May, 2016 Dispatch: On
Tides and Med Mooring
Tides: What you must know and more than you want to
know.
What you must know:
Recently on a combined
Combo(103/104) and 106 (Offshore cruising) course we had the occasion to
experience the bad and the good of tides.
The major novel requirement of the
ASA 106 is that you must do a night-time entrance into Galveston Entrance. This of course meant that we would have to go
far enough offshore and stay out long enough to arrive at the Channel entrance
after sundown. It just so happened that
this coincided with a 3 knot ebb tide!
Now, obviously, a sailboat which is capable of at most 6 kts isn’t going
to make much “speed over the ground” going against a 3 kt. Ebb tide. As expected, it took over 5 hours to cover
the distance which would normally take an hour and a half. This is when one’s patience is worn very
thin, especially in the Galveston entrance because of the extreme challenge of
picking out the channel markers against the constellation of background lights
from the city and the ships in the anchorage.
We had plotted our course beforehand, as recommended, so that we knew
what should be the course from one marker to the next, but even then it was a
challenge which required the attention and participation of every crew-member.
Now, it should be remembered that
the major causes for making a mistake while sailing are: 1. Sleep deprivation, 2. Pain and 3.
Hypothermia. We did not have the risk of
the last two, but there was certainly a risk of the first, so, about 11 pm, I
sent two of the crew-members down below to take a nap while the helmsman and I
continued to pursue the channel markers which appeared to be receding even as
we could see the water slide under our hull.
Our speed over the ground was a whopping 2 kts! One must not lose patience and give up unless
you are going backwards!
Finally, we got into the slip after
1 a.m. Everyone felt that they had
accomplished something.
What you must know about tides:
The depth at low tide (designated
“mllw” = mean lower low water on the chart)
The draft of your vessel
Time of high tide
Time of low tide
The site where this information
applies is relevant. For example, when
you listen to NOAA (or VHF 1) or look in the newspaper you will get a
particular time for, say, “high tide is 8 a.m.”
That particular time applies to GALVESTON ENTRANCE. You must extrapolate the difference in
distance (26 miles up the HSC) to determine the high/low tide at Clear Lake
Channel. You can find this extrapolation
in a book (Coastal Pilot) you can purchase from the Coast Guard or download it,
or you can find it in the little books which can be purchased at bait shops or
West Marine.
For Galveston Entrance to Clear Lake
Channel it is.....drum roll....6 hours! So,
if high tide is 8 a.m. at Galveston Entrance it would be 2 p.m. at Clear Lake
Entrance. This comes as a surprise to
most people. But considering this
difference gives some clue to what a tide actually is.
How We Know
Isaac Newton and the
mechanical world view.
Everyone knows the
story about Isaac Newton and the apple falling off a tree. Apparently, the story is true, and it is even
more fascinating than you might imagine.
In 1665, Isaac Newton was a student at Cambridge University. Because of the plague, the University was
closed, so Newton took himself to his aunt’s farm for two years. Since he went without his books he had a lot
of time to think. During 1665 and 1666
he discovered the law of universal gravitation, the laws of optics and invented
the calculus. But he did not publish any
of it. Twelve years later, back in
London, Edmund Halley (of the comet fame) and Christopher Wren (the architect
of Westminster Cathedral were in a coffee shop discussing the tides and the path
of the moon around the earth. Halley bet
Wren that the brilliant mathematician out at Cambridge would know the answers
to their questions, so he went and asked
Newton. Sure enough, Newton knew the
answers to Halley’s questions, but he had never published it and couldn’t find
his notes. (If Newton were alive today
he would be on meds! - and I don’t necessarily mean that as a criticism of
Newton) So he had to start all over
again. This time, because of the threat of
competitors (Wilhelm Leibniz, a German living in Paris, in particular) to be
certain that he got the credit he thought he deserved, he created his entire
mechanical world view of the attraction between two bodies (we know them as
“Newton’s First Law, Newton’s Second Law, Newton’s Third Law), which he
published in his Principia Mathematica...This book was the basis for all
of physics until Einstein’s General Theory of Relativity in 1915. The work is considered by most historians to
be the greatest scientific treatise ever produced by man. As Alexander Pope wrote:
“Nature and nature’s
laws were night. God said, ‘Let Newton
be,’ and all was light.”
So, turning to some oceanographic
facts to explain tides:
The Oceanography of Tides
What we know as high
and low tide is that it is actually a single wave that sweeps around the Earth
as it spins. Actually, rather than
thinking of the tides as being a wave it is more accurate to think that the
water on the surface of the earth is attracted to the Moon as it passes over
and the Earth spins UNDERNEATH the water.
