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From: Sisler, Clyde <Clyde.Sisler_at_wang.com>
subject: [Paddlewise] Tides & Currents
Date: Tue, 26 Jan 1999 08:20:38 -0500
I was struck by the number of times tidal currents played a role in the
accidents in the book Deep Trouble.  The term 'swept out to sea' stirs up
some pretty scary images but how bad can it really be?  Given that a person
can stay in the boat, how far out can they be swept?  A mile, two miles?
Even at full ebb, the tidal (not ocean) current has to dissipate somewhere.

Granted one might well spend some uncomfortable hours and then have to
paddle back, but still......
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From: Richard Culpeper <culpeper_at_geocities.com>
subject: Re: [Paddlewise] Tides & Currents
Date: Tue, 26 Jan 1999 08:46:39 -0500
One of my friends, Duncan Taylor, while in view of his wife on shore, was
swept out to sea while kayaking at a beach in Maurtius.  Despite an
intensive air-sea search, no trace of him was ever found.

Richard Culpeper
www.geocities.com/~culpeper

----------
> From: Sisler, Clyde <Clyde.Sisler_at_wang.com>
> To: 'Paddlewise' <paddlewise_at_lists.intelenet.net>
> Subject: [Paddlewise] Tides & Currents
> Date: Tuesday, January 26, 1999 8:20 AM
> 
> I was struck by the number of times tidal currents played a role in the
> accidents in the book Deep Trouble.  The term 'swept out to sea' stirs up
> some pretty scary images but how bad can it really be?  Given that a
person
> can stay in the boat, how far out can they be swept?  A mile, two miles?
> Even at full ebb, the tidal (not ocean) current has to dissipate
somewhere.
> 
> Granted one might well spend some uncomfortable hours and then have to
> paddle back, but still......
>
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From: R. Walker <rww_at_mailbox.neosoft.com>
subject: Re: [Paddlewise] Tides & Currents
Date: Tue, 26 Jan 1999 10:59:49 -0600
> One of my friends, Duncan Taylor, while in view of his wife on shore, was
> swept out to sea while kayaking at a beach in Maurtius.  Despite an
> intensive air-sea search, no trace of him was ever found.

I could not find this placename.  I did find a place "Mauritius", an 
island off the East coast of Madagascar.   I guess the question 
there becomes, did he have a GPS and compass?  I think most of 
us ocean paddlers always have the fallback position of being able 
to select the general direction of the coast line, paddling 
perpendicular to the current for some distance, and then heading 
for shore.   A person swept out to sea off an isolated island has a 
much more difficult problem, in that their default safe return course 
can't be assumed like "if I head west or north, I can't help but hit 
land."   A lesson here I suppose is that if you aren't surrounded by 
land like on a lake, be sure to have an adequate water supply and 
navigational gear that will allow a return from 20 miles out in any 
random direction.

Even if you are just surfing, how hard can it be to slip a pre-packed 
drybox and a couple 2 liter bottles of water in your rear hold.


Richard Walker
Houston, TX
http://www.neosoft.com/~rww/kayak_log.html
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From: Sisler, Clyde <Clyde.Sisler_at_wang.com>
subject: RE: [Paddlewise] Tides & Currents
Date: Tue, 26 Jan 1999 09:33:09 -0500
One of my friends, Duncan Taylor, while in view of his wife on shore, was
swept out to sea while kayaking at a beach in Maurtius.  Despite an
intensive air-sea search, no trace of him was ever found.

--------------

That must have freaked his wife out.  What kind of skills and wind & wave
conditions?
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From: Bob Denton <BDenton_at_aquagulf.com>
subject: RE: [Paddlewise] Tides & Currents
Date: Tue, 26 Jan 1999 10:58:20 -0500
Here in Florida, if you're swept into the Gulf Stream, about 3 miles off
shore, you can end up in Ireland.... Far enough?!
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From: Bob Denton <BDenton_at_aquagulf.com>
subject: RE: [Paddlewise] Tides & Currents
Date: Tue, 26 Jan 1999 11:01:00 -0500
My brother lives on Mauritius. When was this and where? Gran Bay?

