An HF-radar test deployment amidst an ADCP array on the West Florida Shelf

For 11 days in January 2002, the Conrad Blucher Institute for Surveying and Science, Texas A&M University-Corpus Christi, in collaboration with the College of Marine Science, University of South Florida, deployed a pair of 25-MHz CODAR Ocean Systems HF-radars on the West Florida Shelf over an array of six acoustic Doppler current profilers. The radar footprint had a maximum range of 60 km offshore, and it included mooring locations between the 10 m to 30 m isobaths. We examine, using a variety of metrics, the correlation between the surface currents measured remotely by the HF-radar and the subsurface currents measured by the ADCPs, which were either bottom- or surface buoy-mounted. Qualitative comparisons are generally good for this inner-shelf environment where the wind-driven current magnitudes were less than about 40 cm/s. The scalar regression analysis shows correlation coefficients (R) of 0.8 to 0.9 for the alongshelf components but 0.6 or less for the cross-shelf components. Complex vector correlation produces correlation values of 0.76 to 0.90 and a consistently clockwise veering from the radar-measured currents to the ADCP-measured ones ranging from 1.3 to 5.2 . The alongshelf surface currents measured by the radar are about 30% larger than those of the ADCPs measured 2 to 3 m below the surface according to standard deviations and linear regression slopes.

[1]  David A. Jay,et al.  Data Analysis Methods in Physical Oceanography , 1999 .

[2]  R. Weisberg,et al.  An upwelling case study on Florida's west coast , 2000 .

[3]  William J. Emery,et al.  Data Analysis Methods in Physical Oceanography , 1998 .

[4]  Donald E. Barrick,et al.  EVOLUTION OF BEARING DETERMINATION IN HF CURRENT MAPPING RADARS , 1997 .

[5]  B. Cameron Reed,et al.  Linear least‐squares fits with errors in both coordinates. II: Comments on parameter variances , 1992 .

[6]  R. Weisberg,et al.  Seasonal modulation of the West Florida Continental Shelf Circulation , 1996 .

[7]  B. Lipa,et al.  Least-squares methods for the extraction of surface currents from CODAR crossed-loop data: Application at ARSLOE , 1983, IEEE Journal of Oceanic Engineering.

[8]  R. Weisberg,et al.  Response of the West Florida Shelf circulation to climatological wind stress forcing , 1999 .

[9]  D. Crombie Resonant backscatter from the sea and its application to physical oceanography , 1972 .

[10]  P. Sprent,et al.  Query: The Geometric Mean Functional Relationship , 1980 .

[11]  P. E. An,et al.  Very high-frequency radar mapping of surface currents , 2002 .

[12]  D. Crombie,et al.  Doppler Spectrum of Sea Echo at 13.56 Mc./s. , 1955, Nature.

[13]  Donald E. Barrick,et al.  First-order theory and analysis of MF/HF/VHF scatter from the sea , 1972 .

[14]  P. K. Kundu,et al.  Ekman Veering Observed near the Ocean Bottom , 1976 .

[15]  B. Cameron Reed,et al.  Linear least‐squares fits with errors in both coordinates , 1989 .

[16]  John F. Vesecky,et al.  HF Radar Instruments, Past to Present , 1997 .