco, Mexico two days later. Following satellite evidence of a well-defined circulation and organized convective activity, the National Hurricane Center upgraded the disturbance to a tropical depression at 1200 UTC on June 11. After attaining winds of 35 mph (55 km/h) and a minimum barometric pressure of 1004 mb (hPa; 29.65 inHg), the depression began to traverse cooler waters and much more stable air. This caused all associated convection to fade away, and the depression degenerated to a non-convective remnant low at 0000 UTC on June 13. The remnant low continued northwest until dissipation by 0600 UTC on June 15. Tropical Depression Four-E A tropical wave emerged off the western coast of Africa on June 23. It reached the eastern Pacific on July 3, where associated convection began to increase three days later. Continued slow development occurred thereafter, and following satellite trends, the disturbance was upgraded to Tropical Depression Four-E at 1800 UTC on July 9. Tracking westward, the depression began to move across waters too cool to support a tropical cyclone and into an environment of moderate shear. The low-level circulation became ill-defined and exposed, leading to degeneration to a remnant low at 0600 UTC on July 11 about 910 mi (1465 km) west-southwest of Cabo San Lucas, Mexico. The low continued northwest until dissipation at 0000 UTC the following day. Tropical Depression Five-E On June 21, a tropical wave emerged off the western coast of Africa. It entered the eastern Pacific on July 10, and shower and thunderstorm activity began to increase a day later as a result. Tracking westward, the wave gradually became better organized; by 1200 UTC on July 14, the disturbance acquired enough organization to be upgraded to a tropical depression. Within an environment of moderate wind shear, the low-level center quickly became poorly defined as convection dissipated. Turning west-northwest on July 15, the depression entered cooler waters and an increasingly stable airmass, causing the system to degenerate into a