Think of spinning a bucket of water - the bucket spins under the water
which builds up on the sides. This
creates the phenomenon of two daily tides:
Again
to be even more accurate, the tides are caused by the complicated combined
effects of the attractions of the Earth, the Moon and the Sun as a body. When the Earth is closest to the Moon the
water on that side of the Earth bulges towards the Moon. There is a simultaneous bulge of water on the
opposite side of the Earth. I have read
of two different theories for this phenomenon, which produces two (diurnal)
tides a day. One explanation is that the
far-side bulge is caused by the centrifugal force of the spinning ocean. Another explanation seems to me to be more
plausible: The ocean on the side of the
Moon is closer to the Moon than the Earth, so it bulges towards it. The Earth’s center of gravity is more massive
and closer to the Moon than the ocean on the far side of the Earth, so it is
pulled away from the water on that side, producing the bulge.
What
this variability in the explanation of the tides indicates an interesting
fact: The force of gravity is still
largely a mystery to physics, and currently there are competing theories.
Why the tide is so
much later at Clear Lake Entrance: Add
to this already complicated picture, interference of continents, inlets, bays,
the spin and tilt of the Earth and you get some sense of the difficulty of
predicting the tide times. The tidal
wave that comes into the Clear Lake Entrance is coming from the Atlantic,
across the Gulf of Mexico, up through the Galveston Bay Entrance, then it has
to slosh around the coastline of the Bay until it sweeps into Kemah.
I mentioned in an
earlier dispatch of the extreme tidal range at that time in Galveston Bay,
making it such that I was unable to get my boat out - that was a “spring” tide,
when the Earth, Moon and Sun are lined up, which together with a north wind
sucked the water out of the Bay.
So, what is the
wavelength of the ocean tide? 20,000
kilometers!
As I stated, Newton’s
theory of the tides is based on the theory of universal gravity which was
ridiculed by Einstein as (“action at a distance”). This theory holds that two bodies are
attracted to each other in a manner which is directly proportional to their
mass and indirectly proportion to the square of the distance between them. Newton never presented a hypothesis to
explain gravitational attraction. He
said, “I offer no hypotheses.” (He
actually wrote it in Latin, but Ill spare you).
Even today, physics does not have an explanation for universal
gravitation and the theory is not part of what is called the Standard Model of
Particle Physics (which includes three forces - the Electromagnetic Force, the
Weak Force (together, the “Electroweak Force), and the Strong Force). Today physicists are attempting to subsume
the Standard Model of particle physics and the theory of gravity under what is
called “String Theory.” I am told that
it would take about 6 years of constant study to master the mathematics to
become a String Theorist. This is about
how long it would take to make two leisurely circumnavigations of the
Earth. So, I had better get started on
it. (The circumnavigation, I mean)
Back to Houston Ship Channel
After, a rest of several hours we
then proceeded up Houston Ship Channel towards Kemah. As expected, we now rode a flood tide, so our
speed over ground was 8 kt! those(The Lord
taketh away, and (for those who are patient) the Lord giveth.
So, on the entrance, we were trying
to climb up a wave,
While,
On the passage from Galveston to
Kemah up the HSC, we were riding down a wave.
You know, it is said, “location, location, location.” Well, I must add: time, time time.
A lot more is known
about gravity than in Newton’s day. It
is known, for example, that gravitation is responsible for the rings of Saturn
and for the volcanic eruptions on a moon (Io) of Jupiter!
Think about it: While we were interacting with the ocean’s
wave we were interacting with the same force that affects Saturn and
Jupiter! I don’t know if I should feel
humbled or defiant (like Lieutenant Dan in Forest Gump - “Is this all
you got!?”)
I suppose that this is
the meaning of the sentence:
“May the Force Be With
you.”
References:
1. Cartwright, David Edgar. Tides: A Scientific History. Cambridge: CUP, 2000.
2. Pugh, David. Changing Sea Levels:
Effects of Tides, Weather and Climate.
New York: CUP, 2004.
3. Burton David M. History of Mathematics: An Introduction. Dubuque.
IA: Wm. C. Brown.
Anchoring and Med Mooring
In our Combo course (103/104) we don’t
typically teach Mediterranean Mooring. I
have discussed it previously and commented that it is used all over the Med
(and elsewhere) because it allows a marina to stack in more boats. I realize that that statement is a bit
biased, so here is another explanation: It encourages you to get to know your
neighbor better.
