B41009 SA 2300 153/80/82/0808G12/ APP MMMM SWL 0803  10M 08  20M 09
B41009 SA 2100 154/80/82/0710G12/ APP MMMM SWL 0703  10M 10  20M 10
B41009 SA 1900 165/80/82/0708G10/ APP MMMM SWL 0703  10M 08  20M 08
B41009 SA 1800 172/80/82/0506G06/ APP MMMM SWL 0803  10M 05  20M 05

B41010 SA 2300 159/80/82/3606G08/ APP 6007 SWL 0704  10M 07  20M 07
B41010 SA 2200 158/80/82/3608G10/ APP 6012 SWL 0804  10M 08  20M 08
B41010 SA 2100 160/80/83/3508G10/ APP 7016 SWL 0804  10M 08  20M 08
B41010 SA 2000 166/80/83/3506G08/ APP 8013 SWL 0903  10M 06  20M 07
B41010 SA 1900 170/80/83/3504G06/ APP 8012 SWL 0803  10M 04  20M 04

23 June 1999 buoy data.  Basically there was a light northerly gradient wind which is depicted well by the data at Buoy 41010.  The easterly winds at Buoy 41009 were exagerated due to the effect of the sea breeze.  Sea heights of 3-4 feet do not look very impressive, especially with a 7-9 second period, but most of this was likely swell as the local winds were very light.  Also, inspection of detailed wave data from the National Data Buoy Center showed that there were occasional longer periods.  This did not show up in the locally generated buoy data since the occasional 14 second periods had wave heights of only 1.0-1.5 feet.  The reason for this is that the program shows the dominant wave period (the wave period associated with the highest wave), which in this case was the 7-9 second period associated with 2-3 ft seas.