Tropischer Sturm Agatha (2010)

Tropensturm im Pazifik in 2010
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Vorlage:Infobox Hurricane Tropical

Meteorological history

The origins of the cyclone were from an area of convection, or thunderstorms, that developed on May 24 off the west coast of Costa Rica.[1] At the time, there was a trough in the region that extended into the southwestern Caribbean Sea, associated with the Intertropical Convergence Zone.[2] The system drifted northwestward, and conditions favored further development.[3] On May 25, the convection became more concentrated, and the National Hurricane Center (NHC) noted the potential for a tropical depression to develop.[4] The next day, it briefly became disorganized,[5] 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.[6]

Preparations and impact

As a developing tropical disturbance, the system was expected to produce heavy rainfall for several days along the Pacific coastline from Nicaragua to the Gulf of Tehuantepec.[6]

References

Vorlage:Reflist

Vorlage:2010 Pacific hurricane season buttons

  1. Avila/Blake: Tropical Weather Outlook. National Hurricane Center, 24. Mai 2010, abgerufen am 28. Mai 2010.
  2. Dave Sandoval: Tropical Weather Discussion. National Hurricane Center, 28. Mai 2010, abgerufen am 24. Mai 2010.
  3. Lixion Avila: Tropical Weather Outlook. National Hurricane Center, 25. Mai 2010, abgerufen am 28. Mai 2010.
  4. Cangialosi/Pasch: Tropical Weather Outlook. National Hurricane Center, 26. Mai 2010, abgerufen am 28. Mai 2010.
  5. Brown/Roberts: Tropical Weather Outlook. National Hurricane Center, 27. Mai 2010, abgerufen am 28. Mai 2010.
  6. a b Scott Stripling: Tropical Weather Discussion. National Hurricane Center, 27. Mai 2010, abgerufen am 28. Mai 2010.