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Sea Surface Currents and Waves

High-frequency (HF) radar uses radio-wave backscatter to map surface currents over wide swaths of the coastal ocean. These are commonly referred to as HF Radar Instruments and take advantage of the propagation of radio waves over large distances out and back across the surface of the conducting sea water, and they have resonant interactions with ocean surface waves (i.e., the ones that can make people seasick). Back at the shoreline, a measurement of the frequency offset (i.e., Doppler shift) of the reflected radio waves provides a remotely sensed measurement of the speed of the ocean waves and surface currents. For more information see Detailed sensor description >>

The Bodega Marine Laboratory operates five HF Radar stations located in Bodega Bay, Point Reyes, Salt Point, and Point Arena, CA.

HF Radar Data Products -

Ocean Surface Currents from Bodega Bay to Point Reyes

Ocean Surface Currents from Bodega Bay to Point Arena

Google Map of Surface Current Plots from Point Sur to Bodega Bay

Wave Height Data for Bodega Bay

Long Range Wave Height Data for Bodega Bay

Long Range Wave Height Data for Point Arena

Detailed sensor desciption

About available data sets

 

 

Disclaimer: WARNING: Environmental data are provided by BML/BOON with the understanding that they are not guaranteed to be correct or complete. Conclusions drawn from such information are the sole responsibility of the user. While we have attempted to ensure that these data are accurate and reliable, BML/BOON makes no warranty, expressed or implied, as to the accuracy, completeness, or utility of this information, nor does the fact of distribution constitute a warranty.

 
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