Klima-, Energi- og Forsyningsudvalget 2020-21
KEF Alm.del Bilag 359
Offentligt
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Technical Report Prepared for:
European Energy
Document Number:
EEN-01-01-TRP-001-1
Omø Syd Offshore Wind Farm Ornithology Impact
Bird Modelling - Final Report
KEF, Alm.del - 2020-21 - Bilag 359: Henvendelse af 20/6-21 fra European Energy om udpegning af fuglebeskyttelsesområde i Smålandsfarvandet
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KEF, Alm.del - 2020-21 - Bilag 359: Henvendelse af 20/6-21 fra European Energy om udpegning af fuglebeskyttelsesområde i Smålandsfarvandet
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Omø Syd Offshore Wind Farm Ornithology
Impact
Bird Modelling - Final Report
Revision History
1
0
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A
Rev.
17-Jun-21
10-Jun-21
08-Jun-21
31-May-21
28-May-21
Date
Update following additional client comments
Update following additional client comments
Update following client review
Client Issue
Internal review
Description
SP
SP
SP
SP
SP
By
MN
MN
MN
MN
MN
Checked
Approved
MHL
MHL
MHL
MHL
© 2021 EPConsult Energies Ltd and European Energy. All rights reserved
EPConsult Energies
Østerbrogade 212
2100 Copenhagen Ø
Denmark
T: +45 5359 3555
T: +44 20 7582 5555
www.ep-consult.dk
[email protected]
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Table of Contents
1
2
3
4
4.1
4.2
4.3
4.4
4.5
4.6
4.7
5
5.1
5.2
5.3
5.4
Introduction ......................................................................... 7
Phase 1 Baseline Data: Birds ..........................................10
Phase 1 Baseline Data: Environment..............................12
Baseline Data Description ...............................................13
Seabed Sediment Type ...................................................... 13
Water Depth ....................................................................... 13
Seabed slope...................................................................... 14
Seabed current speed........................................................ 14
Seabed suitability index for filter-feeding bivalves (DHI) .. 15
Distance from shore........................................................... 15
Shipping activity (AIS 2016 all-vessel shipping data) ....... 16
Phase 2 Developing the Spatial Model ...........................23
Water depth ........................................................................ 24
Seabed slope...................................................................... 25
Seabed current speed........................................................ 26
Seabed suitability index for filter-feeding bivalves (DHI
model, Skov
et al.
2012) ................................................... 27
Distance from shore........................................................... 28
Shipping activity (AIS 2016 all-vessel shipping data) ....... 29
Spatial Autoregressive (SAR) Modelling ............................ 30
Model Validation ................................................................ 31
Phase 3: Application of the spatial model to test the
SPA alternatives ................................................................36
Summary and Conclusions ...............................................38
References.........................................................................39
5.5
5.6
5.7
5.8
6
7
8
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Table of Tables
Table Number and Title
Table 3-1: Summary of environmental data included in the spatial modelling analysis
Table 4-1: Seabed sediment type within the study area and within the proposed SPA.
Table 5-1: Summary of the results of the Spatial Autoregressive Modelling for Common Eider
Table 5-2: Summary of the results of the Spatial Autoregressive Modelling for Red-necked Grebe
Table 6-1: Common Eider population estimates and densities for each of the SPA options
Table 6-2: Red-necked Grebe population estimates and densities for each of the SPA options
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Table of Figures
Figure Number and Title
Figure 1-1: Bird Protected Areas
Figure 1-2: Aerial Bird Survey Transects, 2014-15 and 2020-21
Figure 4-1: Water Depths within the study area
Figure 4-2: Seabed slope within the study area
Figure 4-3: Seabed current speed within the study area
Figure 4-4: Filter-feeding bivalve suitability index (source: DHI) within the study area
Figure 4-5: Distance from the shore within the study area.
Figure 4-6: Shipping activity levels (source: AIS 2016) within the study area
Figure 4-7: Seabed Sediment Type
Figure 4-8: Bathymetry
Figure 4-9: Seabed Slope (degrees)
Figure 4-10: Seabed Current Speed (m/s)
Figure 4-11: Filter Feeding Bivalve Suitability Index
Figure 4-12: Shipping Activity (All Vessels AIS 2016)
Figure 5-1: Common Eider density across seabed sediment types
Figure 5-2: Red-necked Grebe density across seabed sediment types
Figure 5-3: Common Eider density and water depth.
Figure 5-4: Red-necked Grebe density and water depth
Figure 5-5: Common Eider density and seabed slope
Figure 5-6: Red-necked Grebe density and seabed slope
Figure 5-7: Common Eider density and mean bottom current speed
Figure 5-8: Red-necked Grebe density and mean bottom current speed
Figure 5-9: Common Eider density and DHI filter-feeding bivalve habitat suitability index
Figure 5-10: Red-necked Grebe density and DHI filter-feeding bivalve habitat suitability index
Figure 5-11: Common Eider density and distance from the shore
Figure 5-12: Red-necked Grebe density and distance from the shore.
