The second strategic factor is wind shifts. Shifting winds allow us to
reach the windward mark more quickly than we can in steady winds.
When the wind shifts, our close-hauled compass courses change. With each
shift one tack is lifted up above its earlier course, and the other tack in
headed below its previous course. When one tack is lifted the other is
headed, and vice versa. Our goal upwind is to sail each tack when it is
lifted. By sailing the lifted tack, we sail a more direct route to our
upwind destination (Fig. 5).
The fundamental upwind strategy is to sail toward the new wind or wind
shift. As we will see, this strategy keeps us on the lifted tack. The
application of this principle changes with different types of shifts; but
the fundamental rule-sail to the shift-never changes.
The best way to keep track of wind shifts is track your close-hauled
compass course. Before and during the race keep a record of compass
headings and establish a range of highs and lows for each tack. By
recording the shifts, you can look for patterns (see Figure 2) and
anticipate upcoming shifts.
Of course, reading the compass only tells about a shift after it has
arrived. In addition to the compass, observe the wind on the water and
watch its effect on other boats. Work to recognize and predict shifts
before they arrive.
Wind shifts are generally categorized in two types: oscillating and
persistent. Oscillating winds shift back and forth, like windshield wipers.
Persistent shifts swing gradually in one direction, like the hands of a
clock. A shift to the right is a clocking shift, or "veer;" a shift to the
left is called a "back" (Fig. 6a, b).
From experience we know the real world is more complex than simple
oscillating or persistent shifts. For starters we are going to look at
strategy in these two textbook types of shifts. After that we will look at
other variations.
We will look at wind shift strategy by first looking at the textbook
strategies for oscillating and persistent shifts.
The basic strategy in an oscillating breeze is to tack with the shifts.
As the wind shifts one tack is lifted so we can point closer to the mark
(or average wind) while the other tack is headed further away. When the
wind shifts again the advantage will be reversed; whenever one tack is
lifted the other is headed. By coming about when headed and sailing on the
lifted tack, we can take advantage of the windshifts to improve upwind
performance. We use the term staying in phase to describe the process of
tacking on the headers and sailing on the lifts.
Sometimes the wind shifts gradually back and forth. This is seen most
often when the winds are coming over open water. At other times the shifts
hit all at once. We see this when the shifts are coming off shore, or in
the northwest winds after a cold front.
On starboard tack a higher compass reading is a lift, a lower number is
a header. On port lower is a lift, higher is a header. It is most
important to recognize headers since they suggest it is time to tack. Use
the phrase Port, Higher, Header as an aid to remember the correlation
between compass readings and shifts.
By collecting wind information before the race and updating information
as the race progresses, we should know at any moment whether we are sailing
a lifted, headed, or average course. If conditions change, our lifted and
headed numbers will have to be adjusted.
Sailing in oscillations seems pretty straightforward. If the shifts come
in a regular cycle and no one gets in your way, it should be easy to stay
in phase. Somehow it doesn't always work that way. If you find yourself
out of phase, sail the tack which takes you closest to the mark, or towards
the next puff, while you sort things out.
Tacking as the wind crosses the average works great if the wind spends
equal time on each side of average and the mark is straight upwind. This is
not always the case. When the leg or shifts are not balanced, then the
crossover angle for tacking must be adjusted to match. For example, if the
leg is skewed to three times as much starboard as port, then we'll need to
sail on starboard for three quarters of the wind range, and port for one
quarter.
Similarly, if there are other strategic considerations, our tacking
angles may be skewed. For example, if there is better wind or current to
one side of the course, we would only sail away from that side at the
extreme end of the shift spectrum.
In preparation for our 12:15 start we periodically record and plot our
wind information. Using the close-hauled compass course on each tack, we
are able to calculate the wind direction. The Wind Graph from our Race
Planner shows the following (Fig. 7):
The wind speed is a steady 8 to 9 knots.