> -----Original Message-----
> From: owner-paddlewise_at_lists.intelenet.net
> [mailto:owner-paddlewise_at_lists.intelenet.net]On Behalf Of Richard
> Culpeper
> Sent: Tuesday, January 26, 1999 8:47 AM
> To: Sisler, Clyde; 'Paddlewise'
> Subject: Re: [Paddlewise] Tides & Currents
> 
> 
> One of my friends, Duncan Taylor, while in view of his wife 
> on shore, was
> swept out to sea while kayaking at a beach in Maurtius.  Despite an
> intensive air-sea search, no trace of him was ever found.
> 
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From: Richard Culpeper <culpeper_at_geocities.com>
subject: Re: [Paddlewise] Tides & Currents
Date: Tue, 26 Jan 1999 11:41:16 -0500
Yes, it did.  It hurt many people, for Duncan was a very special person who
had touched many lives.

He was an experienced inland wilderness canoeist (and for many years was
president of the Wilderness Canoe Association), but was inexperienced at
kayaking and ocean paddling.  He was at a resort on the south side of the
island, where he came upon a kayak rental on the beach.  He rented one and
went for a spin, so he had no understanding of the local conditions, and no
proper equipment, water, etc.  The conditions were pleasant, with some
waves out from shore.  His wife described him bobbing along and, as he got
further out, disappearing from sight between the waves.  There is a
possibility that he was dumped in these waves, but this does not explain
his disappearance.  The consensus is that he ended up in the ocean current
(either in or out of his boat), heading for Africa, and air-sea serches
were mounted to that effect.  It looks like he had enough technique to
paddle into trouble, but not enough experience with salt water ocean sea
kayaking to have avoided troube in the first place.

Richard Culpeper
www.geocities.com/~culpeper

----------
> From: Sisler, Clyde <Clyde.Sisler_at_wang.com>
> To: 'Paddlewise' <paddlewise_at_lists.intelenet.net>
> Subject: RE: [Paddlewise] Tides & Currents
> Date: Tuesday, January 26, 1999 9:33 AM
> 
> One of my friends, Duncan Taylor, while in view of his wife on shore, was
> swept out to sea while kayaking at a beach in Maurtius.  Despite an
> intensive air-sea search, no trace of him was ever found.
> 
> --------------
> 
> That must have freaked his wife out.  What kind of skills and wind & wave
> conditions?
>
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From: Bob Denton <BDenton_at_aquagulf.com>
subject: RE: [Paddlewise] Tides & Currents
Date: Tue, 26 Jan 1999 12:21:21 -0500
Mauritius is similar to many of the Caribbean or Hawaiian islands. It's a
pleasant, non threatening tourist environment and one really wouldn't be too
concerned about currents, etc. I have seen the kayaks, and they are for rent
at most of the typical tourist hotels. They are actually fg SOTs and well
made. Of course most tourists paddle around the lagoon, but if he paddled
through the reef, then he may have been swept away or dumped on the reef and
eaten.

There was a case of a guy who rented a jet ski in Cancun a few years ago and
was never seen alive (or dead) again. His wife paid thousands for an air
search and had her credit card debited for the cost of the ski.

Just because the water is blue, flat and warm, doesn't mean it's a walk in
the park!

cya
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From: K. Whilden <kwhilden_at_u.washington.edu>
subject: Re: [Paddlewise] Tides & Currents
Date: Tue, 26 Jan 1999 17:20:49 -0800 (PST)
Hi Clyde,

If I recall correctly, most of the accidents involving currents in Deep
Trouble were problems specificly associated with crossing eddylines. The
eddyline caused a flip, thus leaving the paddler at the mercy of the
currents. In the two stories I am thinking of, the paddlers were unable to
self-rescue the boats because of swamping and lack of adequate flotation,
but if those paddlers could have self-rescued, it would have been possible
for them paddle back to shore fairly easily. In the San Juans at least,
the currents usually are not faster than fast paddling speed except for
localized areas near shore where the current speeds up (e.g. eddylines and
tide rips). These local areas are fairly easy to paddle around, given a
rudimentary knowledge of currents and eddylines. Sometimes though, it is
impossible to avoid being swept into an eddyline, which is why I
evangelize a little bit of whitewater experience even for those who never
plan to take up whitewater as a sport. It doesn't take much practice on
the river to be able to handle eddylines with ease.

