Kristie Andresen and Steve Litvin

The Use of CODAR High Frequency Radar to Attain Wave Height Measurements

What Can the data be used for?



The directional spectrum of waves measure the distribution of wave energy in period (or frequency) and direction.  Different contributions to local wave energy can be identified in a measurement of the directional spectrum. For example, swell from distant storms will be detected by a concentration of energy in longer period (lower frequency) waves, where locally wind-generated waves will show an energy peak in lower period (higher frequency) waves.

The direction of propagation of wave energy and the period of the most energetic waves are important for many practical applications, e.g., the design and and operation of coastal and offshore structures and storm surge forecasts.
 
 

Figure 1 - Spectral analysis of CODAR wave data from LEO-15 over three days in March, 2000 shows that the dominant waves at the first part of the measurement period are approximately 6-second locally wind-generated waves.  Each line on the plot above is a 7-hour average.
 
 

Figure 2 - Additional data from the three-day period, now moving to hour averages so that the shift from 6-second to wind-generated waves to dominant 15-second swell can be seen.  The blue then red lines occur first, followed by green and cyan, and finally black, pink and yellow.  This shows energy from the swells building, peaking and then decreasing again.  The pattern above could suggest swell from an offshore storm appearing at the coast.
 
 

Figure 3 - Energy contained by the 15-second swell continues to decrease, as we see a further shift of the dominant waves to waves of a lower period.  Each line represents and hourly average.  Chronological order of the colored lines is as in the previous plot (blue, red, green, cyan, black, pink, yellow).


How do these measurements compare?     Main Project Page     Conclusions