Last update: Wednesday, 25-Nov-2015 15:30:52 CET
University of Hamburg HF-Radar Home Page
Information Projects Publications Experiments Links Tests Institute of Oceanography Address

Shipborne Measurement of Surface Current Fields by HF Radar

Presented at the OCEANS'94, Session OM5, Water Currents, Floaters and Drifters

Klaus-Werner Gurgel
University of Hamburg, Institute of Oceanography, Tropolwitzstrasse 7, D-22529 Hamburg, Germany.
Tel: +49-40-42838-5742, Fax: +49-40-42838-5713,

A full paper has been published in the conference proceedings


HF radar is a remote sensing technique for measuring surface currents and ocean wave directional spectra by using the process of backscattering of electromagnetic decameter waves from the rough sea surface. The landbased HF radar system CODAR (COastal raDAR) has originally been introduced by Barrick in 1977. In Germany, the CODAR has been extended for shipborne operation. The system uses electromagnetic waves of about 10~m length (29.85~MHz). There are several difficulties to be resolved for successful measurements of surface current fields from a slowly sailing ship.

First of all, the ship's speed has to be less than the phase velocity of the coupled ocean waves (half the electromagnetic wave length). Practically, the speed should be about 1 to 2 knots. Speed and course have to be as constant as possible. Variations greater than 0.75 knots and 20 degrees per minute will significantly decrease the systems accuracy.

Another problem is the distortion of the receiving antenna characteristics by the ship's metal environment. Before starting a measurement campaign, the receiving antenna system as installed on the ship has to be calibrated. A special direction finding algorithm is then used to gain sufficient azimuthal resolution and accuracy.

The third difficulty in analysing the backscattered sea echos is the ship's pitch and roll movement causing a superposed phase modulation. The amplitude of this distortion depends on the strength of the ship's movement and so is a function of the sea state too. A special filter algorithm has to be used to suppress this modulation.

At least, the measured surface current fields include the superposed speed of the ship. The ship's velocity on the open ocean has to be measured as exactly as possible (sigma ~1 cm/s). The Global Positioning System (GPS) is used. After degradance of the GPS by Selective Availability (SA), the accuracy is no longer sufficient (sigma ~7 cm/s for 18-minute means) and a P-code receiver or differential GPS has to be used.

The shipborne CODAR has been used during several cruises to the Arctic Front above Mohn's Ridge near Svalboard. The measured surface current fields have been compared to geostrophically calculated currents, derived from CTD (Conductivity Temperature Depth) and XBT (eXpendable Bathy Thermograph) measurements. When subtracting the winddriven part from the CODAR current fields, a good agreement can be found within the calculated accuracy.

This work has been funded by the German Research Foundation within the Sonderforschungsbereich 318.
last update 21-Jan-1998
Klaus-Werner Gurgel's Homepage
Comments to:
WASd webserver
OpenVMS Operating SYSTEM
  Valid HTML 4.0!