Cheers,
Kevin
Kayak Academy Whitewater Instructor
http://www.halcyon.com/kayak



On Tue, 26 Jan 1999, Sisler, Clyde wrote:

> I was struck by the number of times tidal currents played a role in the
> accidents in the book Deep Trouble.  The term 'swept out to sea' stirs up
> some pretty scary images but how bad can it really be?  Given that a person
> can stay in the boat, how far out can they be swept?  A mile, two miles?
> Even at full ebb, the tidal (not ocean) current has to dissipate somewhere.
> 
> Granted one might well spend some uncomfortable hours and then have to
> paddle back, but still......
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From: Richard Strickland <rstrix_at_yahoo.com>
subject: Re: [Paddlewise] Tides & Currents
Date: Tue, 26 Jan 1999 22:36:22 -0800 (PST)
As a local oceanographer and kayaker with some experience in and
knowledge of the San Juans and similar regional waters (although not
as much as K. Whilden's fabled employer at Kayak Academy), I would
like to make several points of fact and/or opinion:

1) The other answers to Clyde's question, regarding Mauritius, did not
seem to address his point about "tidal" as opposed to "ocean"
currents. Tidal currents are inherently oscillatory with about a 6.25-
or 12.5-hour average period, depending on location. Hence Clyde's
suggestion that if one could stay with (preferably IN) the boat long
enough, one should return to one's approximate starting point in half
a day at most. Large-scale wind-driven ocean ocean currents (such as
those around Mauritius), in contrast, are generally unidirectional for
long periods of time. Any prevaling local wind and wave transport
would add to the latter hazard. 

2) In a statistical sense, Kevin may be correct that "currents usually
are not faster than fast paddling speed," i.e., over a majority of the
area for a majority of hours on an annual basis. However, there are
several channels in the San Juans where currents exceed 2-3 knots over
most of their width and length for several hours a day and for several
successive days during spring tidal periods (around new/full moon),
especially during May-July and November-January. That's fast for me to
paddle for a period of hours (shorter burst are OK). Maximum currents
exceed 4 knots in many areas during these times. Thus I would argue
that strong currents are common enough to get the uneducated paddler
into conditions where he/she could not control his/her position for
several hours at a time. P.S. This happened to me in my greener years.

3) Many experienced paddlers I've met also seem to assume that slack
currents are synchronous with high and low water. In the San Juans, as
in many other narrow channels, however, currents and water levels are
commonly (not always) out of phase, often by as much as 1-2 hours or
more. Failure to read tidal current tables instead of tidal height
tables is particularly dangerous where high/low water occurs AFTER
slack, such as occurs in Deception Pass (8 knot maximum currents), so
that the unwary paddler would potentially launch into an accelerating
current.

4) There are large open-water areas in the San Juan vicinity, as well
as long channels, both of which may have strong currents over broad
areas (tens of miles). It is not hard for a paddler to piggyback tidal
currents intentionally for 10-12 miles on a  single tidal cycle in
some places, so the displacements in an accidental scenario can be
greater than what Clyde is visualizing. Furthermore, distance from
shore would logically seem to diminish the odds of rescue.

5) The complex current patterns in the San Juan area, including large
scale eddies and significant differences in the timing of current
stages over short distances, could easily result in a paddler not
being able to retrace his/her path when the current reversed, but
rather being entrained into another channel altogether.

6) The bottom line, to amplify Kevin's point, is that being "swept out
to sea" is not so much the issue (in the San Juans, anyway), so much
as being swept uncontrollably into areas with hazardous conditions
such as eddylines, tide rips, high seas, or oil tankers :-(.

Thank you for listening to my sermon.

Richard Strickland
Seattle

---"K. Whilden" <kwhilden_at_u.washington.edu> wrote:

> If I recall correctly, most of the accidents involving currents in
Deep
> Trouble were problems specificly associated with crossing eddylines.
The
> eddyline caused a flip, thus leaving the paddler at the mercy of the
> currents. 

[SNIP]

> In the San Juans at least,
> the currents usually are not faster than fast paddling speed except
for
> localized areas near shore where the current speeds up (e.g.
eddylines and
> tide rips). These local areas are fairly easy to paddle around,
given a
> rudimentary knowledge of currents and eddylines. Sometimes though,
it is
> impossible to avoid being swept into an eddyline...

> On Tue, 26 Jan 1999, Sisler, Clyde wrote:
> 
> > I was struck by the number of times tidal currents played a role
in the
> > accidents in the book Deep Trouble.  The term 'swept out to sea'
stirs up
> > some pretty scary images but how bad can it really be?  Given that
a person
> > can stay in the boat, how far out can they be swept?  A mile, two
miles?
> > Even at full ebb, the tidal (not ocean) current has to dissipate
somewhere.
> > 
> > Granted one might well spend some uncomfortable hours and then
have to
> > paddle back, but still......


