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21
Abstract— Survey standardization
procedures can reduce the variability in trawl catch eff iciency thus
producing more precise estimates
of biomass. One such procedure,
towing with equal amounts of trawl
warp on both sides of the net, was
experimentally investigated for its
importance in determining optimal
trawl geometry and for evaluating the
effectiveness of the recent National
Oceanic and Atmospheric Administration (NOAA) national protocol on
accurate measurement of trawl warps.
This recent standard for measuring
warp length requires that the difference between warp lengths can be no
more than 4% of the distance between
the otter doors measured along the
bridles and footrope. Trawl performance data from repetitive towing
with warp differentials of 0, 3, 5, 7,
9, 11, and 20 m were analyzed for
their effect on three determinants
of f latfish catch efficiency: footrope
distance off-bottom, bridle length in
contact with the bottom, and area
swept by the net. Our results indicated that the distortion of the trawl
caused by asymmetry in trawl warp
length could have a negative inf luence on f latfish catch efficiency. At a
difference of 7 m in warp length, the
NOAA 4% threshold value for the 83112 Eastern survey trawl used in our
study, we found no effect on the acoustic-based measures of door spread,
wing spread, and headrope height offbottom. However, the sensitivity of the
trawl to 7 m of warp offset could be
seen as footrope distances off-bottom
increased slightly (particularly in the
center region of the net where flatfish
escapement is highest), and as the
width of the bridle path responsible
for flatfish herding, together with the
effective net width, was reduced. For
this survey trawl, a NOAA threshold
value of 4% should be considered a
maximum. A more conservative value
(less than 4%) would likely reduce
potential bias in estimates of relative
abundance caused by large differences
in warp length approaching 7 m.
Manuscriptsubmitted20October2004
totheScientificEditor’sOffice.
Manuscriptapprovedforpublication
6June2005bytheScientificEditor.
Fish.Bull.104:21–34(2006).
Variationintrawlgeometrydueto
unequalwarplength
KennethL.Weinberg
DavidA.Somerton
NationalMarineFisheriesService
AlaskaFisheriesScienceCenter
7600SandPointWayN.E.
Seattle,Washington98115-0070
E-mailaddress(forK.L.Weinberg):
[email protected]
Standardization of trawl survey procedures can reduce the variability in
abundance indices between samples,
survey vessels, and over time by reducing the variability in trawl catch efficiency. Such standardization was the
focus of the recently developed U.S.
National Oceanic and Atmospheric
Administration (NOAA) protocols for
the operation of its groundfish bottom
trawl surveys (Stauffer, 2004). The
first of these protocols concerns the
measurement of towing cables or
warps. For vessels towing with two
warps, the NOA A protocols specify
that the difference in length between
port and starboard warps may not
exceed 4% of the wire length between
otter doors measured along the bridles
and footrope. The need for adopting
such a critical value was considered
essential because of the belief that
unequal warp lengths—from inaccurate measurement or subsequent
stretching—would lead to distortion of
trawl geometry and a change in catch
efficiency, particularly for operations
that use trawl winches with the brakes
set or locked. The adopted value, however, was chosen somewhat arbitrarily
because experimental data showing the
dependency of trawl geometry or fishing performance on warp symmetry
was lacking for any of the bottom trawl
surveys subject to the protocols.
In this study, we examine the effect of unequal warp lengths on the
geometry of the 83-112 Eastern trawl
which is used by the Alaska Fisheries Science Center (AFSC) to conduct
the annual eastern Bering Sea shelf
survey. Although we monitor a full
suite of trawl dimensions, such as
door spread, wing spread, and headrope height that are typically measured on trawl surveys, our attention
wasprimarilyfocusedonthedistance
between the footrope and lower bridles with the sea floor. Prior studies
with this trawl have demonstrated
that escapement under the footrope
(Somerton and Otto, 1999; Munro
and Somerton, 2002 ; Weinberg et
al., 2004) and herding by the bridles
(Somerton and Munro, 2001) are the
most important determinants of catch
eff iciency for f latf ishes and other
benthic species. Although we understand that catch efficiency depends
on animal behavior as well as trawl
geometry, a goal of our study was to
assess whether the 4% critical value
is appropriate to prevent an appreciable degradation of catch efficiency
due to warp asymmetry, the result of
unequal trawl warp lengths.
Materials and methods
Experimental design
The experiment was conducted during
14−17 September 2003 along the Alaska
Peninsula in Bristol Bay approximately
85 km NE of Amak Island (55°58ʹN,
162°55ʹW) on smooth, relatively level
bottom at a depth of 82 m. Trawling
was performed with the chartered
38-m stern trawler FV Vesteraalen.
The Vesteraalen is powered by a single
1725-hp engine and is equipped with
split Rapp Hydema (Rapp Hydema AS,
Bodø, Norway) trawl winches carrying
2.5 cm (1ʺ) diameter, compacted, solidcore trawl warp.
22
Fishery Bulletin 104(1)
door legs
+ extension
15.2 m
bridle
55.0 m
10 m
61.9 m
17.1 m
footrope center
footrope corner
footrope wing
50 m
bridle
40 m
bridle
25 m
bridle
otter door
Figure 1
Schematic diagram of the 83-112 Eastern survey trawl and rigging shown
from the side (upper panel) and from above (lower panel). The experimentally
determined mean door spread and wing spread dimensions shown apply when
towing at a depth of 82 m with 274 m of trawl warp on each side. Bottom
contact sensor units, shown as oversized triangles along the bridles and
footrope, are labeled by position as discussed in the text.