The important physical difference is
that there is no walkway or dock between the boats. So, many many fenders are required.
The other features of Med mooring
which are different is that you lay an anchor out in the water, or pick up a
line (“lazy line”) and attach it to your bow, then back onto the dock.
So, learning how your boat backs is
critical.
I recently came up with a method of
teaching Med mooring by incorporating it with teaching standard anchoring:
Consider the procedures consist of
three stages:
1. Prepare the anchor and lines.
2. Drop the anchor.
3. Secure the anchor.
Stage 1: So, with regular anchoring: The lookout and anchor -crew stands up on the
bow and directs the helmsman to a good anchoring site, based on the look of the
water (in the Bahamas, for example, through the coral).
The boat is motoring INTO the
wind.
This is Stage 1. The anchor and rode are prepared so that they
can be dropped when required. This stage
should be practiced even before the procedure is begun, and can even be
practiced while in the slip.
The anchor rode is taken from the
anchor locker and “faked” so that it will play out smoothly when the anchor is
deployed. The anchor may be hung over the
bow and held firmly in place.
Stage 2: The bow-crew directs the
helmsman with appropriate pre-agreed hand signals to stop (usually a closed
fist). The boat is allowed to stop and
begin to drift backwards with the wind.
Then the anchor is dropped.
The boats is allowed to drift
backwards until about 1/2 of the previously calculated amount of rode plays
out, then:
Stage 3: The anchor is secured. Then the helmsman is directed by appropriate
hand gestures to motor back at about 1500 rpm to set the anchor. If the anchor is set then the remainder of
the rode is played out. It not, then
there should be consideration of another site with perhaps better holding
ground.
Now, of course, you set an anchor
watch.
Med Mooring
Now, if you have learned this procedure
with standard anchoring off the bow, then Med mooring is straight-forward:
Stage 1: Before entering the slip one should approach
the slot in forward and look for a “lazy line,”
a line which is attached to a cleat on the dock. If one is spied, you will not need to drop a
bow anchor but will pick it up instead.
Prepare the anchor and the
lines. The anchor is prepared as in
standard anchoring. Additionally, the
lines which will be thrown onto the dock are prepared and attached to the stern
cleats.
If there is a lazy line, the anchor
does not have to be prepared.
Multiple fenders are hung from the
sides.
Then the helmsman proceeds to slowly
back towards the selected spot between two boats.
Stage 2: This is the same as in standard anchoring, except
that the helmsman indicates when to drop the anchor (usually when the boat is
about 3 boat-lengths from the dock).
He indicates this by merely holding
up two fingers.
The bow-crew drops the anchor and
the helmsman continues backing toward the dock.
Again: if there is a lazy line, the anchor is not
dropped.
Stage 3: Then, when the boat just begins to enter the
space between the two boats the helmsman holds up three fingers, indicating
that the bow-crew should secure the anchor.
The helmsman continues backing into the space. (The anchor should now be secure and becoming
taut).
When the boat approaches the dock,
the helmsman (or a crewman) throws the lines which have been secured to the
stern cleats to someone on the dock where they are secured, or, if there is no one
on the dock, the helmsman approaches the dock close enough for a crewmember to
jump in the dock (using the usual precautions to not jump until the boat is
virtually touching the dock
If there is a lazy line, it is now
picked up and walked to the bow, fed through a bow pad eye then secured to a
cleat.
The boat should now be anchored at the bow or secured by a lazy line and
secured to the dock at the stern.
There are several good Youtube
videos of Med mooring. The one I like the
best is titled: Stern-to mooring
techniques Greece
If your boat does not back down with
a degree of control, or if there is a really strong cross wind, a different
approach can be tried. Head the boat
into the wind and at the proper drop point let go the anchor and allow the boat
to settle back, gently snubbing the rode to set the anchor. Let out slightly less rode than the distance
from the anchor to the bows of the other boats.
Take a line ashore in the dinghy and manually sweat the the stern into
position at the entrance to the slot, from where it can be further worked into
the slot.
Some precautions: Position your boat fore and aft so that your
spreaders do not tangle with those of your neighbors.
I haven’t mentioned why it is better
to back in rather than motor in forward -- it is easier to get off the boat at
the transom than clamber the bow. Duh!
mWC
April,
2016 Dispatch: On the BVI, the Caribbean
Sea, water pump belts and fuel filters
On
the BVI
I recently spent some time cruising
in the BVI. It has been over 10 years
since I was last there and there were some changes. The BVI is still the most popular spot to
charter a boat and the number of vessels in the water has grown considerably,
but it is still a great place to cruise – particularly for a first-time
charterer. The Moorings and Sunsail
bases are on the south side of Tortola, in Roadtown, which is sheltered. One does not have to worry about leaving and
returning to the marina because a pilot will take you out and, on return, will
come out and board you and take you in to base. The majority of vessels in the waters now
are catamarans. One doesn’t have to
worry about not having catamaran certification because the managers will check
you out and instruct you on the boat before you leave.