_________________________________________________________
DO YOU YAHOO!?
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From: K. Whilden <kwhilden_at_u.washington.edu>
subject: Re: [Paddlewise] Tides & Currents
Date: Tue, 26 Jan 1999 23:07:29 -0800 (PST)
On Tue, 26 Jan 1999, Richard Strickland wrote:
<snip>
> 2) In a statistical sense, Kevin may be correct that "currents usually
> are not faster than fast paddling speed," i.e., over a majority of the
> area for a majority of hours on an annual basis. However, there are
> several channels in the San Juans where currents exceed 2-3 knots over
> most of their width and length for several hours a day and for several
> successive days during spring tidal periods (around new/full moon),
> especially during May-July and November-January. That's fast for me to
> paddle for a period of hours (shorter burst are OK). Maximum currents
> exceed 4 knots in many areas during these times. Thus I would argue
> that strong currents are common enough to get the uneducated paddler
> into conditions where he/she could not control his/her position for
> several hours at a time. P.S. This happened to me in my greener years.

Hi Richard,

Thanks for your very informative post! I intentionaly left out of my post
any reference to large spring currents and some of the constricted
channels such as Obstruction Pass where currents can get faster than
maximum paddling speed. I wanted to see if anyone was paying attention.
You passed my informal and probably unnecessary test with flying colors.
In fact, considering how much I learned from your post, maybe I should do
this kind of thing more often. Nah...

Now one more comment about paddling against currents. Don't do so unless
absolutely necessary! It is far too much work and effort, and very
difficult if the current is above three knots. It is very difficult to
paddle against even a one knot current, and three knot current is almost
impossible except for short distances.  It is much better to plan to
paddle with the current. One of my favorite trips in the San Juans is to
paddle from Washington Park on Fidalgo Island to Doe Bay on Orcas Island,
leaving just as the current turns to a spring flood. First there is the
challenging ferry glide across a current that goes 90 degrees to the
direction of travel. This is great practice for using ranging navigational
techniques. Then there is a fabulous tide rip on strawberry island to play
and surf. And then for the finale, there is a ride on the Rosario Strait
Express current with a stop at Doe Bay for a hot tub soak. A lot of fun
indeed. Last time I did this trip, we made the 8 nmi one-way distance in
2:04 hours, including a 30 minute stop to play at the rip.

So the moral of the story, if there is one, is to let the currents do the
work for you, but also learn about eddylines, because they are
inseperable.

Lot's o' speedy paddling,
Kevin

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From: Barbara Kossy <bkossy_at_igc.apc.org>
subject: Re: [Paddlewise] Tides & Currents
Date: Wed, 27 Jan 1999 05:49:12 -0800 (PST)
Here abouts in the San Francisco Bay Area there are a number of paddles
easily done "against" the current. We use the reversal currents behind the
points to push us along. Then scoot around the points and into the opposing
currents, and pop back into the reversals.
The key is knowing local conditions.
Barbara 

At 11:07 PM 1/26/99 -0800, K. Whilden wrote:
>
>On Tue, 26 Jan 1999, Richard Strickland wrote:
><snip>
>> 2) In a statistical sense, Kevin may be correct that "currents usually
>> are not faster than fast paddling speed," i.e., over a majority of the
>> area for a majority of hours on an annual basis. However, there are
>> several channels in the San Juans where currents exceed 2-3 knots over
>> most of their width and length for several hours a day and for several
>> successive days during spring tidal periods (around new/full moon),
>> especially during May-July and November-January. That's fast for me to
>> paddle for a period of hours (shorter burst are OK). Maximum currents
>> exceed 4 knots in many areas during these times. Thus I would argue
>> that strong currents are common enough to get the uneducated paddler
>> into conditions where he/she could not control his/her position for
>> several hours at a time. P.S. This happened to me in my greener years.
>
>Hi Richard,
>
>Thanks for your very informative post! I intentionaly left out of my post
>any reference to large spring currents and some of the constricted
>channels such as Obstruction Pass where currents can get faster than
>maximum paddling speed. I wanted to see if anyone was paying attention.
>You passed my informal and probably unnecessary test with flying colors.
>In fact, considering how much I learned from your post, maybe I should do
>this kind of thing more often. Nah...
>
>Now one more comment about paddling against currents. Don't do so unless
>absolutely necessary! It is far too much work and effort, and very
>difficult if the current is above three knots. It is very difficult to
>paddle against even a one knot current, and three knot current is almost
>impossible except for short distances.  It is much better to plan to
>paddle with the current. One of my favorite trips in the San Juans is to
>paddle from Washington Park on Fidalgo Island to Doe Bay on Orcas Island,
>leaving just as the current turns to a spring flood. First there is the
>challenging ferry glide across a current that goes 90 degrees to the
>direction of travel. This is great practice for using ranging navigational
>techniques. Then there is a fabulous tide rip on strawberry island to play
>and surf. And then for the finale, there is a ride on the Rosario Strait
>Express current with a stop at Doe Bay for a hot tub soak. A lot of fun
>indeed. Last time I did this trip, we made the 8 nmi one-way distance in
>2:04 hours, including a 30 minute stop to play at the rip.
>
>So the moral of the story, if there is one, is to let the currents do the
>work for you, but also learn about eddylines, because they are
>inseperable.
>
>Lot's o' speedy paddling,
>Kevin
>
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>