The 83-112 Eastern is a low-rise, 2-seam, f latfish
trawl designed for use on smooth, soft bottom. The
nylon net is constructed of 10.1-cm stretch mesh in
the w ing and body, 8.9 cm in the inter mediate,
and double 8.9-cm mesh lined with a 3.1-cm mesh
in the codend. It is towed behind a pair of 1.8 × 2.7
m steel “ V” doors, weighing approximately 816 kg
apiece, which are attached to the net by two 3-mlong door legs (consisting of 1.6-cm long-link chain);
a 12.2-m-long door leg extension (consisting of 1.9-cm
diameter stranded wire); and a pair of 55-m-long,
bridles (consisting of 1.6-cm diameter bare stranded
wire) on each side of the net (Fig. 1). The 25.5-m-long
(83 ft) headrope has 41 evenly spaced, 20.3-cm diameter
floats that provide 116.4 kg of total lift. The 34.1-m-long
(112 ft), 5.2-cm diameter footrope is constructed of 1.6-cm
diameter stranded-wire rope protected by a single wrap
of both 1.3-cm diameter polypropylene line and split
rubber hose. The footrope is weighted with 51.8 m of
chain (0.8-cm proof-coil) attached at every tenth link,
forming 168 loops to which the netting is hung. An additional 0.6-m-long, 1.3-cm long-link chain extension
connects each lower bridle to the trawl wing tips to
help keep the footrope close to the bottom. Because the
wire length between otter doors measured along the
bridles and footrope is 175.6 m, the critical value for
differential warp length for this trawl established by
the NOAA 4% rule is 7 m.
Prior to the experiment, the warp length to be used
was measured to the nearest 0.1 m with a calibrated,
in-line wire counter (Olympic 750-N, Vashon, WA). A
zero reference point was painted on each trawl warp,
as determined by first setting the wire counter to zero
with the trawl door just beneath the water surface and
then measuring out 274 m (150 fm), the survey standard warp length for a fishing depth of 82 m. To verify
this benchmark measurement, the process was repeated
and all replicate measurements were found to be within
0.3 m, which is less than the 1 m specified by the NOAA trawl survey protocols for replicate measurements.
Subsequent reference marks, measured by tape, were
then placed along each warp at 3, 5, 7, 9, 11, and 20 m
from the zero mark.
The experiment consisted of examining the effect of
seven differences in warp length, henceforth referred to
as “offsets,” where one warp was positioned at values
of 0, 3, 5, 7, 9, 11, or 20 m longer. An experimental set
consisted of all seven offsets, chosen in random order. A
treatment consisted of towing the trawl, with the winch
brakes locked, at the specified offset for 5 minutes at
3 knots while maintaining a constant vessel heading.
Treatments were preceded by a 2-min equalization period at the specified offset. A haul consisted of two
treatment sets: one with a port offset and the other
with a starboard offset—the order having been chosen
randomly for each haul. To minimize the effect of bottom currents on trawl symmetry, hauls were made in
pairs along the axis of the dominant current direction,
either with or against the current—again, the order
having been chosen randomly. This direction was determined by deploying a current meter (Nobska MAVS-3,
Woods Hole, MA) 3 m above the bottom for one day
23
Weinberg and Somerton: Variation in trawl geometry due to unequal warp length
prior to the start of the experiment. Hauls were
made with the trawl codend open to eliminate any
catch effects on trawl geometry.
Several measures of trawl geometry and performance were taken during each treatment. The
distancebetweenthe doors(doorspread),thewing
tips (wing spread), and the center of the headrope
to the sea floor were measured acoustically with
Scanmar sensors (Scanmar, Asgardstrand, Norway) to 0.1 m at 4-s intervals. Water flow, both
perpendicular and tangential to the headrope,
was measured to 0.1 knot at 24-s intervals with a
Scanmar trawl speed sensor placed at the center
of the headrope. Vessel position was measured
with satellite navigation at 2-s intervals. Bridle
tension was measured in kilograms at 2-s intervals using in-line tension recorders (Billings Ind.
TR-999, N. Falmouth, MA) attached behind the
door legs. Bottom current velocity in cm/s and
direction data were recorded at 10-s intervals.
Footrope off-bottom distance was measured at
five positions simultaneously by placing bottom
contact sensors (BCS) at the center of the footrope, at the corners located 3 m to either side
of the center, and on each wing 1 m behind the
wing tip (Fig. 1). These sensors are self-contained
units consisting of a tilt meter, which measured
angle to the nearest half degree at 0.5 s elapsed
time intervals, and a data logger housed in a watertight stainless steel container that fits inside
a steel sled (Somerton and Weinberg, 2001). One
side of this sled clips into a clamp on the footrope,
which allows that end of the sled to pivot freely
about the footrope while the other end drags along
the bottom (Fig. 2). In this way, changes in the
distance of the footrope from the bottom produced
changes in the recorded tilt angle. Conversion
from tilt angle to distance off-bottom was accomplished by applying a calibration function derived
for each BCS unit by fitting a quadratic function
to data from an experiment in which angles associated with known distances from a hard surface
were measured. The BCS unit extended 44 cm
behind the footrope and weighed (BCS, sled, and
footrope clamp) 8.9 kg in seawater. The clamp extended beneath the footrope by 2 cm and, depending on the extent of penetration into the sediment,
could raise the footrope off the bottom (Fig. 2).
Because the degree of penetration is unknown,
no adjustments to our calibration functions were
made.
Bridle off-bottom distance was measured at six positions simultaneously by placing BCS units on the lower
bridle at distances of 25, 40, and 50 m forward of the
wing tip on both sides of the trawl (Fig. 1). However, the
BCS units used on the bridles differed from those used
on the footrope. These units were mounted on a triangular frame designed to hold the BCS perpendicular
to the bridle (Fig. 2; Somerton, 2003). The triangular
frame measured 49 cm in its longest dimension and was
Figure 2
Bottom contact sensors shown mounted to the footrope (upper)
and bridle (middle). The footrope shown in the “on-bottom”
position without lateral tension and on a hard surface is
elevated 2 cm by the footrope clamp (lower).
held in place by a cable stop that also extended beneath
the bridle by about 2 cm. The weight of a bridle BCS
unit and frame was 8.7 kg in seawater.