Figure 5-13: Common Eider density and shipping activity index (AIS 2016)
Figure 5-14: Red-necked Grebe density and shipping activity index (AIS 2016)
Figure 5-15: Common Eider: density surface model
Figure 5-16: Red-necked Grebe: survey densities 2020-2021
Figure 5-17: Wind farm options and possible SPA exclusion zones
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1
Introduction
The proposed Omø Syd wind farm lies within an area proposed as a Special Protection Area/Bird Protection
Area (SPA) for birds under the EU Birds Directive. This report investigates the possible exclusion of the wind
farm site from the SPA and whether that exclusion could be offset through alternative extensions to the
SPA, to provide quantitative evidence to assist in the overall assessment process. Common Eider and Red-
necked Grebe both occur in the area in internationally important numbers (>1% of the flyway population),
and hence meet the qualifying thresholds for designation.
The aim of this study is to compare the numbers of the two qualifying species (Common Eider
Somateria
mollissima
and Red-necked Grebe
Podiceps grisegena)
within three Special Protection Area (SPA) option
areas: (a) designation as currently proposed, (b) an alternative designation with the wind farm and a 1km
buffer excluded from SPA; and (3) the exclusion proposed in (b) plus additional extension options. The study
area for this work was defined to include all of the proposed SPA and its surrounds (see Figure 1-1), where
baseline bird and environmental data were available.
The work had three specific phases:
Phase 1 - Integration of all relevant bird survey data to estimate bird densities in grid squares within
the area surveyed.
Phase 2 - Spatial modelling with environmental factors (including seabed habitat type, water depth,
seabed topography, distance from shore and distance from potential sources of disturbance (e.g. main
shipping channels, designated hunting areas) - to understand the factors affecting bird distribution and
predict bird densities in unsurveyed areas.
Phase 3 - Application of the model to test the SPA alternatives.
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Figure 1-1: Bird Protected Areas
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Figure 1-2: Aerial Bird Survey Transects, 2014-15 and 2020-21
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2
Phase 1 Baseline Data: Birds
The first phase of the work was to collate and process the available bird survey data to be used in the spatial
modelling exercise. This included:
Assessing the coverage of the baseline bird surveys in relation to the maximum extent of the proposed
SPA, to identify the gaps (in space and time).
Determining an appropriate size for a grid square overlay of the SPA, optimised for the scale of data
available on birds and habitats/environmental data. A grid square of 1x1km was chosen for the
modelling in line with the spatial scale of the study and the bird surveys. Grid squares were centred on
the survey transects.
Collation of the raw bird survey data and survey effort (transect routes, dates of surveys).
Standardising the data for survey effort.
Taking into account the seasonality of use of the area.
Calculation of an overall value of bird density for grid squares covered by the baseline surveys
expressed as mean count per unit area (with confidence intervals).
Two survey programmes have been undertaken by the developer of the Omø Syd wind farm. Both were
carried out by BioConsult, an international leader in seabird aerial survey techniques. The survey transects
are shown in Figure 1-2. Surveys comprised:
2020-21 - survey area included wind farm site plus buffer and most of the pSPA (a total area of about
1,050km
2
). Nine surveys were carried out over the whole of this area, at approximately 3-4 weeks
intervals between October 2020 and April 2021.
2014-15 - carried out to inform the original project EIA. These covered a reduced survey area of 550km
2
but the same survey methodology and transects as the 2020-21 surveys (within the reduced area).
Figure 1-2 shows the transect routes followed in each year. Five surveys were carried out in total,
between October and December 2014, and in March and April 2015.
All surveys were carried out as visual aerial surveys to maintain consistency over time and allow comparison
with the Danish national monitoring scheme (NOVANA), using a standard survey protocol. Two observers
were used, each covering one side of the aircraft. Flight altitude during surveys was standardised at 78m
(250 feet) at a cruising speed approximately 185 km (100 knots, Kahlert
et al.
2000), to enable rapid
approach to birds sitting on the sea, causing minimal disturbance but still allowing time for identification.
Birds were recorded to three standardised distance intervals out from the track-line taken by the aircraft:
49-174m (band A), 175-459m (band B) and 460m-1km (band C). Observers could not observe a band of
width 49 m on either side of the flight track since this was obscured by the body of the plane. The limits of
each band were determined using a clinometer which enabled the measurement of predetermined angles
below the horizontal measured abeam (at 78m altitude, the 49m cut-off is an angle of 60° from the
horizontal, 174m is 25° and 459m represents 10° declination). Position along the transect was recorded
by noting the precise time (to the nearest second) at which the bird or flock of birds is perpendicular to the
observer using watches synchronised with GPS. The time at which each observation along the transect was
made can be converted into a position by interpolating the GPS data and placing observations into a
predetermined distance from the track-line according to the band in which the bird was recorded.
