Hurricane Elida developed out of a weak tropical wave which formed off the western coast of Central America on July 8. It is possible that the wave formed in the Atlantic Ocean, but there is little evidence to support this theory. The system remained poorly organized for two days before gaining enough convection to be classified using the Dvorak technique on July 10, while located 290 mi (465 km) south of Guatemala. Later that day, a surface low developed but convection remained minimal. During the night and through the morning of July 11, convection increased sufficiently and a tropical cyclone formation alert was issued. By the end of the day, the storm had become Tropical Depression Six-E, six hours earlier than the operational data. At the time of the upgrade, the depression was located 360 mi (580 km) south-southeast of Puerto Angel, Mexico. The depression was moving towards the west-northwest at 16 mph (26 km/h) due to a low to mid-level ridge located to the north of the storm.
The depression was upgraded to Tropical Storm Elida early on July 12 while located 200 mi (370 km) south of Puerto Angel, Mexico. Elida's forward motion slowed somewhat as it neared the southwestern edge of the mid-level ridge. Deep convection developed around the center of circulation and a strong banding feature formed along the western side of the storm. Slow strengthening took place throughout the morning as the center remained underneath the deep convection. Outflow to the north of the storm was slightly restricted, indicating that there was some easterly wind shear. During the afternoon, a well defined banding feature appeared, but the outflow to the north remained highly constricted. Elida began to move slightly faster, still being influenced by the mid-level ridge. The foreword motion was forecast to slow down in the two- to three-day range as it moved away from the ridge. Overnight, wind shear began to weaken and outflow to the north of Elida was established. By the morning of July 13, banding features and outflow were present all around the storm, but wind shear managed to keep the center of Elida slightly displaced from the deepest convection. The movement of a weakening mid to upper-level trough trough would allow Elida to make a westerly turn. Later in the morning, the wind shear lessened and in the early afternoon, a burst of convection near the center of Elida had formed, but subsequently weakened.
Although Elida initially failed to develop an eyewall. in the early afternoon hours, satellite indicated the formation of an eye. Based on this, Elida was upgraded into a hurricane. In the late morning hours, Elida intensified slightly. and a ragged eye appeared in the afternoon as the structure of the storm improved. At this point, forecasters thought the Elida had peaked in intensity or was near its peak. Elida's direction shifted from a west-northwest to west as the ridge located to the north of the storm began influencing the trajectory. The eye disappeared shortly afterwords. as easterly wind shear began to increase. Elida slowly weakened and by the afternoon, Elida was barely holding onto hurricane status. Despite this, Elida became better organized overnight as convection wrapped around the eye.
On the morning of July 16, the eye appeared on infrared satellite and cirrus outflow improved all around the system; however, Elida was nearing cooler waters. The mid-level ridge to the north of Elida was now forecast to move with the storm, ensuring westward motion and slightly increasing the foreword speed to 12 mph (19 km/h). Elida accelerated slightly and maintained a westerly motion. The eye quickly disappeared from infrared satellite later in the morning, but deep convection persisted on the eastern side of the center of circulation. In the afternoon, an eye appeared embedded in the deep convection and Elida intensified into a category two hurricane with winds of 105 mph (165 km/) while located 630 mi (1015 km) southwest of Cabo San Lucas, Mexico. By the nighttime hours, thunderstorm activity in the northern semicircle of Elida waned and cold waters began to take their toll on Elida as the eye became cloud filled and less distinct. In the late morning, Elida weakened to a category one hurricane as determined in the tropical cyclone report. Despite continuing deep convection near the center of Elida and even an embedded eye, the center was lagging behind, making the storm slightly tilted. Elida produced a large amount of deep convection overnight, but the winds continued to lessen. The storm continued to move over colder waters, but wind shear was forecast to lessen, leading to slow, steady weakening.
By the morning of July 18, thunderstorm activity associated with Elida diminished further and the storm was downgraded to a tropical storm. Despite being over very cool waters, Elida managed to maintain a small area of deep convection as it slowly weakened. By the afternoon, most of the convection had dissipated and all that remaine. The small area of convection shifted to the east side of the center overnight, allowing Elida to remain a tropical storm with winds barely at 40 mph (65 km/h). By the morning of July 19, Elida was traversing waters of 23°C (73°F) and all the deep convection had dissipated. Due to the lack of convection, Elida was downgraded to a tropical depression. Cold waters prevented any convection from redeveloping in the late morning, and it was unlikely that any convection would form. Elida was later declared a remnant low that afternoon as the system had been devoid of convection for hours. The remnant low continued moving towards the west-southwest before dissipating into an open trough on July 21 while located 690 mi (1,110 km) east-southeast of the Hawaiian Islands.
Read more about this topic: Hurricane Elida (2008)
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