Data analyses
Three tilt angle measurements from each BCS unit were
averaged for each 1.5-s interval, converted to distance
off-bottom by applying the calibration function determined for that unit, and then the off-bottom distances
24
Fishery Bulletin 104(1)
were averaged for each experimental treatment on each
haul. Mean off-bottom distances for each bridle and footrope position, except the footrope center, were grouped by
offset distance (i.e., long side vs. short side of an experimental treatment) where, for example, the distance
measurements from the 25-m position on the starboard
bridle collected on a starboard treatment (long side) was
grouped with the measurements from the 25-m position
on the port bridle during a port treatment. Under these
groupings, we assumed equality and subsequently refer
to the offsets by whether they were on the long or short
side (e.g., long 5 m) rather than whether they were on
the port or starboard side (e.g., port 5 m).
To allow interpolation between the experimental offsets, cubic spline models (Venables and Ripley, 1994)
were f itted to door spread, wing spread, headrope
height, and the off-bottom distances for each bridle and
footrope position as a function of offset. Bootstrapped
empirical 95% confidence intervals (CI; Efron and Tibshirani, 1993) were estimated for all measured categories as described in the following example for off-bottom
distance as follows: 1) assuming that mean off-bottom
distances within a set were correlated because of local
environmental conditions, we chose 1000 bootstrap replicates by sampling entire sets of measurements with
replacement; 2) we fitted a cubic spline, weighted by the
inverse of the variance, to each bootstrap sample, and
then predicted the mean off-bottom distance for each
1 m of offset; and 3) we ranked the predicted values,
then chose the 25th highest and lowest values as the CI
bounds. Similarly, we estimated the empirical 95% CIs
about the mean off-bottom distance at zero offset in the
same manner except that only zero offset treatments
were considered.
angle-of-attack between the bridle and the direction
of travel ( α ). For flatfish, the vertical distance of the
bridle from the sea floor at which a herding response is
initiated (reaction height) will vary with species, size,
viewing conditions, arousal state, and other variables,
but for illustrative purposes, we considered a reaction
height of 1 cm where video observations indicated that
this value is appropriate for a small flatfish, initially
at rest and unaware of the approaching bridle (Somerton, unpubl. data). Thus the value of the bridle contact
length was determined as the distance between the
wing tip and the point along the bridle at which the
interpolated value of off-bottom distance reached the
reaction height. The angle-of-attack, a, was not measured during the experiment; however, when the trawl
is symmetric, α can be modeled as
Modeling trawl shape
Headrope shape and effective net width
To help visualize the distortion of the trawl that occurs
in response to offset, we created three views of the trawl:
1) the shape of the lower bridle when viewed laterally, 2)
the shape of the headrope when viewed from above, and
3) the shape of the footrope when viewed from in front
of the trawl. In addition, we calculated the area swept
by the bridles (herding area) and the effective net width
(i.e., the greatest lateral dimension of the net).
The curved shape of the headrope when viewed from
above can be approximated as a quadratic (parabolic)
function when the warps are equal in length and there
are no external forces to distort the symmetry of the net
(Fridman, 1969). If the shape remains parabolic as the
warp offset is increased, then the headrope shape can
be uniquely determined with three geometric measurements: 1) the length of the headrope; 2) the distance
between wing tips; and 3) the tangent to the headrope at
its center. The first quantity was measured at the start
of the experiment. The second quantity was measured
acoustically on all hauls, and then averaged by treatment.
The third quantity was calculated as the quotient of the
tangential water velocity (U) divided by the perpendicular
velocity (V) measured by the headrope speed sensor (i.e.,
U/V). With these quantities, the headrope shape was
determined as described in Appendix A.
Although the shape of the headrope determined by
this method is assumed to be parabolic, the headrope
becomes increasingly asymmetric about the direction
of travel as the degree of warp offset increases because
the wing tip on the short side of the net precedes that
on the long side. When this distortion occurs, the mea-
Bridle shape and herding area
The shape of the lower bridle, when viewed laterally
(i.e., off-bottom distance as a function of position along
the bridles), was approximated by linear interpolation between the mean off-bottom distances measured
at the wing, and the 25-, 40-, and 50-m bridle positions. Such shape functions were calculated for both
the long side and the short side of the trawl at each
offset increment.
The herding area can be considered as a function
of the bridle contact length, that is, the length of the
bridle that is sufficiently close to the bottom to elicit a
herding response (Somerton and Munro, 2001) and the
α = Sin −1 ( 0.5(D − W ) / B) ,
where D = the distance between doors;
W = the distance between wing tips; and
B = the distance between the wing tip and the
door.
It is not clear, however, how α will differ between the
long and short side of the trawl when warp offsets occur.
For illustrative purposes, we assumed that α is symmetrical and remains constant during all experimental
values of warp offset. Thus, for each side of the trawl
and for each offset, a value of bridle contact length and
α were first calculated as above, then the width of the
herding area on each side of the trawl was computed as
the bridle contact length times sin (α) and the two areas
were summed together.
25
Weinberg and Somerton: Variation in trawl geometry due to unequal warp length
2500
20
2000
Tension (kg)
V (cm/sec)
10
0
-10
1500
-20
1000
-20
-10
0
10
20
U (cm/sec)
-20
0
10
20
Warp offset (m)
Fi gure 3
Current velocity vectors during each of the
13 experimental tows are shown with arrows.