No correction was made for diving/submerged birds, so the values should be treated as minimum
estimates, but this would not be expected to affect the proportionate distributions (and hence the key
conclusions of the report).
The visual aerial surveys raised two specific data issues:
Declining detectability from the survey platform - birds were recorded to distance bands from the survey
aircraft, but this was effectively only two bands for these surveys and so few birds were recorded in
band C - only 3% of Common Eider records and zero Red-necked Grebe were recorded in band C during
2020-21, and 6.5% of Common Eider in 2014-15. No Grebes were again recorded in band C in 2014-
15.
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o
Whilst it would be possible to adopt a simple approach and use only the Band A data to calculate
bird densities (Diederichs
et al
2002), this would mean discarding large amounts of data that were
recorded in Band B. Options were therefore explored to maximise the use of the data, use the
principles of distance sampling to estimate correction factors to incorporate the Band B data as
well as that from Band A (though with effectively only two bands DISTANCE software itself could
not be used). Distance correction factors were calculated for Band B for each survey, standardising
to the same overall density as Band A. Data from Band C was not used in the density estimates
(as this comprised only a very small proportion of the data set and was insufficient to generate
reliable estimates).
Identification to species level - whilst Common Eiders were readily recognisable from a survey plane, it
is difficult to separate Red-necked Grebe from another grebe species that occurs frequently in this
area, Great Crested Grebe. Whilst some observers were able to do this confidently, others recorded
only to ‘grebe species’.
o
Further examination of the survey data showed that there was a marked seasonal pattern of
occurrence of confirmed identifications of these species, that could be used to classify the
unidentified records. Overall, from the 2020-21 data, 91% of confirmed Great Crested Grebe
records occurred before 15 November, whilst 94% of Red-necked Grebe were seen after this date,
so this was used as a cut-off to classify the unidentified records to species.
Older data from the NOVANA monitoring and from the Smålandsfarvandet Offshore Wind Farm proposal
(which did not go ahead) were also collated for this study but time constraints (and issues with data
temporal and spatial coverage) meant that they could not be included explicitly in the modelling work. There
may, however, be an opportunity for further model testing and refinement using those data during the EIA
updating exercise. For this current exercise, the 2020-21 data have been used for the initial model building
as the most up-to-date baseline and with widest coverage, then that model has been tested with the 2014-
15 data over the reduced area that those earlier surveys covered.
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3
Phase 1 Baseline Data: Environment
Data on the environmental factors that could affect Common Eider and Red-necked Grebe distribution
across the study area were collated and are summarised in Table 3-1. They included:
seabed sediment type;
water depth;
seabed slope;
seabed current speed;
seabed suitability index for filter-feeding bivalves (DHI model - Skov
et al.
2012)
distance from shore;
shipping activity (AIS 2016 all-vessel shipping data);
hunting and hunting-free areas.
All were available across the whole of the study area.
Table 3-1: Summary of environmental data included in the spatial modelling analysis
Environmental Data
Seabed sediment type
Index of seabed suitability for filter-
feeding bivalves
Water Depth
Seabed slope;
Seabed current speeds
Shipping activity
Distance from shore
Designated hunting areas and
shooting-free refuges in the region;
Source
GEUS download
DHI model (Skov
et al.
2012)
COWI
COWI
DHI
AIS data 2016 (all
vessels)
https://www.soefartsstyrelsen.dk/sikkerhed-til-
soes/sejladsinformation/download-data/datasaet
Calculated from coastline
https://miljoegis.mim.dk/spatialmap?profile=miljoegis-
skovdrift
Derived from a DHI hydrodynamic/nutrient
flow/ecological productivity model that incorporates
data on tide, salinity, temperature and nutrient run-off
and loadings (Skov
et al.
2012)
Bathymetry by 50m grid
Calculated from bathymetry data to 50m grid
Comments
It had been intended to investigate the effect of hunting disturbance as an additional variable in the
modelling, but as no quantitative data were available on hunting levels or locations within the proposed
SPA, this was not investigated further.
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4
4.1
Baseline Data Description
Seabed Sediment Type
The seabed sediment types across the study area are shown in Figure 4-7. The total areas of each habitat
within the proposed SPA are given in Table 4-1.
Table 4-1: Seabed sediment type within the study area and within the proposed SPA.
Seabed sediment type
Mud and muddy sand
Muddy sand
Sand
Till/diamicton
Area (study area) km
2
72
140
127
338
% of study area
11%
21%
19%
50%
4.2
Water Depth
The study area bathymetry is shown in Figure 4-8, with deeper areas shown in blue and shallower in red.