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From: Sisler, Clyde <Clyde.Sisler_at_wang.com>
subject: RE: [Paddlewise] Tides & Currents
Date: Wed, 27 Jan 1999 09:02:36 -0500
Thanks for your very informative post! I intentionaly left out of my post

------------
I add my thanks also, Richard, that was a great post although I personally
wouldn't have thought of oscillatory as an adverb.  Cyclical, maybe.
Oscillatory, I don't think so!  :-).
------------

Now one more comment about paddling against currents. Don't do so unless
absolutely necessary! It is far too much work and effort, and very

------------
The image I have now of the Deep Trouble reports is of people paddling
madly, more from reaction, adrenilin and fear than with any plan or
objective in mind.  This eventually would lead to fatigue and even less
control of the boat and the situation.

The thought behind my post was simply being caught in a current I couldn't
overcome or evade and being swept past the last point of land.  Rather than
paddling wildy to obtain an unreachable objective I thought it might make
more sense, under the right circumstances, to conserve energy, stay upright
and (wishfully) trying to ferry out of the current if/when conditions
permitted.

Granted wind, waves, skill, fatigue, etc. all come into play along with the
current but I didn't/don't think being swept past that last point of land is
neccessarily a death sentence, at least not most of the time.

I agree with another post that some whitewater experience would be
invaluable.  Being able to punch in and out of an eddyline without leaning
the wrong (natural) way is important (and fun) as is ferrying or setting
(isn't that what they call ferrying while heading with the current?).  How
else are ya gonna get out to those standing waves for a little surfing?  :-)

My whitewater canoeing is 20+ year old but little bits and pieces seem to
surface when needed.
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From: Richard Culpeper <culpeper_at_geocities.com>
subject: Re: [Paddlewise] Tides & Currents
Date: Wed, 27 Jan 1999 10:09:34 -0500
Aside from the issue of being swept by the tide out into something such as
an ocean current, there is also the problem of what might happen out in the
briny even if the tide will pretty much bring you back.  Sometimes walking
back is not feasible (due to deep water channels and mud flats), leaving
you unprotected for extended periods where a shift in the wind could build
some nasty breakers in the shallows (e.g. Hannah Bay at the southern edge
of Hudson's Bay).  

(BTW, when I was a youngster I bunged up an empty oil barrel, lashed some
driftwood to it, and happily floated out with the tide from our cottage on
Oak Bay on the Bay of Fundy.  I bobbed about until the tide brought me back
in again.  I did not realize that I would be out for so long, so I was
expecting my folks to be angry with me.  As it was, they were not, for as I
later learned from my mother, she had spent a fair number of years as a
child bobbing in and out with the tide, and thought nothing of swimming for
extended periods.  Sometimes I wonder how she and her siblings ever
survived to adulthood.)

Cheers,
Richard Culpeper
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From: Richard Strickland <rstrix_at_yahoo.com>
subject: Re: [Paddlewise] Tides & Currents
Date: Wed, 27 Jan 1999 14:36:46 -0800 (PST)
> Here abouts in the San Francisco Bay Area there are a number of
paddles
> easily done "against" the current. We use the reversal currents
behind the
> points to push us along. Then scoot around the points and into the
opposing
> currents, and pop back into the reversals.
> The key is knowing local conditions.

True fact, Barbara, in the San Juans as well as that other San. Using
hte back eddies was how I saved my tush when I misread the currents in
the "greener" days I referred to.

