WALLY   BARNES   &   ACCOMPLICES

TIDAL   CURRENTS ...... PART   DUEX



***** The following article appeared in SOURCES,   the NAUI Journal of Underwater Education.   Reprinted here with permission from NAUI.   Our thanks to their staff for permitting us to share this important information with our readers.*****

This article is the second of three parts on the diving impact of tides   and   tidal currents.   Please refer to part one before reading this section as we are expanding concepts explained there.   We repeat that this article is   NOT INTENDED   to be universal,   but general in nature   and   in   NO WAY should be construed to be representative of any particular site.   Users are advised to seek local information regarding differences between the strength   and   timing of tides   and   tidal current maxima   and   slack waters.

ANGLE   AND   DISTANCE OF THE SUN   AND   MOON
Not to get too boring with technicalities,   but let's remember that the sun   and   moon are not always in the same celestial plane.   When they are,   we get an   ECLIPSE   and   the points of maximum centrifugal   and   centripetal force coincide.   Then,   we really are talking about extremely   high HIGH TIDES   and   extreme   low LOW TIDES   ...... and   its consequential extremely strong   TIDAL CURRENTS.   Of course,   eclipses occur on new   or   full moons ...... SPRING TIDES ...... only.

COULD WE COMPLICATE MATTERS MORE ???   Of course !!!   We could indicate that the moon,   at its closest distance (perigee) from Earth,   the stronger its influence.   By the same token,   the farther the distance,   the lesser the effect over the tides.   With a decreased moon effect,   the lesser the change of tidal height.   Remember,   the higher (or lower) the tide,   the stronger (or weaker) the tidal current ...... and   this is what divers must understand to avoid a face to face encounter with a strong tidal current.   We could also add meteorological effects on currents,   like strong wind blowing   or   water accumulating against land masses   and   rushing back   or   rivers   and   estuaries discharging unusual amounts of water causing currents.   But things are stuffy enough the way they are to add those irregular   and   highly unpredictable events.   Let's stick to tides   and   its currents.
This was the case of our last   "Wreckers Delight"   Liveaboard trip to the Florida Keys (see window in main menu) ...... where we visited the Duanne,   the Bibb   and   the Eagle Wrecks (all deep wrecks) in one weekend.   We just had an eclipse the day before departure,   under a gorgeous harvest full moon which was just in its perigee the day before ...... and   believe it,   all those factors made the current streak by really howling!!!

HOW TO USE TIDE TABLES
Divers don't need a PhD to tell them that currents are critical to a person jumping from a boat   and   swimming underwater several hundred feet away.   A diver's average speed is about 100 ft/minute,   which is around one knot   or   one mile per hour (give   or   take).   A diver can usually cope with currents less than 60 ft/minute ...... anything above that would cause over-stress   and   exertion (depending on stamina,   equipment   and   physical conditions).   Tidal currents can vary from zero to well above 200 ft/min ...... that's why dive planning   MUST   include the tidal current factor in it.
Let's get into the nitty gritty of the article.   When a region in the ocean is at high tide,   we assume water is no longer coming in (otherwise the level would continue to rise).   That means the incoming current is   ZERO.   The same logic follows for low tide.   When at low tide time,   no water is outgoing   or   the level would continue to fall.   The TIDAL CURRENT AT THE TIME OF HIGH   OR   LOW TIDE IS NEAR ZERO,   or   at least so weak (less than 20ft/min),   we call it  SLACK   water.   Returning to our original point of high tide, ...... now the water will begin to flow toward other sites which have rising levels   and   a tidal current starts.   Slowly at first ...... then stronger   and   stronger ...... until a maximum strength is reached at about halfway to the next (low) tide time ...... roughly three hours (since we have six hours between high   and   low tide).   From that maximum at the midway point,   it begins to weaken until it reaches a ZERO again at the next tide time.
In the tide tables,   the information you need is the time of the high   and / or   low tide.   We will consider these times as the slack (near zero) current.   We will then estimate that halfway between the slack times,   the current will be at its maximum strength.

EXAMPLE :
With a high tide at 13:03 (1:03pm)   and   a low tide at 19:21 (7:21pm) ...... we start with slack current (near zero) at 1:00pm.   Then,   there will be a weak out-going movement getting progressively stronger until 4:10pm,   when it reaches its maximum speed,   then weakening until it is back to near ZERO at 7:20pm (time of low tide).   It will now reverse the flow   and   a weak incoming current will start rising the water level becoming stronger   and   reaching maximum strength halfway to the next high tide ...... at which time it will zero again   and   start the cycle all over.
We now know when the currents are going to be stronger   or   weaker,   but how strong???   The answer is in the moon phase.   At  SPRING TIDE   ...... new   or   full moon ...... that maximum current is bound to be very strong   and   should be avoided by divers ...... unless,   of course,   you are doing a drift dive.   If you are planning a reef dive that day,   make sure you're in the water very close to 1:00pm with the   SLACK   current   and   out of the water before 2:30pm when the increase in current speed becomes sudden and dangerous.   On the other hand,   if that dive was planned during a   NEAP   tide ...... first   or   last quarter moon ...... the dive could be carried out even at 4:00pm since its strength is NOT likely to be extreme.   AGAIN,   THESE ARE GENERAL CONCEPTS OF TIDAL CHANGES   AND   DO NOT APPLY UNIVERSALLY TO ALL PLACES   AND   AT ALL TIMES.   CONSULT YOUR LOCAL DIVING AUTHORITIES WHEN IN DOUBT   OR   TO LEARN LOCAL FACTORS INFLUENCING THESE CONCEPTS.

Check your local tide tables,   notice the height of the high tide   and   of the low tide;   open ocean differences of three (3) ft   or   more usually cause currents well above 60 ft/min.   In the above example,   dive near the time of high   or   low tide ...... when the current is SLACK (high tide,   because it brings clean water from the deep sea is usually clearer than low tide which normally brings dirty water from nearshore).   During NEAP tides,   the difference from high tide to low tide is small (less than 1.5 ft)   and   the water rush is NOT too strong,   so your timing is not really critical.   Of course,   if your swimming skills are not fully developed,   don't take chances,   dive when the currents are slack whether it is SPRING   or   NEAP tide.
Where can you get tide information ???   That's the easiest one.   Check your local newspaper,   your TV weather reports   or   even radio.   Even yesterday's data is good,   just add one hour to that time for as good approximation.

To quickly summarize what we have discussed here :
ONE......Tidal currents are SLACK near low   or   high tide time.   That's four times a day.   Maximum current speed is halfway between tide times.
TWO ......Strong maxima during SPRING TIDES ( full   or   new moon).   Weak maxima when NEAP tides (first   or   last quarter moons).
THREE ....Your local newspaper carry the tide time information   or   local TV weather reports.
Now that we know how tides relate to current,   its effect on divers   and   the times to avoid strong tidal currents ...... and   just as important ...... how   and   where to get this information,   we can make it an integral part of our dive plan.   It is only to your own benefit   and   safety.   Many books emphasize this importance.   Now you know how to use it!!!
On the third part of this article,   "PART TROIS",   we discuss deviations from these generalities   and   quantifying some of the strong   or   weak currents.   Then a knowledgeable diver can better prepare to cope with strong currents   or   weak ones as the case might be.

STAY TUNED TO THIS STATION !!!!

Any comments,   complaints,   gripes,   grumbles,   grief,   laments   or   accusations can be addressed to our webslave ...... Wally Barnes

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