Fig. 7 - The Wind Graph above shows the plot
of an oscillating wind over time. Using this information, the tactician is
able to plan a strategy to take advantage of the shifts, shown by the
checkered boat, above. The black boat ignores the shifts, and falls
behind.
Stay in Phase-Tack on the Headers
Coming off the starting line, we are sailing on starboard with a compass
course of 180º to 185º. These are high numbers for starboard
tack, which means we are lifted. Gradually our course drops to between
175º and 180º. This is an average course, neither headed or
lifted, and we can sail on either tack.
Soon the crew reports that our course has dropped below 175º. Other
boats are showing similar angles. We are headed. We tack. As we settle on
port tack the compass reads 260º-265º, low numbers which mean we
are lifted on port tack. As the numbers rise, we are getting headed.
Remember: Port, Higher, Header. When our course falls below ouraverage, we tack again and sail lifted on starboard.
As the plot shows
, we continue tacking on the headers in the oscillating shifts. Gradually
we find ourselves to the left of the middle of the course. We use the time
when the wind is at the average direction to sail on port tack, which
returns us to the middle. We sail on starboard only when lifted above
180º; we sail on port for any heading between 260º and
270º.
A New High!
Further up the leg, we are sailing lifted on starboard. Compass readings
show a course between 180º and 185º. Gradually we are lifted to
190º. At this point lights should flash, bells should ring, and sirens
should sound. 190º is beyond our range of oscillations. We are lifted
higher than ever before.
We may have to reevaluate the conditions and modify our strategy. What
is causing this new reading? Helmsman error? Changing weather? Are we
closer to shore? Are there any new clouds? What is going on with the rest
of the fleet?
Is this a momentary aberration, after which we will return to earlier
conditions? Or is this the beginning of a persistent shift? Perhaps the
wind will continue to oscillate, but over a new range.
The key is to first recognize that something new is happening. The next
step is to evaluate the change and make plans accordingly. Ideally we would
have seen it coming-either from wind on the water, an expected shift near
shore, or by observing other boats (in an earlier class-we are leading our
fleet, remember).
The Impact of Shifts-Don't Miss 'Em
Meanwhile, one of our competitors has sailed off the line on starboard
tack and continued one third of the way up the leg before tacking. From
there he sailed across the course on port tack, to the starboard tack
layline. Ignoring the shifts has left our rival out of phase and sailing
headed half the time. On the other hand, he has only had to tack twice! On
a two mile beat with 10º oscillations, a boat which sails in phase
will be minutes ahead of a boat which ignores the shifts. That's even after
we throw in the cost of a couple of extra tacks!
A little later, we'll pull out our slide rules and find out just how big
a deal windshifts are, but for now, just remember: Track the shifts, and
hit 'em!
Similarly, if there are other strategic considerations, our tacking
angles may be skewed. For example, if there is better wind or current to
one side of the course, we would only sail away from that side at the
extreme end of the shift spectrum.
Persistent Shifts
The strategy in a persistent shift is to sail toward the new wind. If
the wind is shifting to the right, then go right. If the wind is shifting
left, go left.
Sail Headed
In a persistent shift, one tack is continuously getting headed while the
other is getting lifted. Our strategy is to first sail the tack which is
getting headed, then sail the tack which is getting lifted. Why? The tack
which is getting headed is getting worse all the time. It is headed now,
but will be headed more later. Sail it now before it gets worse. The tack
which is getting lifted is improving all the time. If we sail it now we
will be missing a better lift later.
Are you Sure it's a Persistent Shift?
How hard is it to split with the fleet and sail into a header? Without
our pre-race info, weather forecast, and/or observation of other boats on
which to build our strategy, it would be crazy. Even with good information
and a well thought out plan, it is hard to stick to your guns as the fleet
tacks away. If you know what is coming, then go to it. Position yourself to
the favored side of the fleet.
The Rewards
How much do you gain by sailing into a persistent shift? It depends how
far the wind shifts and how far you are separated from your competition;
but in a word - Plenty.
PERSISTENT EXAMPLE
We know from our Wind Graph that the wind is gradually backing. Our
starboard tack readings for the hour before the start show a trend:
30º > 25º > 20º > 15º. The port tack compass readings
are similar: 120º > 115º > 110º > 105º. Starboard is
getting progressively headed, while port is getting lifted. The forecast
tells of a low passing to the south. We expect the wind to continue to back
(Fig. 8).