Most of the good anchorages where
the snorkeling is the best now have
mooring balls which can be picked up for the duration of the dive. Most do not allow overnight mooring or
anchoring, so you will need to leave your anchorage early in the morning to get
a good mooring for the duration of your snorkeling.
In
the Caribbean Sea
On this same trip we sailed south of
the BVI out into the Caribbean Sea to the east of the Leeward Islands. This is a good area to get some ocean sailing
experience with the swells one would expect to encounter in deeper waters.
We sailed east of Saba island. One must be careful to keep considerable sea
room from Saba island because the “Saba Bank” extends out several miles and has
depths as shallow as 6 ft. in spots.
Keeping a careful DR is important
because there is also a small island (Aves) right out in the middle of nowhere.
Of
water pump belts
Recently while sailing my boat in
Galveston Bay I had an experience which teaches some principles to be known
regarding the (over) heating of the engine.
When I first started my engine there was a screaming sound coming from
my water-pump belt. I had heard this
before and had checked and found that the belt was tight enough, so I just
dripped on some lubricating oil or WD 40 on the belt and the squealing stopped. This time, however, when the sound started, I
could not go down and drip on oil. Soon
the squealing stopped. Then my
overheating alarm came on. When this
occurs, the first thing to do is check to see if water is coming out of the
exhaust which would indicate that the sea-water cooling system is working. I checked and it was coming out.
I
stopped my engine – this is obviously important, because if you don’t you will
permanently damage the engine.
Now,
remember that a marine diesel engine has two cooling systems – the sea-water
system: consisting of an inlet hose (with stopcock), a water filter, and a pump
(with impeller). Malfunction of any one
of these would result in water not coming out of the exhaust.
As
I said, this was not the problem in my case.
So,
now, I turned to consider the fresh water system:
This system is internally circulated
(and cooled by the sea-water through a heat exchanger)
It does not start circulating until
the water temperature rises to 42 degrees (in the case of my 30 hp Yanmar).
For it to begin circulating a
thermostat must open.
So,
I assumed that the problem was that the thermostat was malfunctioning. Now, one can remove the thermostat (after the
engine has cooled – be careful!) and the water will circulate. This could be a temporary fix.
The
fact that this overheating alarm occurred about 15 minutes after starting the
engine made me suspicious that the problem was the thermostat.
Of
course, the problem could have been caused by there being too little water (or
antifreeze) in the internal system, so, after letting the engine cool, I
checked the water level and it was okay.
So,
I set about to remove the thermostat – then I noticed – the water pump belt was
missing! It had broken and fallen down
in the pan under the engine. So this was
the obvious problem. Luckily I had a
spare on board and, after installing the new one, the engine ran coolly into the
marina.
Now,
the question should arise: How come
there was sea-water coming from the sea-water system if the water pump belt was
broken?
There are two possible answers:
1. The two
systems run on separate belts. This is
true for some engines.
2. The
sea-water system runs without requiring a belt drive. And this, surprisingly, turned out to be the
answer in the case of my Yanmar 30. I
had to go to the engine booklet to see how it works. The explanation is vague – but it clearly is
separate from the fresh water system.
The moral of this tale:
1.
If your engine is heating but your sea-water is circulating, look at your fresh
water system.
2. Do the diagnostics
before you set about doing the treatment.
On
fuel filters
On a recent course we had an
experience which taught a lot of lessons.
When we left Kemah, the wind and waves were very heavy and tossed us
around dramatically as we motored across the Bay towards the Boater’s Cut at
HSC marker. After turning into the HSC
the wind and waves tossed us around even more and the engine throttled down
significantly. After passing through the
narrow part of the channe at Red Fish Island, l we deployed the jib, to be ready should the engine fail
completely. Sure enough, this is what
happened at about marker ‘45’. One
should be able to speculate what was the problem with the engine.