Vessel direction during these tows is shown
with the dark lines. The axes, labeled U and
V, indicate the latitudinal and meriodonial
components of the velocity vectors in cm / s.
-10
Figure 4
Mean tension (in kilograms) measured on both port and starboard
door legs is shown plotted as a function of warp offset in meters.
Note that on the side with the shorter warp (negative offset),
tension is higher than when the warps are equal and that on the
side with the longer warp, the tension is lower.
sured distance between wing tips becomes increasingly
greater than the effective net width (i.e., the distance
from wing tip to wing tip projected on a plane perpendicular to the direction of travel). The method used to
estimate effective net width was based on headrope
geometry and is described in Appendix A.
Footrope shape viewed from the net mouth
Because of footrope geometry, the importance of footrope
bottom contact to overall net efficiency varies along
the length of the footrope. This feature is true not only
because escapement probability likely changes with the
angle of the footrope in relation to the direction of travel
but also because the proportion of the net width spanned
by a unit length of footrope varies. To help visualize the
latter effect better, we projected the off-bottom distances
from their positions along the footrope onto a plane that
was perpendicular to the direction of travel and spanned
by the effective net width, using the footrope shape
model determined for each offset increment described
in Appendix A.
30 cm/s and current direction was approximately parallel to the trawl towing direction (Fig. 3); consequently
the mean current velocity perpendicular to the towing
direction was quite small (1.8 cm/s).
Bridle tension and geometry
For the single haul in which both tension meters worked
successfully, the bridle tension, combined over both
sides, did not change significantly when regressed on the
warp offset (df=11, P= 0.69). This result indicates that
any distortion of the trawl due to the offset treatments
was not sufficient to appreciably affect the combined
tension and, therefore, the hydrodynamic and frictional
drag of the net and the bridles. However, changing the
relative length of the warps resulted in a progressive
transfer of the tension to the shorter warp (Fig. 4). For
example, based on the average combined bridle tension
(3248 kg), when the difference in warp lengths was
11 m, the shorter warp carried 72% of the total net and
bridle drag.
Headrope speed through the water
Results
Twelve successful tows consisting of 24 sets of treatments were completed during the experiment. Bottom
current velocities ranged from about 5 cm/s to about
The velocity component perpendicular to the headrope
(U) decreased with increasing warp offset, whereas the
absolute value of the velocity tangential (velocities from
the port side of the sensor are opposite in sign to velocities from the starboard side) to the headrope (V) at its
26
Net and door measurements
At zero offset, the mean door spread obtained
was 61.9 m. The mean wing spread was 17.1 m,
and the mean headrope height was 2.0 m. Differences in the means of all three quantities were
not apparent at lower offsets, however headrope
height and wing spread were more sensitive to
changesinlargeoffsetsbecausebothweresignificantly (P<0.05) greater than the zero offset means
when offset was increased to 11 m, whereas door
spread did not differ significantly until the offset
was approximately 14 m (Fig. 6).
Bridle and footrope distance off-bottom
by position
Bridle and footrope off-bottom distance varied considerably with position, not only with respect to the mean
value but also with respect to the sensitivity of the mean
to changes in offset. At zero offset, the mean off-bottom
distance of the bridle declined from 12.3 cm at 50 m from
the wing tips, to 3.2 cm at 40 m and 2.0 cm at 25 m (Fig.
7). Mean off-bottom distance remained small along the
footrope, varying from 1.7 cm at 1 m behind the wing tip
to 2.5 cm at the corner and 1.9 cm at the center.
The mean response to changes in offset varied greatly
by position. Along the bridles, the most sensitive location
wasat50m,whereoff-bottomdistanceincreasedonthe
short side and decreased on the long side with increasing
offset (Fig. 7). At 40 m, a similar pattern was repeated,
but for most offsets on the long side, the off-bottom distance was near the minimum recorded, indicating that
the bridle was resting on the bottom. At 25 m, the bridle
was nearly always in contact with the bottom and offbottom distance was insensitive to variations in warp
offset. Along the footrope, the most sensitive position was
the corner where off-bottom distance increased greatly
with offset, particularly with positive offsets due to the
relaxationinwarptension.Atthecenterofthefootrope,
off-bottom distance was also sensitive to warp offset, responding almost identically on the long and short sides.
At 1 m behind the wing tip, sensitivity to warp offset
was quite low and the off-bottom distance indicated that
1.5
Velocity (m/sec)
center increased (Fig. 5). We interpret this as
indication that the speed sensor at the headrope
was rotated in relation to the direction of travel
as the warp offset was increased. Calculating the
angle between the perpendicular at the center
of the headrope and the direction of travel as
tan−1 (U/V), the angle increased from 11° at 3 m
offset to 61° at 20 m offset. Although the absolute
value of the tangential velocity was measured at
values >0 at zero offset, the tangential velocity
was not significantly different than zero (t-test,
P=0.71). This result indicates that the alignment
of the experimental tows in relation to the prevailing current was sufficient to reduce the cross
current to negligible levels.
Fishery Bulletin 104(1)
1.0
0.5
0.0
0
5
10
15
20
Offset (m)
Figure 5
Current velocity (in m / sec) measured at the center of the headrope for each tow is shown separated into the component perpendicular to the headrope (O) and the component tangential to
the headrope (+). The solid and dashed lines connect the means
at each offset increment. Note, for clarity, that the offsets are
incremented by plus or minus 0.1 m for the tangential and
perpendicular components.
the footrope was in contact with the bottom except for
large offsets on the long side.
An alternate method of assessing the sensitivity of
geometry of the 83-112 Eastern trawl to changes in
offset is to determine if the mean off-bottom distance
at 7 m, the maximum offset allowed under the NOAA
protocols for the 83-112 Eastern trawl, differs statistically from the mean off-bottom distance at zero offset.
