TY - CHAP
T1 - The beaches of the State of São Paulo
AU - Mahiques, Michel Michaelovitch de
AU - Siegle, Eduardo
AU - Alcántara-Carrió, Javier
AU - Galiforni Silva, Filipe
AU - Sousa, Paulo Henrique Gomes de Oliveira
AU - Martins, Cristina Celia
PY - 2016
Y1 - 2016
N2 - The geological heritage of the coastal province of Sao Paulo state, characterized by the presence of the Serra do Mar mountain chain, combined with the hydrodynamics and resulting shoreline orientation and wave exposition defines six compartments with different kind of beaches. Thus, the relative position of the Serra do Mar mountain chain mainly controls the type of beach morphodynamics along the coast of the state of São Paulo. It is closer to the littoral in the North, leading to the dominance of reflective beaches, and further in the South, where dissipative beaches, associated with Late Quaternary coastal plains prevail. In the northern sector, wave energy is lower due to the presence of São Sebastião Island and a very irregular shoreline. In contrast, the southern sector is characterized by a large coastal plain and beaches exposed to most of the incident waves. Two compartments have been defined in the northern sector and three more in the southern one, with a transitional compartment among them. Moreover, the area as a whole is intensely occupied, either by an industrial zone (i.e. the Santos harbour area) or by tourism activities.
AB - The geological heritage of the coastal province of Sao Paulo state, characterized by the presence of the Serra do Mar mountain chain, combined with the hydrodynamics and resulting shoreline orientation and wave exposition defines six compartments with different kind of beaches. Thus, the relative position of the Serra do Mar mountain chain mainly controls the type of beach morphodynamics along the coast of the state of São Paulo. It is closer to the littoral in the North, leading to the dominance of reflective beaches, and further in the South, where dissipative beaches, associated with Late Quaternary coastal plains prevail. In the northern sector, wave energy is lower due to the presence of São Sebastião Island and a very irregular shoreline. In contrast, the southern sector is characterized by a large coastal plain and beaches exposed to most of the incident waves. Two compartments have been defined in the northern sector and three more in the southern one, with a transitional compartment among them. Moreover, the area as a whole is intensely occupied, either by an industrial zone (i.e. the Santos harbour area) or by tourism activities.
KW - Coastal Plain
KW - Wave Climate
KW - South Atlantic Convergence Zone
KW - Brazilian Coast
KW - Longshore Sediment Transport
U2 - 10.1007/978-3-319-30394-9
DO - 10.1007/978-3-319-30394-9
M3 - Chapter
SN - 978-3-319-30392-5
T3 - Coastal Research Library
SP - 397
EP - 418
BT - Brazilian Beach Systems
A2 - Short, Andrew D.
A2 - Antonio Henrique da F., Klein
PB - Springer
CY - Cham
ER -