Answer:
The engine was acting as if it was “fuel
starved,” meaning that the jostling waves had kicked up the grundge which grows
in the bottom of diesel. I am told that
there is actually a bacteria which will grow in diesel!. It was obvious at this time that we should
have tended to the engine before turning into the HSC, but now we were
committed. The wind direction would not
allow us to turn back. I elected to not
deploy the main sail because of the risk
of considerable leeway movement towards the spoil banks. So the students had to quickly learn how to
handle a sail boat with extreme lee helm (just the jib was out) while another
crewman and I went below to attend to the engine. Luckily, the student who went down with me
was a mechanic by trade, so he was able to quickly identify and change the fuel
filter. Equally luckily, the other
students, despite having virtually no experience sailing a large vessel,
quickly picked up the skill and cooperatively taught each other how to handle
the bucking vessel. Leadership and
teamwork solved the day.
Just
as expected, the fuel filter was completely blocked with green slimy
grundge. We had an extra filter and once
it was installed and the fuel line bled of air (by opening a bleed hole and
touching the starter a few times) the engine kicked right in and we were able
to motor on to Galveston. If the engine
had not participated in the adventure we would have had to hoist the main and
tack across the HSC (at an appropriate open spot) and anchor in East Bay, south
of Bolivar peninsula, to ultimately be towed
home.
I
learned from the mechanic that some modern engines have an electric fuel pump
so you don’t have to hit the starter to get the fuel to start through the
system. You can tell this if you hear a
“clicking” when you turn on the ignition.
For us, the wind was so loud we could not hear anything, so we hit the
starter.
The
major lesson repeated: attend to a
malfunctioning system before you have to have it. Hoping that it will work when you need it is
a natural human trait, but one not designed to achieve success unless you want
to use up all your luck for a long time.
And you may need that luck for some time when mother nature is not so
kind and forgiving.
mWC
January, 2016 Dispatch
Emergency Calls
There
is some confusion on which emergency calls should be used in certain
situations. The three calls are:
‘Mayday
Mayday Mayday
‘Pan
Pan Pan’
‘Securite
Securite Securite (pronounced
“See-cur-a-tay”)
Mayday
There
is not much confusion about this call.
It is to be used if there is imminent loss of life or the vessel- man
overboard, sinking vessel, in danger of going on the rocks, etc.
But,
with the other two there is some confusion.
Some books write that they have different priorities, but this is not
entirely correct. They actually mean different things to the ones
receiving the call.
‘Securite
– means ‘I am a hazard to navigation,’ so the receiver should be aware of the
situation because the one sending the call may be a hazard to him.
‘Pan…’
means ‘I need attention, or help…” It does not mean that the receiver has to
necessarily look out to be certain that he doesn’t run into the sender.
Consider
these three scenarios and decide what is
the appropriate call:
A.
You lose power while motoring past Kemah Boardwalk, so you drop anchor.
B. You lose power and
start taking on water while motoring out Bolivar Roads, and are not able to get
out of the channel.
C. You lose power
while motoring out Bolivar Roads, but manage to drop an anchor out of the
channel.
___________________________________________________
Scenario A: The appropriate call would be ‘Securite…’ –
you are a hazard to navigation.
Scenario B: The
appropriate call here would be ‘Mayday…’ You are in danger of sinking the boat
(lets suppose that it is a sailboat with a 50’ mast) in one of the busiest
channels in the world. You are more than
just a hazard to navigation.
Scenario C: The
appropriate call would be ‘Pan….’ You are not a hazard to navigation.
But if for example,
the wind picks up and you drift into the channel, then it would become a
‘Securite…’ Or if the winds appeared to
be driving you into the rocks, then it would become a ‘Mayday…’
This last example
shows that these calls should be considered to be dynamic – subject to change
if the circumstances change.
Taking a Different
Tack
One student (whose
first language was not English) once asked me, in reference to some nautical
term, “What is the logic?” The answer
is: There is no “logic.” Nautical terms
come from multiple languages – Dutch, French, German – much like English itself. They were picked up and became common merely
by usage. After the Battle of Trafalgar
(when the little island off the coast of Europe became an “empire,” then the
term used by the British became the language of sailing.
One term which often
leads some confusion is the term ‘tack.’
It is used in three different senses:
To be on a “starboard
tack”
To “carry out a tack”
(from, say, starboard to port)
The front lower corner
of the mainsail.
However, is you look
at the evolution of rigging you will realize that they come from the same
sailing maneuver. Before the development
of an fore-and-aft sail (Gaff, Marconi), the ‘tack’ of the main sail was rigged
forward of the mast. If you were on a
starboard tack, then it was on the starboard side of the mast. If you decided to tack the boat you had to
physically move the tack to the port side of the boat. So, to go from one tack to another you move
the tack of the sail from one side of the mast to the other.
Hope all are having a
good New Year.
mWC