Commerson Crater

Coordinates: 21°12′29″S 55°37′59″E / 21.2079682°S 55.6329524°E / -21.2079682; 55.6329524
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Commerson Crater
View of the upper edge of Commerson Crater.
Highest point
Elevation2,310 m (7,580 ft)
ListingList of volcanoes in Réunion
Coordinates21°12′29″S 55°37′59″E / 21.2079682°S 55.6329524°E / -21.2079682; 55.6329524
Geography
Commerson Crater is located in Réunion
Commerson Crater
Commerson Crater
Parent rangeLes Hauts
Geology
Mountain typeCaldera

Commerson Crater is a caldera in the mountains of Réunion, an overseas department of France. Located in the municipal territory of Saint-Joseph, it is part of the Piton de la Fournaise, a shield volcano on the eastern end of Réunion Island, but is located outside of the Enclos Fouqué, the volcano's most recent caldera.

The caldera was named in honor of Philibert Commerson, a French explorer.

Climate

Due to its elevated position, Commerson Crater receives considerable amounts of rainfall, especially during tropical storms. During Cyclone Hyacinthe in January 1980, it received 6,433 millimetres (253.3 in) of rainfall in 15 days, the most precipitation dropped by a tropical cyclone in a single location.[1] The second greatest amount of rainfall in a single tropical cyclone also occurred in Commerson Crater, when Cyclone Gamede dropped 5,512 millimetres (217.0 in) of rain in 2007.[2] Nowhere else has received even 3,500 millimetres (137.8 in) of rainfall from a single tropical cyclone.

References

  1. ^ Landsea, Christopher W; Hurricane Research Division (March 12, 2007). "Subject: E4) What are the largest rainfalls associated with tropical cyclones?". Tropical Cyclone Frequently Asked Questions. Archived from the original on April 4, 2013. Retrieved April 12, 2013.
  2. ^ Quetelard, Hubert; Bessemoulin, Pierre; Cerveny, Randall S; Peterson, Thomas C; Burton, Andrew; Boodhoo, Yadowsun (2009). "Extreme Weather: World-Record Rainfalls During Tropical Cyclone Gamede". Bulletin of the American Meteorological Society. 90 (5). American Meteorological Society: 603–608. doi:10.1175/2008BAMS2660.1.