The range of water depths across the survey area is shown in the histogram in Figure 4-1. Most of the study
area was relatively shallow, with only a small area of deeper water, predominantly in the western part of the
area (Figure 4-1).
Figure 4-1: Water Depths within the study area
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4.3
Seabed slope
Seabed slope was calculated on a 50m grid basis by COWI for input into the modelling. Slopes across the
study area are mapped in Figure 4-9. The large majority of the seabed across the study area was flat, with
only a small area of areas of higher slope (Figure 4-2).
Figure 4-2: Seabed slope within the study area
4.4
Seabed current speed
Figure 4-10 shows the distribution of seabed current speeds within the study area, and these are
summarised in Figure 4-3. Most areas had low current speeds, with areas of higher speed largely restricted
to the western part of the survey area.
Figure 4-3: Seabed current speed within the study area
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4.5
Seabed suitability index for filter-feeding bivalves (DHI)
The seabed suitability index for filter-feeding bivalves from the DHI model (Skov
et al.
2012) is mapped
across the study area in Figure 4-11 and summarised in Figure 4-4. Large parts of the study were classed
as very low suitability, with two separate zones of higher suitability (shown in Figure 4-11 as red/orange
areas).
Figure 4-4: Filter-feeding bivalve suitability index (source: DHI) within the study area
4.6
Distance from shore
Figure 4-5 summarises the distribution of distances from the shore across the study area. The most frequent
category was within 1km of the shore, and the majority within 5km, up to a maximum of 10km.
Figure 4-5: Distance from the shore within the study area.
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4.7
Shipping activity (AIS 2016 all-vessel shipping data)
Shipping activity within the study area (as determined from the 2016 AIS data) was concentrated within the
main shipping channel on the western edge (Figure 5-15 and Figure 4-6), with much less within the
proposed SPA.
Figure 4-6: Shipping activity levels (source: AIS 2016) within the study area
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Figure 4-7: Seabed Sediment Type
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Figure 4-8: Bathymetry
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Figure 4-9: Seabed Slope (degrees)
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Figure 4-10: Seabed Current Speed (m/s)
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Figure 4-11: Filter Feeding Bivalve Suitability Index
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Figure 4-12: Shipping Activity (All Vessels AIS 2016)
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5
Phase 2 Developing the Spatial Model
The first stage of the modelling was an initial exploration of the bird densities of each of the two key species
(Common Eider and Red-necked Grebe) and each environmental variable.
Figure 5-1 shows the mean (+ standard error) Common Eider density in each of the four main seabed
sediment types. The till/diamicton areas held the highest Eider densities, and the mud/sandy mud the
lowest, i.e., there were mode Eiders on hard substrates. Common Eider densities were statistically
significantly different between sediment types (Kruskal Wallis test: H=15.6, p=0.0014, n=509).
Figure 5-1: Common Eider density across seabed sediment types
There was no clear relationship between Red-necked Grebes density and seabed sediment type (Figure 5-
2), with no statistically significant difference (Kruskal Wallis test: H=6.7, p=0.08, n=509).
Figure 5-2: Red-necked Grebe density across seabed sediment types
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5.1
Water depth
Common Eider densities were higher in shallower water (<10m depth) and lowest below 20m (Figure 5-3).
This difference was statistically significant (Kruskal Wallis test: H = 140.4, p<0.0001, n = 509).
Figure 5-3: Common Eider density and water depth.
Red-necked Grebes were found at reduced density in the shallowest waters (0-5m), and there were no
records at all from deeper waters (more than 20m) (Figure 5-4). This difference was statistically significant
(Kruskal Wallis test: H = 27.5, p=0.0001, n = 509).
Figure 5-4: Red-necked Grebe density and water depth
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5.2
Seabed slope
There was a trend for higher Common Eider densities where seabed slopes were shallower, but this was
only a weak relationship. Densities in the 0.25-0.5 degree mean slope zone were significantly higher than
those in both flatter and more sloping areas (Kruskal Wallis test: H = 49.6, p<0.0001, n = 509).
Figure 5-5: Common Eider density and seabed slope
Red-necked Grebe density was also highest in the 0.25 - 0.5 degree class (Figure 5-6), and this was
statistically significant (Kruskal Wallis test: H = 12.5, p=0.028, n = 509).
Figure 5-6: Red-necked Grebe density and seabed slope
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5.3
Seabed current speed
Common Eider density was generally higher in areas of higher seabed current speed (possibly as a result of
the effect of current on food availability/feeding conditions (Kruskal Wallis test: H = 12.5, p=0.028, n =
509), Figure 5-7.
Figure 5-7: Common Eider density and mean bottom current speed
Red-necked Grebe density was generally similar across the range of seabed current speed, though with the
notable exception of the mid-range speed class which was significantly higher (Kruskal Wallis test: H = 14.2,
p=0.015, n = 509), Figure 5-8.