Fig. 8 - Wind Graph and strategy for a Persistent
Shift.
Sail to the Shift
Coming off the starting line on starboard tack our compass reads
15º. A minute later it reads 10º, and a few minutes after that it
reads 5º. With each little header some of our competition tacks away.
Some tacked to port on the first header off the line. Others have gradually
bailed out as the header continues.
Eventually, with the compass reading 0º, we tack over. Our course
on port tack is 90º. We are short of the layline to the mark.
Gradually we are lifted, first to 85º, then 80º, and finally
75º. We are lifted to the mark, far ahead of those who tacked out
early.
When should We Tack?
The choice of where to tack is a little tricky. Theoretically we want to
tack so we will be lifted exactly to the mark. This curved lifted layline
would give us the full advantage of the shift without sailing any extra
distance. This is a tough call, to say the least. A more realistic approach
is to tack short of the layline. Then, as you approach the mark, tack out
again, and take another guess. Don't overstand or you'll be sailing extra
distance. As you get closer to the mark, you should be able to make an
accurate layline call.
Another (tactical) perspective on where to tack is to maintain position
between the fleet and the shift. Don't sail to the corner-just get a
controlling position.
So Much for the Competition
Coming off the starting line on starboard, we gradually got headed.
Some of the fleet played the header as an oscillating shift, and tacked
out. They expected to be headed again (on port tack) before tacking back to
starboard. This was a big mistake. We knew from our Wind Graph that we were
in a persistent shift. We used persistent shift strategy by sailing into
the header, towards the new wind.
The boats which tacked out early kept getting lifted further and further
on port tack, which made starboard tack look worse and worse. The port tack
boats ended up sailing what is known as the great circle route, getting
lifted around the outside of the mark.
Too Far Ahead
If the fleet goes right and you think the wind is going left, then
position yourself to the left of the fleet. Don't split completely with the
fleet, for two reasons:
First, if you split and you are right, you will end up way ahead, and
everyone will think you were just lucky. You don't want to win by too
much; just a comfortable margin that will let everyone see who is out
front.
Second, if you split with the fleet and happen to be wrong, you are
sunk. (Somehow it is not unlucky to be half a mile behind-you are just
bad.) Hedge your bets.
Other Types of Shifts
As we said above, pure oscillating and pure persistent wind shifts are
quite rare. There are infinite variations.
One variation is a mix of persistent and oscillating shifts. This mixed
condition is characterized by oscillating shifts gradually shifting one way
or the other-veering or backing-over
time.
Several other types of wind shifts occur. One is a major shift where a
new wind completely replaces the existing wind. This can happen suddenly,
or after a period of calm. Winds vary in other ways. There are geographic
shifts caused by the configuration of land and thermal wind shifts created
by the heating of land. There are also differences in the wind due to
differences in current (as we will see below), and there are shifts caused
by the movement of weather systems.
Mixed Conditions
Often conditions are not a pure form of persistent or oscillating
shifts. Instead we end up with a mixed condition, combining both
oscillations and persistent characteristics. The strategy in a mixed
breeze is to favor the side toward the persistent shift while playing the
oscillations.
Part of the trick in coping with these mixed conditions is to realize that
the range of oscillations is gradually changing. The high and low numbers
on each tack will be increasing or decreasing. What was once a header may
now be the median, with a new lower header on the way.
When conditions are too confusing to diagnose, the fall back strategy is
to sail to the mark. Which ever tack takes you closer to the mark is
preferred until there is reason to do otherwise.
Mixed Conditions Example
Here is an example of strategy in mixed conditions (Fig. 9).


Fig. 9 - Wind Graph and strategy for Mixed
Conditions.
Pre-Race Data
Our pre-race data is listed in the Wind Graph. It shows mixed
conditions. The trend is veering, but we have oscillations as well. Our
strategy will have to consider both; we will also have to keep a keen eye
out for changes in conditions. One thing to look for is stronger breeze to
one side. Is the trend shifting and building (as in this example) or
shifting and fading.
. . . And They're Off
It is interesting to see the different strategies which emerge from
these difficult conditions. Some of the fleet will treat the beat as
though they were sailing a persistent shift. Others will tack on the
headers. Some will try to balance the mix. And still others will be
confused and uncertain of how to handle the conditions.
As the fleet moves up the beat in mixed conditions, the apparent leaders
will change with each shift. Often it is unclear until the last shift of
the leg who will come out ahead.
Keep Fighting
In mixed conditions you are never out of it. Keep working, keep trying
to decipher the next shift. There are plenty of opportunities to catch up
(and more than enough chances to get confused). If you find yourself
baffled, try to re-group. Everyone will have their moments-if you can keep
from going to pieces during your bad moments, you'll have another chance
for good times.
Geographic Shifts
We do most of our racing near shore, where the interaction of the land
and water affects our sailing wind. Further offshore conditions are more
stable and predictable; but along the coast, wind conditions are difficult
to predict.
There are many ways the shoreline changes the wind. First, the
shoreline funnels the wind. The wind shifts to follow the shoreline.
Second, offshore winds tend to shift more perpendicular to the shoreline
(Fig. 10a). Third, winds shift around obstacles such as hills, buildings,
and thermal domes in areas with lots of pavement (Fig. 10b).

Fig. 10a - Offshore winds tend to shift more
perpendicular to the shoreline.

