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The steady trade windscauseeasterly equatorial currents
keep the eastsettingEquatorial current
to leeway the waves and the strong Wsettingequatorial current
oblique approach of waves(passive) created bylongshore current
swell approaching the coast at an angle(passive) caused bylongshore ” current
the relative difference of water levels between two bodies of water separated by a narrow channel(passive) Caused byLongshore Current
this straight line air movementsetsup the equatorial current
This current lies to the north of the westsettingEquatorial Current
enoughto createlongshore current
the radiation stress and the uneven distribution of wave setup induced by the uneven distribution of wave height(passive) is ... caused bylongshore current
The region(passive) is influenced byThe region
the height differential between the western and eastern Pacific to be as much as 1 meter ( 3.3 feetcausesthe height differential between the western and eastern Pacific to be as much as 1 meter ( 3.3 feet
in a westerly direction at thirty to forty miles per daycan setin a westerly direction at thirty to forty miles per day
along the chain of Islandssetting northalong the chain of Islands
angled with the Western edge higher than the eastern edge(passive) caused byangled with the Western edge higher than the eastern edge
directly against the Windward Islandssetsdirectly against the Windward Islands
atmospheric instabilities and affects high frequency and satellite communicationcausesatmospheric instabilities and affects high frequency and satellite communication
to the Old Bahama Channelleadingto the Old Bahama Channel
the waves to approach the shoreline at an anglecausesthe waves to approach the shoreline at an angle
When waves strike a shore at an angle , and then retreat from the beach at an anglecreatesWhen waves strike a shore at an angle , and then retreat from the beach at an angle
beach drift ( also known as longshore driftcausesbeach drift ( also known as longshore drift
the mistake(passive) created bythe mistake