Based on the bootstrapped confidence intervals (Fig. 7),
off-bottom distance is significantly different from what
it is at zero offset at the 50-m and 40-m bridle positions
and at the center and corner footrope positions but is
not significantly different at the wing and the 25-m
bridle position.
Bridle shape and herding area
To understand better how the change in tension that
accompanies offsets in warp leads to changes in bridle
shape, we show the mean off-bottom distances plotted
against the BCS positions on the wing and bridles for
both the short side and long side of the trawl. From this
perspective it is clear that as the tension is increased,
off-bottom distance increases on the forward part of the
bridle.Likewise,asthetensionisreduced,theoff-bottom
distance decreases (Fig. 8). For flatfish, the effect of
these changes in off-bottom distance is a change in the
area subjected to herding stimuli. For the case where
the reaction height is 1 cm, the bridle contact length
is determined by the intersection of the line depicting
27
Weinberg and Somerton: Variation in trawl geometry due to unequal warp length
80
75
Door spread (m)
the reaction height with the lines depicting the bridle
shape at each offset (Fig. 8). The change in these lengths
on the short and long sides of the trawl is asymmetric
with changes in warp offset (Fig 9). For the long side,
bridle contact length increases linearly with positive
offset. However, for the short side, bridle contact length
decreases nonlinearly with warp offset—the greatest
changes occurring with small offsets. This difference
likely leads to a change in the total width of the herding
area with changes in warp offset. If, for example, it is
assumed that the angle-of-attack (α) is the same for the
long and short sides of the trawl, then the width of the
herded area declines to a minimum at about 8 m offset,
at which the herded area is reduced by 10.3% compared
to that at zero offset.
70
65
60
55
50
45
0
2
4
6
8
10
12
14
16
18
20
Headrope height (m)
With increasing difference in warp length, the model we
used to describe headrope shape predicts three distinct
changes in shape. First, the headrope is distorted so
that the wing tip on the short side of the trawl precedes
that on the long side in the direction of travel (Fig. 10).
The difference in the forward position of the wing tips,
however, is much less than the warp offset. For example,
an 11-m difference in warp length resulted in an offset
in the position of the wing tips of only 2−3 m. This difference occurs because the increased tension on the short
warp changes the catenary in both the bridles and the
warps (i.e., both become effectively longer as the sag is
reduced). Second, the headrope is distorted so that its
center is increasingly displaced away from the midpoint
between wings and toward the short side of the trawl.
When this displacement occurs, the perpendicular at
the center of the headrope is no longer aligned with the
direction of travel. Third, the headrope is distorted so
that the effective width of the net (i.e., the wing spread
projected to the line perpendicular to the towing direction) becomes increasingly shorter than the distance
measured by the acoustic net sensors. The difference
between the effective and the measured net width is
negligible for offsets up to 7 m but rapidly increases at
greater offsets (Fig. 11).
Wing spread (m)
Headrope shape and effective net width
Footrope shape viewed from in front of the net
The distance of the footrope off-bottom, when viewed from
a position in front of the net, increases with increasing
offset; however, the location of the maximum off-bottom
distance in relation to the midpoint between wings,
shifts slightly with increasing offset (Fig. 12). With offsets of 9 m or less, the position of maximum off-bottom
distance is at the corner of the footrope on the long side
of the trawl. However, with increasing offset, the shift
in the position of the footrope corner changes because
of the rotation of the trawl in relation to the direction
of travel; and at a 20-m offset the footrope corner on
the long side of the trawl is positioned, when viewed on
a plane perpendicular to the direction of travel, almost
exactly midway between the wing tips.
Offset (m)
Fi gure 6
Mean door spread, wing spread, and headrope height
are shown (+) plotted against offset increment. The
means for all values of offset increment were fitted with
a cubic spline function (solid curve). Bootstrapped 95%
confidence bounds are shown with shading. Also shown
are the mean door spread, wing spread, and headrope
height for treatments with zero offset (solid horizontal
line) and the corresponding bootstrapped 95% confidence
bounds (dashed horizontal lines).
28
Fishery Bulletin 104(1)
40
10
Bridle 50 m forward of wing tip
Footrope 1 m aft of wing tip
9
35
8
30
7
25
6
5
20
4
15
3
10
2
5
0
1
−20
−15
−10
−5
0
5
10
15
Bridle 40 m forward of wing tip
18
0
20
−20
−15
−10
−5
0
5
10
15
20
10
15
20
10
15
20
Footrope corner
30
16
25
Distance off-bottom (cm)
14
20
12
10
15
8
10
6
4
5
2
0
−20
−15
4
−10
−5
0
5
10
15
0
20
−20
−15
−10
20
Bridle 25 m forward of wing tip
−5
0
5
Footrope center
18
3.5
16
3
14
12
2.5
10
2
8
6
1.5
4
1
0.5
2
−20
−15
−10
−5
0
5
10
15
20
0
−20
−15
−10
−5
0
5
Offset (m)
Fi gure 7
Mean bridle and footrope distance at each bottom contact sensor position is shown (+) plotted against offset increment.
The means for all values of offset increment were fitted with a cubic spline function (solid curve). Bootstrapped 95%
confidence bounds are shown with shading. Also shown is the mean distance off-bottom for only treatments with zero
offset (solid horizontal line) and the bootstrapped 95% confidence bounds (dashed horizontal lines).
