Ocean swells are generated by storms blowing at sea, far from California.  As the storm-generated waves move away from the storm area, the longer waves move faster, and thus separate from the shorter waves.  This process of waves separating from each other according the the wave length is called dispersion..  As a result of dispersion, waves arriving in California which were generated by a single storm are mostly of one wave period, wavelength, and wave height.  

A swell arriving in California may encounter another swell, generated by a different storm, arriving from a different direction,with a different period and wavelength.  As these two (or more) swells interact, the phenomenon of wave interference  occurs.  Thus as two wave crests interact, a higher wave will result.  Similarly, as two troughs interact, a deeper trough is generated.  Also a wave crest and wave trough can interact to cancel each other, or interact destructively.

As swells appoach shallower water, they slow down and bend to become more nearly parallel to the shoreline.  This is called refraction.  It can cause wave energy to be focused on some areas, such as points of land, and cause wave energy to be lessened in other areas.  Also, as waves refract and bend around small islands or shallow areas, they may interact on the side away from the swell direction, and may cause large waves to develop there.

The combination of these factors, dispersion, wave interference, and refraction, lead to complex patterns in which wave height in California can be quite variable from area to area.  However, by measuring the direction, period and height of a swell or swells on offshore buoys or platforms, and by using information about the shape of the seafloor, scientists can predict wave height in Southern and Central California.  Such work is being performed by the Coastal Data Information Program..

The image shown here is the Southern California swell prediction generated by the CDIP (Coastal Data Information Program) for Dec. 3, 1996.  Examine the image, then answer the questions below, which also appear in your lab handout.

There are a number of important features to notice in the image shown above.  First, notice that the wave height is indicated in various colors, and that a color scale at the lower part of the image shows what colors correspond to which wave heights.  Second, there is a semi-circular diagram in the left part of the image which shows, graphically, the direction and period of the swell or swells approaching Southern California.  Finally, to the right, notice the data concerning the direction, period and height of the waves approaching Southern California.

Notice the high waves along the northwest sides of some of the offshore islands.  

How large are these waves? (Please indicate the height in feet.)

Why are the waves so large in these locations? (Refer back to the introduction if you need to.)

Now examine the California coastline.  What is the approximate latitude and longitude of the area where the highest waves are predicted to occur?

How large are those waves?

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The graph shown below shows predicted wave height along the Southern California coast, from north of Point Conception, west of Santa Barbara, to the Mexican Border.  Examine the graph and answer the questions below.

Where are the waves highest?  

What height (in feet) are they predicted to be?

How do you explain the waves being highest in that location?  (Note: you may want to refer back to the previous image in order to answer this question.)

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The image shown below is portion of the Southern California Swell Prediction, this one covering only the San Diego area.  Examine it then answer the questions below.

Where along the coastline in San Diego are the waves predicted to be the highest? (Give your answer in latitude and longitude)

How high are they predicted to be?

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The graph shown below is a portion of the coastal wave height prediction.  Examine it and answer the questions below.

Where will the waves be highest along the coastline in San Diego County, and how high will they be?

Where will they be lowest, and how small will they be?

Which of these places would you pick to go surfing?

What factors, other than wave height, might you consider before you put your surfboard into your car and head for the beach? (Think of everything you can, including possible non-oceanographic factors.)

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The image shown below is one from July when there was a strong south swell.  Examine it and compare it to the Southern California Swell Prediction which you examined at the beginning of this lab exercise.  Then answer the questions below.

Compare the size, direction and period of the south swell to that which we viewed at the beginning of this lab, and describe where the waves are larger during the south swell, and where they are smaller compared to the data set we viewed earlier.

Notice the area of large wave size near 32.5 degrees north, 119 degrees west (indicated with arrows on the image).  These areas of large swell are immediately northeast of shallow areas of the seafloor known as Cortes Bank and Bishop Rock.  How do you explain these areas of high swell?  (Note: you may want to return to the Introduction to refresh your memory.)

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Examine the image shown here, and answer the questions below.

Describe how the swells on this date are different from the images we saw earlier.

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The image below is a swell prediction from December 11, 1996, based on data from a buoy located in the Monterey Bay area.  Examine the diagram, then answer the questions below.

Where are the largest waves predicted to be striking the shoreline, how high will they be, and what is their period?

How do these values compare to those we observed from December 3 in Southern California?

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Finally, let's consider the latest swell prediction for Southern California.  Click here to access the latest image. (It may take a few minutes to access the computer at UCSD and download the image!)  Then answer the following questions.

What is the date and time of the swell prediction?

What is (or are) the swell direction(s), period(s) and heights?

Where along the shoreline are the waves expected to be largest (give the latitude and longitude), and how large are they expected to be?

Will the surfing be any good in the San Diego area, based on this prediction?