The effect of wind on the residual current velocities in the inlets of Venice lagoon

• Published in: Continental shelf research Vol. 30; no. 8; pp. 915 - 923
• Main Authors: Mancero-Mosquera, I., Gačić, M., Mazzoldi, A.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 15.05.2010
• Subjects: Adriatic Sea; Correlation; Doppler effect; Exponential functions; Inflow; Inlets; Lagoons; Marine; Outflow; Principal components; Residual currents; Wavelet transform; Wind speed; Wind velocity; MED, Italy, Venezia, Chioggia; MED, Adriatic Sea; MED, Italy, Veneto, Venezia, Veneta Lagoon; Wind velocity; Correlation; Wavelet transform; Principal components; Residual currents
• ISSN: 0278-4343; 1873-6955
• DOI: 10.1016/j.csr.2010.02.011

The residual flow in the inlets of Venice lagoon subject to Bora and Sirocco winds has been studied. Current velocities have been monitored since 2001 using Acoustic Doppler Current Profilers (ADCP) installed on the beds of the inlets that connect the lagoon to the Adriatic Sea; these inlets are Lido, Malamocco and Chioggia. Wind velocity data have also been continuously measured at an oceanographic platform 14.8 km offshore from the lagoon; these data were subsequently decomposed into Principal Components, which are associated with Bora and Sirocco wind directions. Analyses show that the inflow in Lido inlet is strongly related to the Bora wind. The outflow in Chioggia inlet occurs during Bora events but shows a slightly weaker correlation with the wind speed, while Malamocco inlet shows little or no influence of Bora winds on flow patterns. A net residual inflow through Lido and Malamocco inlet was found, while outflow prevails in Chioggia inlet. During Bora events, the average residual inflow increased three-fold in Lido inlet, whereas the outflow in Chioggia inlet doubled. The current velocities in Lido and Chioggia inlets are best described by an exponential function of wind velocity with exponents of −0.1187 and −0.0924, respectively. The response to Sirocco events was evident mainly in Chioggia inlet. Specifically, there was a slow down of the outflow in linear proportion to wind speed. In excess of 10 m/s a complete current reversal was observed. Lido and Malamocco inlets showed little or no response to Sirocco winds, except during rare cases when wind speeds exceeded 15 m/s.