Fig. 10b - A city or hill can create oscillating
shifts, with bigger shift near shore.
Fourth, the heating of the land creates thermal winds-sea breezes-which
blow towards shore during the day.
Fifth, the thermals create turbulence and mixing which can pull the
upper winds down to the surface. These upper winds are generally shifted to
the right of the surface winds.
The effect of these geographic changes can be either persistent or
oscillating. In offshore winds, there will commonly be a mixed effect-with
puffs coming from shore lifting the tack which is parallel to shore, and
with those lifts being stronger the closer you get to shore.
The thermal effects on an onshore wind usually create a persistent shift
from the prevailing wind direction to the normal sea breeze direction (Fig
11).

Fig. 11 - As the land heats up, you get a
persistent shift as the prevailing wind shifts to the sea breeze
direction.
These shore effects are described in more detail in Chapter 13: Weather
later in this book.
Weather System Wind Shifts
A Major Change
As weather systems move or weaken, one wind can replace another. A
prevailing wind may be pushed aside by a thermal, or a new weather system
wind may arrive. Whatever the cause, there are occasions where a new and
different wind appears and all the earlier information becomes irrelevant.
If we can anticipate this change based on forecasts or observations (new
clouds etc.) and be in position for it, there can be tremendous gains. But
beware-There is a danger in chasing the predicted conditions and expecting
a shift which does not arrive as scheduled. Summer weather systems often
stall or even disappear as the get to the coast.
Squall Winds
Another type of weather system wind is a localized late afternoon
squall. These can turn the entire fleet on its head. These squalls create
two opportunities-one as the squall hits, and the other as the squall
passes.
Be prepared. If you are ready and can continue to race through the
squall while others scramble, huge gains are possible. Sail toward the new
shift to avoid windward work once it arrives, and be ready to shorten sail.
A squall drill should be part of your crew training.
If the squall is localized, then after the squall passes conditions
often return to the conditions which existed prior to the squall. If the
squall is part of an advancing cold front, then conditions behind the front
will be entirely different from earlier. By recognizing the type of squall
you may be able to anticipate conditions during and after its passage.
Wind Shear
Wind shear is a condition where there are layers of wind-one at
the surface, and the other aloft. Wind shear is uncommon. It occurs most
often over smooth cold water early on a spring day, or at night.
There is a boundary layer of cool air on the surface, and a different
wind aloft. Sail trimming with the wind 30º, 45º or even
180º different from the deck to masthead can be baffling, to say the
least.
Generally the upper wind will become dominant. Fundamental wind
strategy says sail toward the new wind-in this case sail toward the upper
wind, as it will eventually displace the surface wind. If you are a small
boat in a mixed fleet, don't forget to look at the mastheads of larger
boats. Sometimes you will be able to find a wind shear (and a clue to the
expected wind) which does not show at your masthead (Fig. 12).

Fig. 12 - Wind shear is the stacking of two
winds, one on top of the other. The upper wind usually displaces the lower
wind.
Don't confuse wind shear with wind gradient. Wind gradient is the
tendency for winds at the mast head to be stronger than those at deck
level. It exists almost all the time, and is more dramatic in light air,
less pronounced in heavy air.
The Impact of Windshifts
It is often difficult to predict the wind. Is it worth it to try to
figure out what the wind is going to do next? How much difference does it
make? Here's an example:
The Impact of Oscillations
We'll start first with a boat sailing upwind, with a tacking angle of
90°. Usingtrigonometry (yikes), we find that the distance sailed is 1.42
times the straight-line distance. To sail to a mark one mile upwind, the
boat will have to sail a total of .71 miles on port tack, and .71 miles on
starboard tack.
If the wind is oscillating as little as 5° either side of the median,
then performance improves significantly. To sail to a mark one mile upwind,
the boat will have to sail a total of .64 miles on port tack, and .64 miles
on starboard tack. By taking advantage of the shifts, the distance sailed
is reduced to 1.28 times the straight-line distance. To sail to a mark one
mile upwind, the boat will have to sail a total of .64 miles on port tack,
and .64 miles on starboard tack. A savings of .14 miles!
If the wind is oscillating 10° either side of the median, then
performance improves dramatically. To sail to a mark one mile upwind, the
boat will have to sail a total of .57 miles on port tack, and .57 miles on
starboard tack. By taking advantage of the shifts, the distance sailed is
reduced to 1.14 times the straight line distance. A savings of .28
miles!
At a boat speed of 6 knots this represents over 2-1/2 minutes in one
mile! That's right - 150 seconds per mile! These numbers are for a boat
sailing the wind shifts perfectly. If your windshift efficiency is only 40%
of optimum, you'll still save one minute per mile! (Fig. 13)

Fig. 13 - The impact of oscillations can be
significant.
7.5 Current
Current adds complexity to strategic planning. The obvious, and
primary, strategic concern is to seek out better (more favorable or less
adverse) current. When the current is not uniform across the course, it can
be an overriding strategic factor. Currents run stronger in deep water than
in shallow, and faster in narrows than in open water. Below points and
around bends, eddies can develop. Adding further complexity is the fact
that currents change. Correct strategy can change dramatically over a
period of hours. Storms and strong winds can distort surface currents and
delay tides, sometimes making tide tables useless (Fig 14).