Figure 5-8: Red-necked Grebe density and mean bottom current speed
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5.4
Seabed suitability index for filter-feeding bivalves (DHI model, Skov
et al.
2012)
Common Eider density was higher in areas with higher DHI filter-feeding bivalve habitat suitability index
values (Figure 5-9), a result that was highly statistically significant (Kruskal Wallis test: H = 161.9,
p<0.0001, n = 509), and one that would be expected given that filter-feeding bivalves such as mussels
would be likely to form an important part of the Common Eider diet.
Figure 5-9: Common Eider density and DHI filter-feeding bivalve habitat suitability index
Red-necked Grebe density did not show any clear trends with the DHI filter-feeding bivalve habitat suitability
index at lower values (Figure 5-10), with no significant difference between classes (Kruskal Wallis test: H =
8.4, p=0.21, n = 509) (though this would be expected given that this species feeds predominantly on fish).
Figure 5-10: Red-necked Grebe density and DHI filter-feeding bivalve habitat suitability index
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5.5
Distance from shore
Common Eider densities were higher within 3km of the shore, and also, to a lesser extent in the further
(>7km from shore) zone (Figure 5-11). Differences were statistically significant (Kruskal Wallis test: H =
48.0, p<0.0001, n = 509).
Figure 5-11: Common Eider density and distance from the shore
Red-necked Grebe densities were generally higher further from the shore (Figure 5-12). Differences were
statistically significant (Kruskal Wallis test: H = 25.1, p=0.0007, n = 509).
Figure 5-12: Red-necked Grebe density and distance from the shore.
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5.6
Shipping activity (AIS 2016 all-vessel shipping data)
Common Eider densities were generally higher in areas of lower shipping activity, particularly in comparison
with the highest shipping level (Figure 5-13). Differences were statistically significant (Kruskal Wallis test:
H = 61.9, p<0.0001, n = 509).
Figure 5-13: Common Eider density and shipping activity index (AIS 2016)
Higher Red-necked Grebe densities were generally found in the mid-range of shipping activity, with fewer at
both lower and higher shipping levels (Figure 5-14), but these differences were not statistically significant
(Kruskal Wallis test: H = 7.1, p=0.31, n = 509).
Figure 5-14: Red-necked Grebe density and shipping activity index (AIS 2016)
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5.7
Spatial Autoregressive (SAR) Modelling
Spatial Autoregressive Modelling (StataCorp 2021) was used to analyse the bird and environmental data to
investigate how Common Eider and Red-necked Grebe abundance was related to these explanatory
environmental variables. It enabled the location of each grid square to be included in the modelling to take
into account any spatial autocorrelation in the data.
Table 5-1 summarises the results of the SAR for Eider. The model was highly statistically significant overall
(with a pseudo-r2 of 0.295, and p<0.0001), with the main environmental variables associated with
Common Eider density being the DHI filter-feeding bivalve suitability index (strong positive association;
coefficient = 1.32, p=0.005), and distance from the shore (with higher Common Eider densities further from
the shore; coefficient = -0.0047, p=0.015).
Table 5-1: Summary of the results of the Spatial Autoregressive Modelling for Common Eider
Spatial autoregressive model
GS2SLS estimates
Number of obs
Wald chi2(10)
Prob > chi2
Pseudo R2
=
509
= 150.96
= 0.0000
= 0.2954
EI_mean_2021
EI_mean_2021
Depth_mean
Slope_mean
DHIFilterFeed_mean
Current_mean
ShoreDistance
AIS2016_mean
SedimentClass
Muddy sand
Sand
Till/diamicton
_cons
W_contig
EI_mean_2021
e.EI_mean_2021
Coefficient
Std. err.
z
P>|z|
[95% conf. interval]
.7369312
2.554448
1.322938
345.9383
-.0046661
-.0284401
.7817558
8.091822
.4742779
225.5702
.0019229
.047201
0.94
0.32
2.79
1.53
-2.43
-0.60
0.346
0.752
0.005
0.125
0.015
0.547
-.795282
-13.30523
.3933707
-96.17116
-.0084348
-.1209523
2.269144
18.41413
2.252506
788.0477
-.0008973
.0640721
-2.935428
-16.95449
-10.1745
7.409122
3.362433
12.11959
8.404718
5.804013
-0.87
-1.40
-1.21
1.28
0.383
0.162
0.226
0.202
-9.525675
-40.70846
-26.64744
-3.966533
3.654819
6.799479
6.298449
18.78478
.6254558
-.415968
.1658303
.1706669
3.77
-2.44
0.000
0.015
.3004343
-.750469
.9504773
-.0814669
Wald test of spatial terms:
chi2(2) = 14.23
Prob > chi2 = 0.0008
Note:
‘EI_mean2021’ = mean Common Eider density derived from the 2020-21 survey data; ‘Depth_mean’
= Mean sea depth;
‘Slope_mean = Mean seabed slope; ‘DHIFilterFeed_mean’ = mean filter-feeding
bivalve
suitability index (DHI); ‘Current_mean’ = mean bottom current speed; ‘ShoreDistance’ = ditnace of central
point of grid square to shore; ‘AIS2016_mean’ = mean shipping activity
(AIS 2016 data, all vessels),
‘SedimentNo’ = seabed habitat type, with classes given and tested against ‘Mud and sandy mud’ baseline;
W_contig details the spatial correlation matrix.