Richard in Seattle

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From: Richard Strickland <rstrix_at_yahoo.com>
subject: RE: [Paddlewise] Tides & Currents
Date: Wed, 27 Jan 1999 15:00:28 -0800 (PST)
> I personally
> wouldn't have thought of oscillatory as an adverb.  Cyclical, maybe.
> Oscillatory, I don't think so!  :-).
> ------------

To quote: "Tidal currents are inherently oscillatory.." In this usage,
"inherently" is an adverb and "oscillatory" is an adjective.The adverb
(if one accepted its existence) would be "oscillatorily," meaning "in
an oscillatory fashion." Didn't know I was an editor, too, did you?

> ------------
> The image I have now of the Deep Trouble reports is of people paddling
> madly, more from reaction, adrenilin and fear than with any plan or
> objective in mind.  This eventually would lead to fatigue and even
less
> control of the boat and the situation.

Agreed.

> The thought behind my post was simply being caught in a current I
couldn't
> overcome or evade and being swept past the last point of land. 
Rather than
> paddling wildy to obtain an unreachable objective I thought it might
make
> more sense, under the right circumstances, to conserve energy, stay
upright
> and (wishfully) trying to ferry out of the current if/when conditions
> permitted.

Certainly wasting energy to reach an unreachable objective is not
intelligent paddling, and conserving energy when possible is.

> Granted wind, waves, skill, fatigue, etc. all come into play along
with the
> current but I didn't/don't think being swept past that last point of
land is
> neccessarily a death sentence, at least not most of the time.

That may be generally so. I don't know where you paddle, but anyone
who has been to the San Juans should appreciate the other
generalization I was trying to make about them--that difficult sea
conditions are common enough that current/wind/wave conditions do more
than "come into play." I would argue that they are often the dominant
factors one must deal with. I do not generally advocate exhaustion,
and I do unequivocally favor paddling/bracing/rescue skills. However,
I have been in situations in the San Juans where some strong,
sustained effort exerted at the right time in the right direction kept
me in moderate sea conditions when currents that I had not anticipated
were trying to take me someplace really ugly. An ability to read the
water and anticipate and avert impending danger (if possible) is as
much of a paddling skill as bracing, etc.

Richard in Seattle 
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From: K. Whilden <kwhilden_at_u.washington.edu>
subject: RE: [Paddlewise] Tides & Currents
Date: Fri, 29 Jan 1999 11:50:11 -0800 (PST)
On Wed, 27 Jan 1999, Richard Strickland wrote:

> 
> That may be generally so. I don't know where you paddle, but anyone
> who has been to the San Juans should appreciate the other
> generalization I was trying to make about them--that difficult sea
> conditions are common enough that current/wind/wave conditions do more
> than "come into play." I would argue that they are often the dominant
> factors one must deal with. 

Agreed! Although there are areas in the San Juans where currents are
small, and also times of the month away from full or new moons can be
fairly benign current wise. Still, there are always local areas of strong
currents (i.e. rips) that are easy for the unwitting paddler to be swept
into and encounter trouble.

I do not generally advocate exhaustion,
> and I do unequivocally favor paddling/bracing/rescue skills. However,
> I have been in situations in the San Juans where some strong,
> sustained effort exerted at the right time in the right direction kept
> me in moderate sea conditions when currents that I had not anticipated
> were trying to take me someplace really ugly. An ability to read the
> water and anticipate and avert impending danger (if possible) is as
> much of a paddling skill as bracing, etc.
> 
Here here! This is something I have been saying for quite a while. The
abilty to read the water, which means to be able to pick up the subtle
clues from waves and currents, is every bit as important as knowing how to
brace or roll, or even paddle in a straight line. Unless you paddle
exclusively on glassy lakes, there will be sometime when you will
encounter locally rougher conditions due to a current/wind/wave
interaction. being able to spot this in time to avoid it, or to know even
in which direction the current is flowing requires practice. And where
does one get the most effective and safest practice at reading rough
water and wind/wave/current interactions?
(Note: at the risk of sounding like a broken record....)
The river!!

When I first started teaching the whitewater course for George Gronseth, I
had not clued into the importance of reading water. Now I know it is
crucial to developing basic paddling skills. Most beginning river paddlers
neglect this skill on a conscious level, but if they keep paddling, it
eventually becomes instinctual. The challenge for me was learning how to
teach instincts in only two days, because half of my students have no
intention of taking up river kayaking, but are taking the class one to
improve their sea kayaking skills. More than any other thing, I have to
remind my students to think about reading the river. All of the other
skills become much easier to use once the students know exactly where and
when to apply them.