Fig 14 - Currents are created by tides and rivers.
They run stronger in channels than in shallows, and can be a major
strategic factor.
Wind Driven Current
Currents are not limited to rivers and tidal basins. In the Great Lakes,
for example, currents of one full knot are possible. Currents build when
strong winds drive the surface water. After the winds abate, the currents
reverse as the water, which has been stacked up at one end of the lake,
returns to level (Fig. 15).

Fig. 15 - Wind can create current. Wind driven
current can exaggerate or reverse tidal currents in shallow bays. And it
can create currents where there otherwise would be none.
After the wind has pushed water to one end of a basin, the current will
reverse when the wind subsides.
Uniform Across the Course
When the current is uniform throughout the course, it affects the
laylines and sailing angles to the mark. If it is running across the
course, then it can also change the balance of time spent on each tack (See
Fig. 16).

Fig. 16 - When the current is uniform throughout the leg,
the biggest impact is on laylines into the mark. Current can also skew the
course, changing the balance of time on each tack.
When Current is Not Uniform
When the current is not the same across the course area, then we must
seek out the advantage. Differences across the course can shape our
strategy. Unless there are dramatic differences in wind conditions a
current advantage is key to strategic planning.
Current to one side
Obviously if the current is stronger to one side seek out that side if
it is favorable, and avoid that side if it is adverse. A favorable current,
running against the wind, can set up a pronounced chop. Look for this. Sail
into the choppy water and ride the current upwind. Similarly, smooth water
can indicate wind and current running together. Avoid this area upwind
(Fig. 17).

Fig. 17 - When there is stronger current to one side, go
to it if favorable, sail away if adverse. The advantage can change with the
tides.
Current across the course
When the current runs across the course and is stronger in one part of
the leg, you want to take advantage of the change in sailing wind caused by
the current. Sailing bow into the current you will be lifted; sailing with
the current astern you will be headed. For example, in ten knots of wind
and one knot of current the sailing wind is shifted 6º. With one tack
lifted and the other headed, the effect is a 20% advantage in VMG (Fig.
18).

Fig. 18 - When current is not uniform, take advantage of
the shift in sailing wind. In this example we have 10 knots of wind, 1 knot
of current, and boats tacking through 90°. The current gives one boat a 6°
lift, the other a 6° header. The lifted boat's VMG is 20% better than the
headed boat's. (VMG is normally .71 of boat speed. The shift is 6° because
arc-tan 6°=1/10.
A 6° lift creates a VMG of .78, a 6° header creates a VMG of .63.
.63/.78=.80. I'm glad you asked.)
Predictable, to a Point
Current, whether tidal or river generated, is predictable. Tide tables
and current charts should be studied, and their predictions compared with
observation. When the current runs strong it is often more reliable and
predictable than the wind; a small current advantage translates into big
gains.
In tidal areas the advantage can be fleeting-or reverse-over the course
of a race. Obviously we need to pay attention to changes in the tide.
Changes with Wind Conditions
The wind can upset current predictions, particularly in shallow water.
A strong wind blowing over a long period can overwhelm tidal effects,
pushing surface water and delaying or reversing tides. When the winds
abate, the current distortions will remain until the water has had a chance
to return to level by flowing in the direction opposite the earlier wind.
Winds can also create currents where there otherwise are none, as mentioned
above.
Effects on Sailing Wind
Current changes the sailing wind for a boat. The sailing wind is the sum
of the true wind over the bottom and the current. The net effect of current
on the wind reinforces the effect or the current. A favorable current
creates a favorable change in the sailing wind, and an adverse current
makes for an unfavorable change in the sailing wind (Fig. 19). Details are
explained in Chapter 13: Weather near the end of this book.

Fig. 19 - The vector of the current is added
to the true wind to create our sailing wind.
Develop Local Knowledge
One key to success in current is to develop local knowledge. Keep
records of how the current runs in various wind and tide combinations. Our
strategic plan is only as good as the information it is based on. Accurate
current information is critical to good strategic planning.
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