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  <front>
    <journal-meta><journal-id journal-id-type="publisher">WES</journal-id><journal-title-group>
    <journal-title>Wind Energy Science</journal-title>
    <abbrev-journal-title abbrev-type="publisher">WES</abbrev-journal-title><abbrev-journal-title abbrev-type="nlm-ta">Wind Energ. Sci.</abbrev-journal-title>
  </journal-title-group><issn pub-type="epub">2366-7451</issn><publisher>
    <publisher-name>Copernicus Publications</publisher-name>
    <publisher-loc>Göttingen, Germany</publisher-loc>
  </publisher></journal-meta>
    <article-meta>
      <article-id pub-id-type="doi">10.5194/wes-4-273-2019</article-id><title-group><article-title>Initial results from a field campaign of wake steering applied at a commercial
wind farm – Part 1</article-title><alt-title>Initial results from a field campaign of wake steering – Part 1</alt-title>
      </title-group><?xmltex \runningtitle{Initial results from a field campaign of wake steering -- Part 1}?><?xmltex \runningauthor{P. Fleming et al.}?>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes" rid="aff1">
          <name><surname>Fleming</surname><given-names>Paul</given-names></name>
          <email>paul.fleming@nrel.gov</email>
        <ext-link>https://orcid.org/0000-0001-8249-2544</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>King</surname><given-names>Jennifer</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Dykes</surname><given-names>Katherine</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Simley</surname><given-names>Eric</given-names></name>
          
        <ext-link>https://orcid.org/0000-0002-1027-9848</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Roadman</surname><given-names>Jason</given-names></name>
          
        <ext-link>https://orcid.org/0000-0003-2280-5996</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Scholbrock</surname><given-names>Andrew</given-names></name>
          
        <ext-link>https://orcid.org/0000-0003-1241-6356</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1 aff3">
          <name><surname>Murphy</surname><given-names>Patrick</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1 aff3">
          <name><surname>Lundquist</surname><given-names>Julie K.</given-names></name>
          
        <ext-link>https://orcid.org/0000-0001-5490-2702</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Moriarty</surname><given-names>Patrick</given-names></name>
          
        <ext-link>https://orcid.org/0000-0001-7122-5993</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Fleming</surname><given-names>Katherine</given-names></name>
          
        <ext-link>https://orcid.org/0000-0002-4862-0650</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>van Dam</surname><given-names>Jeroen</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Bay</surname><given-names>Christopher</given-names></name>
          
        <ext-link>https://orcid.org/0000-0002-2658-5559</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Mudafort</surname><given-names>Rafael</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>Lopez</surname><given-names>Hector</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>Skopek</surname><given-names>Jason</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>Scott</surname><given-names>Michael</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>Ryan</surname><given-names>Brady</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>Guernsey</surname><given-names>Charles</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>Brake</surname><given-names>Dan</given-names></name>
          
        </contrib>
        <aff id="aff1"><label>1</label><institution>National Wind Technology Center, National Renewable Energy Laboratory,
Golden, CO 80401, USA</institution>
        </aff>
        <aff id="aff2"><label>2</label><institution>NextEra Energy Resources, 700 Universe Blvd, Juno Beach, FL 33408</institution>
        </aff>
        <aff id="aff3"><label>3</label><institution>Dept. Atmospheric and Oceanic Sciences, University of Colorado Boulder, Boulder, CO 80303, USA</institution>
        </aff>
      </contrib-group>
      <author-notes><corresp id="corr1">Paul Fleming (paul.fleming@nrel.gov)</corresp></author-notes><pub-date><day>20</day><month>May</month><year>2019</year></pub-date>
      
      <volume>4</volume>
      <issue>2</issue>
      <fpage>273</fpage><lpage>285</lpage>
      <history>
        <date date-type="received"><day>1</day><month>February</month><year>2019</year></date>
           <date date-type="rev-request"><day>18</day><month>February</month><year>2019</year></date>
           <date date-type="rev-recd"><day>26</day><month>April</month><year>2019</year></date>
           <date date-type="accepted"><day>6</day><month>May</month><year>2019</year></date>
      </history>
      <permissions>
        <copyright-statement>Copyright: © 2019 Paul Fleming et al.</copyright-statement>
        <copyright-year>2019</copyright-year>
      <license license-type="open-access"><license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri" xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p></license></permissions><self-uri xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019.html">This article is available from https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019.html</self-uri><self-uri xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019.pdf">The full text article is available as a PDF file from https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019.pdf</self-uri>
      <abstract><title>Abstract</title>
    <p id="d1e258">Wake steering is a form of wind farm control in which turbines use
yaw offsets to affect wakes in order to yield an increase in total energy
production. In this first phase of a study of wake steering at a commercial
wind farm, two turbines implement a schedule of offsets. Results exploring
the observed performance of wake steering are presented and some
first lessons learned. For two closely spaced turbines, an approximate
14 % increase in energy was measured on the downstream turbine over a
10<inline-formula><mml:math id="M1" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> sector, with a 4 % increase in energy production of the
combined upstream–downstream turbine pair. Finally, the influence of
atmospheric stability over the results is explored.</p>
  </abstract>
    </article-meta>
  <notes notes-type="copyrightstatement">
  
      <p id="d1e277">This work was authored by the National Renewable Energy
Laboratory, operated by the Alliance for Sustainable Energy, LLC, for the U.S.
Department of Energy (DOE) under contract no. DE-AC36-08GO28308.</p>
      <p id="d1e280">The U.S. Government retains and the publisher, by accepting the article for
publication, acknowledges that the U.S. Government retains a nonexclusive,
paid-up, irrevocable, worldwide license to publish or reproduce the published
form of this work, or allow others to do so, for U.S. Government purposes.</p>
</notes></front>
<body>
      