29
Weinberg and Somerton: Variation in trawl geometry due to unequal warp length
Long
50
20
15
0
10
3
5
7
9
11
20
0
0
10
20
30
40
50
45
40
35
30
25
0
Short
25
11
9
20
5
3
15
0
10
5
0
10
20
30
10
15
20
15
20
24.5
7
0
5
20
40
50
Width of swept bridle path (m)
Distance off-bottom (cm)
5
Bridle contact length (m)
25
24.0
23.5
-10.3 %
23.0
22.5
Distance from wing tip (m)
22.0
Figure 8
Mean off-bottom distance is shown plotted against the
distance measured from the wing tip to the positions of
the wing and the three bridle bottom contact sensors.
This approximation to the shape of the bridle when
viewed laterally is shown for each of the offset increments for both the side with the longer warp and the side
with the shorter warp. The dashed line represents the
hypothetical reaction height of a fish. The intersection
of the dashed line with the solid line for each configuration defines the bridle length that is sufficiently close
to the bottom to elicit a herding response.
Discussion
There are two distinct approaches for judging whether a
difference in warp length between the sides of a survey
trawl will lead to a significant bias in estimates of relative abundance. In both approaches we focused on the
adequacy of the maximum 7-m offset allowed for the
83-112 Eastern trawl under NOAA trawl survey protocols. In the first approach, we simply asked whether,
given the sampling effort used in the experiment, any
of the measured dimensions at 7-m offset were statistically different from zero offset. In our experiment,
none of the three standard measures of trawl geometry
(i.e., door spread, wing spread, and headrope height)
0
5
10
Offset (m)
Fi gure 9
The length of the bridle with the off-bottom distance
<1 cm is shown plotted against the offset increment
in meters for both the short warp (solid line) and long
warp (dashed line) sides of the trawl (upper panel). In
both cases the lines are represented using cubic spline
smoothing functions. The width of the swept bridle path
as a function of warp offset is represented in the lower
panel.
differed from mean values at zero offset. This finding
indicates that either these dimensions are fairly robust
to changes in warp offset or that the acoustic measurement of these dimensions was insufficiently precise to
detect a difference. Off-bottom distance, however, was
significantly different at the two forward positions on
the bridles and along the footrope at the center and
corner positions.
From the perspective of trawl survey standardization, however, the detectability of changes in geometry
is not of primary importance; these changes, however,
may produce a significant effect on estimates of relative
abundance. Bias in these estimates could result either
because the change in trawl geometry leads to an inac-
30
Fishery Bulletin 104(1)
20
0 m offset
30
19
Net width (m)
25
20
15
10
5
17
16
15
0
-15
-10
-5
0
5
10
14
15
3 m offset
30
0
25
25
20
20
15
15
10
10
5
5
3
5
7
9
11
20
Offset (m)
5 m offset
30
Figure 11
The mean distance between wing tips measured acoustically (O) during the experimental
tows (net width) and the calculated effective
net width (+) are shown plotted against the
offset increment in meters. Note that there
is little difference between the two measures
of net width until the offset increment is
increased to 9 m.
0
0
Meters
18
-15
-10
-5
0
5
10
7 m offset
30
-15
15
-10
25
20
20
15
15
10
10
5
5
0
5
10
15
9 m offset
30
25
-5
0
0
-15
-10
-5
0
5
10
11 m offset
30
-15
15
25
20
20
15
15
10
10
5
5
0
0
-10
-5
0
5
10
-15
15
-5
0
5
10
15
10
15
20 m offset
30
25
-15
-10
-10
-5
0
5
Meters
Figure 10
Estimated net shape (curve) and position of headrope center (O)
at varying levels of warp offset. The mean distance between wing
tips that was acoustically measured during the experimental tows
is indicated with a dashed line. The maximum lateral dimensions
of the net are indicated with solid vertical lines. The distance
between these lines is the effective net width needed for estimating the area swept by the net.
curate measurement of swept area or because
it leads to a change in catch efficiency.
Relative abundance indices produced for the
eastern Bering Sea shelf survey are based on
catch per area swept between the trawl wings.
As the net distorts on account of differential
warp length, the effective net width will become
increasing less than the width that is acoustically measured during the survey. Thus, net
width will become increasingly overestimated
and relative abundance of fish species therefore
will be underestimated. At 7-m offset, however,
the measured net width differed from the effective net width by only 0.5%, and therefore
this source of error is unlikely to contribute to
bias in the swept area estimates. However, the
difference between measured and effective net
width increases rapidly at greater offsets and
could present a problem if a less restrictive
threshold value of offset were used.
Catch efficiency of the 83-112 Eastern trawl
depends primarily on 1) herding by the bridles,
doors, and the mud clouds they create; 2) the
escapement under the footrope; and 3) the escapement through the mesh in the body of the
net. The relative importance of these three
processes, however, will vary for the major species groups that are targeted in the surveys.
Gadoids (primarily walleye pollock [Theragra
chalcogramma] and Pacific cod [Gadus macrocephalus] appear to have little or no herding
response to the 83-112 Eastern trawl (Somerton, 2004) and rarely pass under the footrope
(Somerton, unpubl. data). However, both Pa-
31
Weinberg and Somerton: Variation in trawl geometry due to unequal warp length
0 m offset
20
long
short
15
10
5
0
0
5
10
15
3 m offset
5 m offset
20
20
Distance off-bottom (cm)
long
short
long
15
15
10
10
5
5
0
short
0
0
5
10
15
0
5
10
15
9 m offset
7 m offset
20
20
long
long
short
15
15
10
10
5
5
short
0
0
0
5
10
0
15
5
10
15
20 m offset
11 m offset
20
20
long
short
long
15
15
10
10
5
5
short
0
0
0
5
10
0
15
5
10
15
Distance from wing tip (m)
Figure 12
Mean off-bottom distances (in cm) at the five bottom contact sensor positions along the
footrope (circles) are shown for each warp offset. The positions are projected onto the wing
tip to wing tip plane to depict the footrope as it would appear if one were looking into the
net from the direction of travel. The vertical solid lines indicate the positions of the wing
tips on the long warp and short warp sides of the trawl. The dashed line indicates the
midpoint between wing tips. Note that the projection considers the reduction in effective
net width with increasing offset.
