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USE OF ACOUSTIC DOPPLER CURRENT PROFILERS TO DESCRIBE VELOCITY DISTRIBUTIONS AT THE REACH SCALE 1
Author(s) -
Shields F. Douglas,
Knight Scott S.,
III Sam Testa,
Cooper Charles M.
Publication year - 2003
Publication title -
jawra journal of the american water resources association
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.957
H-Index - 105
eISSN - 1752-1688
pISSN - 1093-474X
DOI - 10.1111/j.1752-1688.2003.tb04426.x
Subject(s) - channelized , meander (mathematics) , current (fluid) , geology , acoustic doppler current profiler , channel (broadcasting) , habitat , streamflow , flow velocity , vorticity , spatial variability , spatial ecology , doppler effect , flow (mathematics) , vortex , hydrology (agriculture) , oceanography , geometry , ecology , geography , physics , meteorology , drainage basin , mechanics , geotechnical engineering , mathematics , computer science , engineering , biology , telecommunications , statistics , cartography , astronomy , electrical engineering
Research has demonstrated the utility of metrics based on spatial velocity gradients to characterize and describe stream habitat, with higher mean spatial gradients indicative of higher levels of physical heterogeneity and thus habitat quality. However, detailed description of the velocity field that is needed to compute these metrics is difficult to obtain. Acoustic Doppler current profilers (ADCPs) may be used to rapidly collect detailed representations of river depth and velocity fields in rivers deeper than 1 m. Such data were collected in March 2000 from cross sections of the Little Tallahatchie River, Mississippi, representing three distinct habitat types (naturally sinuous, channelized, and abandoned channel). These datasets were used to compute component velocities, vorticity, and area weighted mean vorticity (circulation). Velocities and circulation were highest in the meander, lowest in the abandoned channel, and intermediate in the channelized reach. Secondary flow, expressed as the average magnitude of the lateral (transverse) velocity divided by the total velocity, was significantly higher in the meander. The sinuous natural channel and abandoned channel displayed distinctive spatial patterns, with regions of depressed velocity consistently occurring near banks. ADCPs hold great potential as tools for the study of riverine ecosystems, but data reduction is difficult using existing software.