The SAR results for Red-necked Grebe are shown in Table 5-2. There was a much weaker relationship
between grebe density and the environmental data than there was for Common Eider (with a pseudo-r2
value of only 0.033), though the analysis did still identify a statistically significant relationship between
grebe density and the DHI filter-feeding bivalve suitability index (a weak negative association; coefficient =
-0.00704, p=0.004). The data for Red-necked Grebes were statistically problematic as well, as they
contained a high proportion of zero values (82% of surveyed grid squares held zero r Red-necked Grebes).
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Table 5-2: Summary of the results of the Spatial Autoregressive Modelling for Red-necked Grebe
Spatial autoregressive model
GS2SLS estimates
Number of obs
Wald chi2(10)
Prob > chi2
Pseudo R2
=
509
= 63.60
= 0.0000
= 0.0332
RNG_mean_2021
RNG_mean_2021
Depth_mean
Slope_mean
DHIFilterFeed_mean
Current_mean
ShoreDistance
AIS2016_mean
SedimentClass
Muddy sand
Sand
Till/diamicton
_cons
W_inv
RNG_mean_2021
e.RNG_mean_2021
Coefficient
Std. err.
z
P>|z|
[95% conf. interval]
.0100775
-.0195533
-.0070359
.7270698
9.14e-06
.0007597
.0098401
.0774475
.002432
.6814129
.0000123
.0007378
1.02
-0.25
-2.89
1.07
0.74
1.03
0.306
0.801
0.004
0.286
0.459
0.303
-.0092088
-.1713476
-.0118026
-.6084749
-.000015
-.0006864
.0293638
.132241
-.0022692
2.062614
.0000333
.0022058
.0530355
-.1312287
-.0702287
-.3485771
.0892147
.0951864
.0897957
.1064883
0.59
-1.38
-0.78
-3.27
0.552
0.168
0.434
0.001
-.1218222
-.3177906
-.246225
-.5572903
.2278932
.0553332
.1057675
-.1398639
3.233291
-1.557351
.7353747
1.34616
4.40
-1.16
0.000
0.247
1.791983
-4.195777
4.674599
1.081074
Wald test of spatial terms:
chi2(2) = 19.67
Prob > chi2 = 0.0001
5.8
Model Validation
The outputs from these models were tested initially against the 2020-21 data, to compare the model
predictions with the observed densities of each species. A further independent test of the predictions was
carried out with the 2014-15 data, to see how the model predictions compared with the observed densities
in that winter (only the 2020-21 data were used in the model development), though this could only be
carried out for the reduced survey area that was covered in that year.
Both the 2014-15 and the 2020-21 survey data were strongly correlated with the predicted densities for
Common Eider (r
s
= 0.44 and r
s
= 0.49 respectively, p<0.0001 and n=509 in both years). The predicted
values from the model matched well to the observed survey data, validating the model predictions.
For Red-necked Grebe the SAR model predictions were a poor fit for both the 2014-15 (r
s
= -0.089, p=0.05,
n=509) and the 2020-21 data (r
s
= 0.082, p=0.07, n=509), showing no statistically significant correlation.
The predicted values did not match well to the observed survey data, indicating that the model predictions
were not reliable for this species. This means that the model cannot be used to produce reliable predictions
of Red-necked Grebe densities outside the areas surveyed.
As a reliable model has been produced for Common Eider, this has been used to construct a density surface
model, using a combination of the observed data from the 2020-21 surveys (that covered a wider survey
area) and filling the gaps with the model-predicted densities. The results are shown in Figure 5-15.
The lack of a statistically reliable model for Red-necked Grebe using the environmental variables to predict
grebe density meant that an alternative approach had to be adopted. This was based on the assumption
that the surveyed grid squares within each zone were representative of Red-necked Grebe densities across
the whole of each zone. Population estimates and bird densities were calculated directly from the survey
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data (including correction for distance sampling where data had been collected across more than a single
distance band, as in the main analysis above). The Red-necked Grebe densities (derived directly from the
2020-21 aerial surveys, hence the gaps in coverage) are mapped in Figure 5-16.