cific cod and walleye pollock are found gilled in the
body of the net; therefore some mesh escapement may
occur, especially if any distortion of the net results in
altered water flow through the meshes. Video observa-
tions of crabs (snow and Tanner crabs [Chionoecetes
sp.] and king crabs [Paralithodes sp.] show that they
also exhibit little or no herding response to the 83-112
Eastern trawl (Weinberg, unpubl. data). However, both
32
Chionoecetes species (Somerton and Otto, 1999) and red
king crab (Weinberg et al., 2004) do escape under the
footrope. Flatfishes (including yellowfin sole [Limanda
aspera], flathead sole [Hippoglossoides elassodon], and
rock sole [Lepidopsetta bilineata] display a strong herding response to the 83-112 Eastern trawl (Somerton
and Munro, 2001); as much as 49% of the catch consisted of fish that were herded by the bridles into the
net path. Likewise, f latfishes are readily capable of
escaping under the footrope and, for species such as
yellowfin sole, at least 25% of the largest individuals
escape in this manner (Munro and Somerton, 2002).
Thus, the capture efficiency of the trawl is speciesspecific. The change in catch efficiency due to warp
offset is likely minimal for species not captured as a
function of herding and footrope escapement behaviors;
however, because flatfish are susceptible to herding and
are adept at footrope escapement, their catch rate could
potentially be affected most by warp offsets.
Bridle efficiency (i.e., the fraction of fish in the area
between the wing tips and doors that are herded into
the path of the net) for flatfish catch is strongly influenced by the size of the herding area or area swept by
the bridles because flatfish are stimulated to herd by
the close approach or direct contact of the lower bridle.
Although we were able to measure the off-bottom distance along the bridle and thereby predict the shape of
the bridle, there is still considerable uncertainty as to
the exact size of the herding area because the reaction
height of a fish will vary with species, size, physiological
state, state of arousal to the approaching bridle, viewing
conditions for the fish, and, perhaps, other variables.
Additionally, there is uncertainty in the estimate of the
size of the herding area because it is based on the assumption of symmetry in the bridle angle-of-attack—a
symmetry that is increasingly untenable with increasing
offset. Despite this uncertainty, it is likely that the loss
of herding area on one side of the trawl is not countered
by an increase on the other side; thus some overall loss
of herding efficiency is to be expected. In the hypothetical case chosen in our study, the reduction in herded
area was 10.3%, which when applied to a strong herding
flatfish such as rock sole (the herded component of the
catch has been estimated to be about 49%, Somerton
and Munro, 2001), the expected reduction in catch with
an 8-m offset would be roughly 5%.
Flatfish escapement under the footrope will be influenced not only by the increase in off-bottom distance
but also by the location along the footrope where the
increase occurs. At a 7-m offset, the footrope off-bottom
distance is about 2 cm higher in the footrope corner
on the long side of the trawl and approximately 1 cm
higher at the center and opposing corner than at zero
offset (Fig. 12). Footrope off-bottom distances increased
appreciably with greater offsets. Weinberg et al. (2002)
demonstrated that f latfish escapement can increase
with similar increases in footrope off-bottom distance;
however their study focused on a different trawl and
considered escapement for the entire footrope rather
than by position along the footrope. Although we are
Fishery Bulletin 104(1)
unaware of any studies that quantify escapement rate
by position along the footrope, our video observations
indicate that flatfish are less likely to escape under the
footrope near the wings than in the center (Somerton,
unpubl. data). Because it is thecenter portion of the footrope where most of the increases in off-bottom distance
occur in the 83-112 trawl, flatfish escapement is likely
increased and potentially could represent a significant,
but presently unquantifiable, loss in catch and a source
of bias in estimates of relative abundance.
In conclusion, most aspects of the 83-112 Eastern
trawl geometry were significantly degraded by warp
offsetdifferencesequaltoorgreaterthan7mcompared
to zero offset. More importantly, the locations where the
detectable differences occurred could affect catch efficiency; therefore a NOAA threshold value of 4% should
be considered a maximum value for the 83-112 Eastern
trawl and perhaps a more conservative value (less than
4%) would be prudent. However, given today’s standardizedsurveyproceduresfor measuringwarpandforrealtime monitoring of warp offset, the probability of warp
offsets even approaching 7 m is highly unlikely on our
surveys when locked-winches are used. Likewise, we
argue that any appreciable differences in warp lengths
between sides due to stretching are unrealistic because
AFSC charter vessels use large diameter, compressed,
solid-core wire. In fact, a review of the 413 hauls made
during the 2004 EBS survey revealed that only three
tows had a recorded maximum 1-m length difference
between sides (Weinberg, unpubl. data).
Acknowledgments
We would like to thank Captain Brad Lougheed and the
FV Vesteraalen crew, Niles Griffen, Waldemar Janezak,
Van Ngo, and Todd Becker for their outstanding professionalism, positive attitudes, and constant attention to
detail;AFSCscientistsStanKotwickiandDennisBenjamin for their assistance at sea; reviewers Guy Fleischer
and Henry Milliken for their helpful comments; and the
AFSC editorial staff, including Gary Duker, Jim Lee,
and Karna McKinney for their help during the in-house
review and manuscript preparation process.
Literature cited
Efron,B.,andR.Tibshirani.
1993. An introduction to the bootstrap, 436 p. Chapman
and Hall, New York, NY.
Fridman,A.L.
1969. Theory and design of commercial fishing gear.
(Transl. from Russian by Israel Program Sci. Transl.,
Jerusalem) 1973, 489 p. [Available as TT 71-50129
from Natl. Tech. Inf. Serv., Springfield, VA.]
