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Temporal and spatial adjustments of channel migration and planform geometry: Responses to ENSO driven climate anomalies on the tropical freely-meandering Aguapeí River, São Paulo, Brazil

Journal Article


Abstract


  • Two reaches of Aguapeí River, a left-bank tributary of the Paraná River in western São Paulo state, Brazil, were studied with the objective of assessing the role of bend curvature on channel migration in this wet-tropical system and examining if land-use changes or ENSO (El Niño Southern Oscillation) driven climate anomalies over nearly half a century have changed migration behaviour and planform geometry. Meander-bend migration rates and morphometric parameters including meander-bend curvature, sinuosity, meander wavelength and channel width, were measured and the frequency of bend cutoffs was analysed in order to determine the rate of change of channel adjustment over a 48year period to 2010. Results show that maximum average channel migration rates occur in bends with curvatures of about 2-3 r c /w, similar to other previously studied temperate and subarctic freely meandering rivers although not as pronounced and with a tendency to favour tighter curvature. From 1962 to 2010 the Aguapeí River has undergone a significant reduction in sinuosity, a shift from tightly curving to more open bends, an overall decline in channel migration rates, an associated decrease in the frequency of neck-cutoffs and an overall increase in channel width. As the majority of the drainage basin (96%) was already deforested in 1962, channel form and process changes were, unlike an interpretation for an adjacent river system, not attributed to altered land-use but rather to a sharp ENSO-driven increase in the magnitude of peak flow-discharges of some 32% since 1972. In summary, this research revealed that recent climate and associated flow regime changes are having a pronounced effect on river channel behaviour in the Aguapeí River investigated here.

Publication Date


  • 2018

Citation


  • Suizu, T. Medeiros. & Nanson, G. C. (2018). Temporal and spatial adjustments of channel migration and planform geometry: Responses to ENSO driven climate anomalies on the tropical freely-meandering Aguapeí River, São Paulo, Brazil. Earth Surface Processes and Landforms, 43 (8), 1636-1647.

Scopus Eid


  • 2-s2.0-85042106159

Ro Metadata Url


  • http://ro.uow.edu.au/smhpapers/5254

Number Of Pages


  • 11

Start Page


  • 1636

End Page


  • 1647

Volume


  • 43

Issue


  • 8

Place Of Publication


  • United Kingdom

Abstract


  • Two reaches of Aguapeí River, a left-bank tributary of the Paraná River in western São Paulo state, Brazil, were studied with the objective of assessing the role of bend curvature on channel migration in this wet-tropical system and examining if land-use changes or ENSO (El Niño Southern Oscillation) driven climate anomalies over nearly half a century have changed migration behaviour and planform geometry. Meander-bend migration rates and morphometric parameters including meander-bend curvature, sinuosity, meander wavelength and channel width, were measured and the frequency of bend cutoffs was analysed in order to determine the rate of change of channel adjustment over a 48year period to 2010. Results show that maximum average channel migration rates occur in bends with curvatures of about 2-3 r c /w, similar to other previously studied temperate and subarctic freely meandering rivers although not as pronounced and with a tendency to favour tighter curvature. From 1962 to 2010 the Aguapeí River has undergone a significant reduction in sinuosity, a shift from tightly curving to more open bends, an overall decline in channel migration rates, an associated decrease in the frequency of neck-cutoffs and an overall increase in channel width. As the majority of the drainage basin (96%) was already deforested in 1962, channel form and process changes were, unlike an interpretation for an adjacent river system, not attributed to altered land-use but rather to a sharp ENSO-driven increase in the magnitude of peak flow-discharges of some 32% since 1972. In summary, this research revealed that recent climate and associated flow regime changes are having a pronounced effect on river channel behaviour in the Aguapeí River investigated here.

Publication Date


  • 2018

Citation


  • Suizu, T. Medeiros. & Nanson, G. C. (2018). Temporal and spatial adjustments of channel migration and planform geometry: Responses to ENSO driven climate anomalies on the tropical freely-meandering Aguapeí River, São Paulo, Brazil. Earth Surface Processes and Landforms, 43 (8), 1636-1647.

Scopus Eid


  • 2-s2.0-85042106159

Ro Metadata Url


  • http://ro.uow.edu.au/smhpapers/5254

Number Of Pages


  • 11

Start Page


  • 1636

End Page


  • 1647

Volume


  • 43

Issue


  • 8

Place Of Publication


  • United Kingdom