An analogy that I like is the equate reading the water with knowing the
rhythm when partner-dancing. In salsa or swing for instance, knowing all
of the steps, spins, and moves is one thing, but without rhythm this is
pretty much useless. With rhythm, all of those steps, spins and twirls are
effortless and look and feel great!

Cheers,
Kevin Whilden
The Kayak Academy (http:www.kalcyon.com/kayak)



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From: Richard Strickland <rstrix_at_yahoo.com>
subject: Re: [Paddlewise] Tides & Currents
Date: Fri, 29 Jan 1999 15:58:51 -0800 (PST)
---Dave Kruger <dkruger_at_pacifier.com> wrote:
> > ... That is, maximum forward speed (maximum flood)
> > would coincide with high water (as the wave crest passes), max ebb
> > would occur at low water (wave trough), and slacks would occur
halfway
> > between. This model conforms to the two observations you made
(below):
> > slacks are (ideally) 3 hours out of phase with high/low water, and
> > currents are the derivative of the heights (since sine and cosine
are
> > derivatives of each other and 90 degrees out of phase).
> 
> Richard, there is an inconsistency in the above.  I
> think if  "currents are the derivative of the heights"  then max
current
> should occur mid-tide, not at max-tide (and min-tide), which is what
> "maximum forward speed (maximum flood) would coincide with high water"
> suggests.  I believe you meant to say both tides and currents were
> *in-phase* for this model.  Correct?

I stand corrected before God and Paddlewise. Forgive the hurried-over
math. Max speed at max elevation would indeed be in-phase. (Corrected
by a chemist--oh, the shame of it!)
 
> What we have here corresponds more closely to the "standing wave"
model
> because in model 2), max-tide (and min-tide)
> both correspond roughly to *slack* (attributing the hour or so
offset to
> the effects of superimposed downriver current).  This is the model
which
> has tide height and current velocity 90 degrees out of phase, I
believe.

Right again. I would have to analyze the "offset" to confirm whether
it results from river current. At the risk of getting this mixed up
again in translating my island mentality to a river mentality, the
bias toward ebb generated by the river flow should, over the long
term, make the flood phase of the cycle shorter than the average 6 hrs
25 minutes and the ebb phase longer than that.

As I visualize it, analyzing the relationship of currents to height
would be affected by your position along the river, since there would
be a salt water "front" that would propagate upstream during the flood
and downstream during the ebb. (The leading edge of the front would be
along the bottom and the surface would lag, but it is the surface we
are interested in as paddlers, yes?) Upstream of the front, the
current should always be ebbing even as the water level is rising (at
decreasing speed closer to the front as the front forges upstream
during flood). Downstream of the front, the current & height should be
correlated more as we have discussed. Thus the tidal pattern at a
given site would change as the front swept back and forth past it. So
it would seem to be a fairly complex situation. Perhaps the situation
is simplest in Astoria, close to the mouth.

Maybe some more insights will come to me in the hot tub tonight ;-).
And maybe you have some ground-truth observations to share. I don't
know offhand the river distances over which the tidal front ranges in
the Columbia, but if I recall correctly, tidal effects are felt as far
upstream as Portland.

> The piece of the dialog which really illuminated the difference
between
> what we have here and what happens in the San Juans was this:
> 
> > Currents in that area are considered to be partly hydraulic, that
is,
> > driven by differences in sea level from one side of the channel to
the
> > other. These differences result, for example, when incoming tides
> > "pile up" water on the upstream sides of the islands faster than the
> > water can drain downstream through the channel. Then, when the water
> > level starts falling after high tide, water level is still higher on
> > the upstream side than on the downstream side. Thus the flood
> > continues (even after high water has passed) until the level is
equal
> > at the two ends of the channel, resulting in a slack. Then the
situation
> > [reverses].
> 
> I only see this in minor side-channels of the Columbia which are
separated
> from the main River by a very narrow opening.  The main stem
Columbia down
> here never functions like this -- and now (thanks to you) I understand
> why:  the mouth of the River is too large relative to the vertical
> excursion in tide (and consequent horizontal exchanges of water mass).

Excuse me, I need to get back to work. Isn't this more fun than
metallurgy?

Richard in Seattle


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