Munro,P.T.,andD.A.Somerton.
2002. Estimating net efficiency of a survey trawl for
f latfishes. Fish. Res. 55:267−279.
Somerton,D.A.
2004. Do Pacific cod (Gadus macrocephalus) and wall-
33
Weinberg and Somerton: Variation in trawl geometry due to unequal warp length
eye pollock (Theragra chalcogramma) lack a herding
response to the doors, bridles and mudclouds of survey
trawls? ICES J. Mar. Sci. 61:1186−1189.
2003. Bridle efficiency of a survey trawl for f latfish:
measuring the length of the bridles in contact with the
bottom. Fish. Res. 60:273−279.
Somerton,D.A.,andP.T.Munro.
2001. Bridle efficiency of a survey trawl for flatfish. Fish.
Bull. 99:641−652.
Somerton,D.A.,andR.S.Otto.
1999. Net efficiency of a survey trawl for snow crab,
Chionoecetes opilio, and Tanner crab, C. bairdi. Fish.
Bull. 97:617−625.
Somerton,D.A.,andK.L.Weinberg.
2001. The affect of speed through the water on footrope
contact of a survey trawl. Fish. Res. 53:17−24.
Stauffer,G.
2004. NOAA protocols for groundfish bottom trawl surveys of the nation’s fishery resources. NOAA. Tech.
Memo. NMFS -F/ SPO- 65, 205 p. Alaska Fisheries
Science Center, 7600 Sand Point Way N.E., Seattle,
WA, 98115.
Venables,W.N.,andB.D.Ripley.
1994. Modern applied statistics with S-plus, 462 p.
Springer-Verlag, New York, NY.
Weinberg,K.L.,D.A.Somerton,andP.T.Munro.
2002. The effect of trawl speed on the footrope capture
efficiency of a survey trawl. Fish. Res. 58:303−313.
Weinberg,K.L.,R.S.Otto,andD.A.Somerton.
2004. Capture probability of a survey trawl for red
king crab (Paralithodes camtschaticus). Fish. Bull.
102:740−749.
Appendix 1: Estimating headrope and footrope
shape when the warps differ in length
20
y = cx 2,
(1)
where c is a constant controlling the shape (Fig. A1).
As the headrope is distorted by a differential in warp
length, not only does the value of c change, but the
headrope is displaced along the path of the parabola, so
that its center is no longer aligned with the vertex of the
parabola. A unique solution to the shape of the headrope
when it is distorted in this manner can be determined
from three types of data: the total headrope length (L),
the measured distance between the wing tips (W), and
the measured slope (tangent) of the parabola at the
center of the headrope (tan). The third quantity can be
obtained from the V (perpendicular to the footrope) and
U (tangential to the footrope) velocities measured by the
headrope speed sensor as the quotient U/V. With these
quantities, the solution can be obtained as follows.
A small length interval measured along the headrope
can be expressed as
1
ds = (dy2 + dx 2 ) 2 .
(2)
Which, after substitution of the derivative of Equation
1, is
(
ds = 1 + (2cx)2
)
1
2
dx.
(3)
The length of any segment of the headrope, measured
from the port end (xlower), is then
x
S=
∫ (1 + (2cx)
xlower
2
)
1
2
ds.
(4)
15
Y (m)
If a trawl headrope has the same shape as a flexible
twine under a uniformly distributed load, then the shape
of the headrope can be approximated as a quadratic
(parabolic) function (Fridman, 1969; p. 84) as
10
5
0
-10
-5
0
5
10
X (m)
Figure A1
Shape of a trawl headrope as described
by a parabola. The total length of the
headrope (shown with a solid line) is
equal to L. The measured width of the
trawl (shown with a dashed line) is
equal to W. The circle indicates the
center of the headrope where a speed
sensor is located. The speed sensor
measures water speed both perpendicular and parallel to the headrope.
A segment equal to the total length of the headrope
is obtained by integrating up to the starboard end
(xupper).
The solution is approximated numerically in two stages. First, for a trial value of c, Equation 4 is integrated
from trial values of xlower up to the value of x at which
S=L/2 (i.e., xmiddle). The tangent at this position is then
evaluated as 2cxmiddle (based on the derivative of Eq.
1). This process is then repeated iteratively to find the
value of xlower for the specified value of c at which the
calculated tangent equals the tangent value determined
from the headrope speed sensor. The value of xupper is
34
Fishery Bulletin 104(1)
then determined by integrating Equation 4 from xlower
to the value of x at which S=L. The wing tip to wing
tip distance Dwingtip is then calculated as
(
Dwingtip = ( yupper − ylower )2 + (xupper − xlower )2
),
1
2
(5)
where yupper and ylower are obtained from Equation 1. In
the second stage, c is varied and the above process is
repeated iteratively until the value of Dwingtip is found
that is closest to the measured net spread. At this point
the calculated values of Dwingtip and the tangent at the
headrope center will equal the measured values.
The headrope-shape model for each offset was used
to project the off-bottom distances measured at the five
positions along the footrope onto a plane orientated
perpendicular to the direction of travel to depict the
shape of the footrope as it would appear from a position
in front of the trawl. To do this, a shape function was
developed for the footrope. Assuming that the coordinates of the endpoints of the footrope (xlower, xupper, ylower,
yupper) were the same as the headrope, Equation 5 was
iteratively integrated with varying values of c until the
estimated value of the footrope length (S) equaled the
true length (34.1 m):
xupper
S=
∫
xlower
(1 + (2cx) )
2
1
2
dx.
(6)
Once c is determined, Equation 4 is integrated to find
the value of x associated with the value of S at each BCS
(bottom current sensor) position on the footrope.