4.5 Article

Tropical Cyclone Impacts on Coastal Regions: the Case of the Yucatan and the Baja California Peninsulas, Mexico

Journal

ESTUARIES AND COASTS
Volume 37, Issue 6, Pages 1388-1402

Publisher

SPRINGER
DOI: 10.1007/s12237-014-9797-2

Keywords

Tropical cyclones; Chlorophyll-a; Baja California Peninsula; Yucatan Peninsula; Mexico

Funding

  1. Inter-American Institute for Global Change Research (IAI) CRN II by United States National Science Foundation [2048, 2050, GEO-0452325]
  2. National Council on Science and Technology in Mexico (CONACYT) [23448]
  3. NASA's Applied Sciences Program [NNA07CN12A]
  4. National Science Foundation through Florida Coastal Everglades (FCE) Long-Term Ecological Research program [DBI-0620409]
  5. NASA-JPL project (LSU) [1452878]
  6. Direct For Biological Sciences
  7. Division Of Environmental Biology [1237517] Funding Source: National Science Foundation
  8. Directorate For Geosciences [1138881] Funding Source: National Science Foundation

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Tropical cyclones (TCs) are large-scale natural disturbances that generate strong winds and heavy rainfall, impacting coastal and inland environments. TCs also influence biogeochemical and hydrological cycles controlling aquatic primary productivity in tropical and subtropical coastal ecosystems. We assessed TC landfall activity and identified sites along the Mexican east and west coasts with high frequency in the period 1970-2010 and evaluated TCs with significant precipitation. Changes in chlorophyll-a (Chl-a) concentrations before and after storm impacts were estimated using remotely sensed ocean color. There were 1,065 named TCs with a wide diversity in tracks. Three states with the highest number of landfalls were identified: Baja California Sur and Sinaloa on the west coast and Quintana Roo on the east coast. While a relative increase in Chl-a values following TC landfalls in the Baja California and Yucatan Peninsula regions appeared to be strongly linked to TC strength, the intensity of precipitation, the spatial scales of the two peninsulas, and the relative movement of TCs appeared to have contributed to Chl-a variability. Satellite estimates of Chl-a in the nearshore coastal waters following TC passage were likely enhanced by coastal morphology and water discharge along with constituents such as suspended particulate, colored dissolved organic matter and nutrients from rivers, tributaries, and groundwater.

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