Further analysis of the Red-necked Grebe data was undertaken to test if their numbers were consistent in
areas between years. If that were the case, then the grid square densities from the two years (2014-15 and
2020-21) would be expected to be correlated. There was statistically significant correlation between Red-
necked Grebe densities in 2014-15 and 2020-21 (r
s
=0.16, p=0.002, n=507), suggesting that they were
showing some preference for similar areas between years, but this relationship was weak, probably
reflecting variability in their primary food resource (fish).
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Figure 5-15: Common Eider: density surface model
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Figure 5-16: Red-necked Grebe: survey densities 2020-2021
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Figure 5-17: Wind farm options and possible SPA exclusion zones
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6
Phase 3: Application of the spatial model to test the
SPA alternatives
The spatial model was used to derive robust population estimates and measures of overall bird use for the
proposed Special Protection Area (pSPA), and for an alternative area with the Omø Syd wind farm excluded
from the pSPA. The excluded area also included a 1km buffer around the wind farm, incorporated to avoid
the possibility of disturbance effects into the SPA. Additional potential SPA extensions were also investigated
to see if they might offset the negative effect of the exclusion area on the SPA.
Three SPA options were therefore considered:
Option 1 - SPA as current proposed boundary
Option 2 - SPA with exclusion area around current wind farm location;
Option 3 - SPA with exclusion area and alternative potential SPA extension areas..
These options are mapped in Figure 5-17.
The aim of this phase of the work was to determine how many Common Eider and Red-necked Grebe each
of the SPA alternatives would support, and hence what the proportionate reduction would be in the SPA
Eider and Red-necked Grebe populations for the Option 2 and Option 3 alternatives.
The modelling data were also used to determine whether removing the wind farm area from the SPA makes
a material difference to the overall quality of the SPA, in terms of its ability to achieve its threshold
population and to deliver and maintain its conservation objectives (for each of the two alternative options).
The contribution from each of the four possible extension areas is shown in the Table.
Table 6-1 summarises the modelled Common Eider population sizes and densities within the pSPA options.
The key comparisons are the Common Eider populations for each of the options, and the proportionate
change that this represents from the current pSPA. Option 2, with the wind farm and a 1km buffer excluded
from the SPA would result in a reduced total SPA mean population (20,711 compared with 22,531), but
this would still represent about 91.9% of the current pSPA.
The alternative Option 3 with the wind farm exclusion but also with four potential extensions to the SPA
gave a predicted net gain to the Common Eider SPA population, with the updated SPA predicted to hold a
mean population of 23,960 (106.3% of the current pSPA). The contribution from each of the four possible
extension areas is shown in the Table.
Table 6-1: Common Eider population estimates and densities for each of the SPA options
Option
Option 1: current pSPA
Option 2: pSPA with Omø Syd Wind Farm exclusion
Effective loss
Extension 1 gain
Extension 2 gain
Extension 3 gain
Extension 4 gain
Total potential gain (1-4)
Option 3: All extensions combined + Option 2
Mean
population
22,531
20,711
1,820
766
908
1,500
75
3,249
23,960
33.6
712
9
19
43
22
Mean
density
33.3
34.2
Sample
size
677
605
72
81
77
35
3.4
% current
pSPA
100%
91.9%
-8.1%
+3.4%
+4.0%
+6.7%
+0.3%
+14.4%
106.3%
Table 6-2 summarises the estimated Red-necked Grebe population sizes and densities within the three
pSPA options. As for Common Eider, the key comparisons are the Red-necked Grebe populations for each
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of the three options, and the proportionate change that this represents from the current pSPA. Option 2,
with the wind farm and a 1km buffer excluded from the SPA would result in a reduced total SPA population
(145 compared with 165), which would represent about 87.9% of the current pSPA.
For reference, the threshold of international importance given in the pSPA documentation (Petersen
et al.
2016 and 2019) for Red-necked Grebe is 500 (though with the flyway population estimated at 30,000-
45,000). The Red-necked Grebe populations derived from the recent aerial surveys fall well below this
threshold. Option 2 reduced the grebe numbers to 87.9% of the current pSPA levels. From the information
provided in Petersen
et al
2016, 2019 and 2020, it appears to be being suggested that ship-based surveys
produce rather higher populations estimates for this species (with about 1,110-1,900 individuals reported
from surveys in 2014). With problems of species identification and this apparent under-recording of this
species from aerial surveys, it is difficult to draw any firm conclusions for Red-necked Grebe, though the
available evidence would suggest that the additional exclusion areas would reduce the grebe numbers
supported within the SPA by 12.1%.
