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Tropical Storm Agatha

Pacific tropical storm in 2010

  • 14 min read
  • 4 chapters
Tropical Storm Agatha near landfall in Guatemala on May 29, 2010
National Aeronautics and Space Administration (NASA) · Public domain

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Through Flood, Pascal (unit) and Rain

In all, Agatha caused at least 204 fatalities, and roughly $1.1 billion in damage throughout Central America. Despite the catastrophic damage in Guatemala, along with a high fatality rate, Agatha was not retired, and therefore was used again in the 2016 season.

Meteorological history

Tropical Storm Agatha originated from an area of convection, or thunderstorms, that developed on May 24, off the west coast of Costa Rica. At the time, there was a trough in the region that extended into the southwestern Caribbean Sea, associated with the Intertropical Convergence Zone. The system drifted northwestward, and conditions favored further development. On May 25, the convection became more concentrated, and the National Hurricane Center (NHC) noted the potential for a tropical depression to develop. The next day, it briefly became disorganized, as its circulation was broad and elongated; however, the disturbance was in a very moist environment, and multiple low level centers gradually organized into one. The low continued to get better organized; however, there was a lack of a well-defined circulation. On May 29, after further organization of the circulation and convection, the NHC initiated advisories on Tropical Depression One-E while the system was located about 295 miles (475 km) west of San Salvador, El Salvador.

Upon becoming a tropical cyclone, the system was located in an environment with little wind shear and waters of 30 °C (86 °F). As such, it was expected to strengthen, although the mountainous terrain of the Central American coastline limited significant intensification. The depression moved slowly northeastward around the western periphery of a ridge located over northern South America. Several hours later, satellites monitoring the system discovered tropical storm-force winds, prompting the NHC to upgrade the depression to Tropical Storm Agatha. Around this time, it was noted that there was a 40% chance of the system undergoing rapid intensification within the following 24 hours as the only limiting factor was its proximity to land. However, the storm failed to intensify much, peaking in intensity with winds of 45 mph (75 km/h) and a barometric pressure of 1001 mbar (hPa; 29.56 inHg). Within two hours of reaching this strength, Agatha abruptly relocated northward and made landfall at 22:30 UTC near Champerico, Guatemala.

After landfall, Agatha continued to cause floods and landslides, however it did not bring a lot of tropical storm force winds on shore. The system weakened quickly after coming on shore, dropping its winds to 25 mph (20 knots, 40 km/h) and its pressure to 1007 mbar (hPa; 29.74 inHg) before dissipating. A burst of convection re-emerged east of Belize, in the Atlantic basin, on May 31. On June 1, the National Hurricane Center stated that the remnants of Tropical Storm Agatha had only a low chance of regeneration in the western Caribbean Sea.

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