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

被引:0
|
作者
Luis M. Farfán
Eurico J. D’Sa
Kam-biu Liu
Victor H. Rivera-Monroy
机构
[1] Unidad La Paz,Department of Oceanography and Coastal Sciences, School of the Coast and Environment
[2] Centro de Investigación Científica y de Educación Superior de Ensenada,undefined
[3] B.C.,undefined
[4] Louisiana State University,undefined
来源
Estuaries and Coasts | 2014年 / 37卷
关键词
Tropical cyclones; Chlorophyll-a; Baja California Peninsula; Yucatán Peninsula; Mexico;
D O I
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中图分类号
学科分类号
摘要
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 Yucatán 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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页码:1388 / 1402
页数:14
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