Table 6-2: Red-necked Grebe population estimates and densities for each of the SPA options
Option
Option 1: current pSPA
Option 2: pSPA w/o current
Omo Syd WF
Mean count
165
145
Mean density
0.244
0.240
Standard error
0.042
0.046
Sample size
677
280
% current pSPA
100.0%
87.9%
The possible SPA extensions have the potential to support small numbers of Red-necked Grebe, and
probably sufficient to offset the reduction from excluding the wind farm from the SPA (given the large overall
total area in comparison with the area lost to the exclusion), but it was not possible to quantity this using
spatial modelling, as the model was not sufficiently reliable (primarily due to the limitations of the baseline
data).
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7
Summary and Conclusions
This study has provided a quantitative comparison of the numbers of the two qualifying species (Common
Eider and Red-necked Grebe) within the two SPA option areas that were being investigated: (a) the current
proposed designation, and (b) an alternative designation with the wind farm and a buffer excluded from
SPA. A third option was also identified during the study, with the wind farm exclusion and four possible SPA
extensions also considered to offset the effect of the exclusion area.
Analysis of the aerial bird survey data has enabled bird densities to be estimated across the survey area,
and, for Common Eider, this has been developed with a spatial autoregression model to predict bird
densities in areas of the SPA that have not been surveyed (on the basis of a range of environmental
variables including the suitability of the seabed conditions to support filter-feeding bivalves, distance from
shore, water depth, current speed, seabed sediment type and shipping activity).
Removing the wind farm area from the SPA (Option 2) made no material difference to the overall quality of
the SPA, in terms of its ability to achieve its threshold population and to deliver and maintain its conservation
objectives. The SPA would considerably exceed the threshold population of 9,800 individuals for all three
options. Comparing the proportionate change in Common Eider populations, the wind farm in its current
position (plus a 1km buffer) excluded from the SPA (Option 2) would result in a reduced total SPA population
to about 91.9% of the current pSPA. The alternative option with the wind farm exclusion but also the SPA
extensions (Option 3) would result in a net gain for the Common Eider SPA population to 106% of the current
pSPA. For Red-necked Grebe, Option 2, would result in a reduction to 87.9% of the current pSPA population.
Quantification of the benefits of the possible SPA extensions was not possible given the limitations of the
baseline survey data, but it is very likely that this combination of exclusion and extension areas would allow
the SPA Red-necked Grebe population to achieve its required conservation status (exceeding the threshold
for designation and meeting its conservation objectives).
The initial recommendation would be to exclude the current proposed wind farm site and a 1km buffer from
the pSPA, as shown in Figure 5-17. This would result in an 8.1% reduction in the SPA Common Eider
population, and a 12.1% reduction in its Red-necked Grebe population.
An alternative option was identified, to extend the SPA to include additional areas and offset the reduction
from the wind fam exclusion. Four possible SPA extensions were identified, which together could deliver a
6% increase in the SPA population of Common Eider in combination with the proposed wind farm exclusion.
Such an approach would also likely offset the reduction in the Red-necked Grebe population within the SPA
as a result of the proposed wind farm exclusion.
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8
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Diederichs, A., Nehls, G. & Petersen, I. K. 2002. Flugzeugzählungen zur großflächigen Erfassung von
Seevögeln und marinen Säugern als Grundlage für Umweltverträglichkeitsstudien im Offshorebereich.
Seevögel, 23: 38-46.
Kahlert, J., Desholm, M., Clausager, I. & Petersen, I.K. 2000. Environmental impact assessment of an
offshore wind park at Rodsand: Technical report on birds. NERI Report: 86pp.
Petersen, I.K., Nielsen, R.D. & Clausen, P. 2016. Assessment of IBA (Important Bird Areas) in relation to bird
protection areas - with particular reference to marine species and areas. Aarhus University, DCE - National
Centre for Environment and Energy, 98 pp. - Technical report from DCE - National Centre for Environment
and Energy No. 202 http://dce2.au.dk/pub/TR202.pdf
Petersen, I.K., Nielsen, R.D. & Clausen, P. 2019. Updated assessment of IBA designations in relation to
eight specific marine areas. Aarhus University, DCE - National Centre for Environment and Energy, 80 pp. -
Technical Report No. 203 http://dce2.au.dk/pub/TR203.pdf
Petersen, IK 2020. Academic contribution regarding. designation of marine bird protection areas. Aarhus
University, DCE - National Centre for Environment and Energy, 25 pp. - - Note No 2020 | 19
https://dce.au.dk/fileadmin/dce.au.dk/Udgivelser/Notater_2021/N2020_19.pdf
Skov, H.
et al.
2012. MOPODECO. Modelling of the Potential coverage of habitat forming species and
Development of tools to evaluate the Conservation status of the marine Annex I habitats. TemaNord
2012:532. ISBN 978-92-893-2368-0. http://dx.doi.org/10.6027/TN2012-532. Nordic Council of
Ministers 2012.
StataCorp. 2021. Stata: Release 17. Statistical Software. College Station, TX: StataCorp LLC.
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