<sec id="Ch1.S1" sec-type="intro">
  <label>1</label><title>Introduction</title>
      <p id="d1e291">Wind farm control is a field of research in which the control actions of
individual turbines are coordinated to improve the total performance of the
wind farm as defined by the total power production of the wind farm and the loads experienced by downwind turbines. Wake steering is a form of
wind farm control wherein an upstream turbine intentionally offsets its yaw
angle with respect to the wind direction to benefit downstream turbines
<xref ref-type="bibr" rid="bib1.bibx25 bib1.bibx6" id="paren.1"/>.<?xmltex \hack{\newpage}?></p>
      <p id="d1e298">Wake steering has been studied through wind tunnel studies
<xref ref-type="bibr" rid="bib1.bibx18 bib1.bibx21 bib1.bibx22 bib1.bibx2" id="paren.2"><named-content content-type="pre">e.g.,</named-content></xref>,
and large-eddy simulation (LES) studies of wake steering have been undertaken
to date <xref ref-type="bibr" rid="bib1.bibx8 bib1.bibx24 bib1.bibx13" id="paren.3"><named-content content-type="pre">see, for
example,</named-content></xref>.
Coupled with theoretical derivations, the results of the previously mentioned
studies have enabled the development of control-oriented engineering models
of wakes and wake steering that can be used to design and analyze wake
steering controllers for wind farms and predict the performance
benefit. Important examples include the Jensen wake model
<xref ref-type="bibr" rid="bib1.bibx14" id="paren.4"/> and the model of wake steering by
<xref ref-type="bibr" rid="bib1.bibx15" id="text.5"/>.</p>
      <?pagebreak page274?><p id="d1e317">Flow Redirection and Induction in Steady State (FLORIS;
<xref ref-type="bibr" rid="bib1.bibx20" id="altparen.6"/>) is a software repository that provides an engineering
model of wake steering that can be used in the design and analysis of wind
farm control applications <xref ref-type="bibr" rid="bib1.bibx11" id="paren.7"/>. Originally based on
<xref ref-type="bibr" rid="bib1.bibx14" id="text.8"/> and <xref ref-type="bibr" rid="bib1.bibx15" id="text.9"/>, it now employs
the wake recovery and redirection models of
<?xmltex \hack{\mbox\bgroup}?><xref ref-type="bibr" rid="bib1.bibx3 bib1.bibx4" id="text.10"/><?xmltex \hack{\egroup}?> and
<xref ref-type="bibr" rid="bib1.bibx19" id="text.11"/>. <xref ref-type="bibr" rid="bib1.bibx1" id="text.12"/> provide a detailed
description of the current FLORIS model. The FLORIS model is open source and
available for download and collaborative development
(<uri>https://github.com/nrel/FLORIS</uri>, version 1.0.0, last access:
1 May 2019). Development is ongoing, and future models will incorporate the
advances proposed in <xref ref-type="bibr" rid="bib1.bibx17" id="text.13"/>.</p>
      <p id="d1e350">Critical to advancement, improvement, and eventual adoption of wake steering
are field trials of wake steering in realistic environments.
<xref ref-type="bibr" rid="bib1.bibx25" id="text.14"/> attempted wake steering at a scaled wind
farm. One important campaign took place at the National Wind Technology
Center in Boulder, Colorado. In that study, a rear-facing scanning lidar from
the University of Stuttgart was placed on top of the nacelle of a GE 1.5 MW
turbine, which held various yaw offset positions for periods of 1 h at a
time <xref ref-type="bibr" rid="bib1.bibx9" id="paren.15"/>. The data from that campaign were used to
investigate the accuracy of predictions made by FLORIS
<xref ref-type="bibr" rid="bib1.bibx1" id="paren.16"/> and the impact on turbine loads caused by
yaw offsets <xref ref-type="bibr" rid="bib1.bibx7" id="paren.17"/>. A related campaign is being
undertaken at the Scaled Wind Farm Technology facility in Lubbock, Texas.
Similar to the National Wind Technology Center study, a rear-facing lidar (in
this case the Technical University of Denmark spinner lidar) is used to scan
the wake of a V27 experimental turbine. The resulting data are used to
examine wake behavior <xref ref-type="bibr" rid="bib1.bibx12" id="paren.18"/> and understand loading
impacts <xref ref-type="bibr" rid="bib1.bibx28" id="paren.19"/>. Finally, a first published field trial
at a commercial offshore wind farm is presented in
<xref ref-type="bibr" rid="bib1.bibx10" id="text.20"/>. In that study, a single turbine implements a
yaw offset control strategy to benefit three downstream turbines.</p>
      <p id="d1e376">Still, there is a need for more conclusive field campaigns on the performance
of wake steering and the evaluation of the latest models. For this
reason, a new field campaign was initiated as a collaboration between the
National Renewable Energy Laboratory (NREL) and NextEra Energy Resources. A
portion of a commercial wind farm was selected as a test site, and
significant additional sensing equipment is being deployed, including a
(ground-based) lidar, meteorological (met) tower, and two sodars. Additional
nacelle-based lidars are being deployed for the upcoming second phase. Wake
steering controls based on the latest version of FLORIS are implemented on
two turbines. This paper presents the results of the first phase of this
campaign focused on wake steering.</p>
      <p id="d1e379">The main contribution of this paper is the initial results and analysis of a
land-based wake steering field-test campaign. The paper presents the
controller as implemented in the present phase and proposes improvements
based on these initial results. The performance of wake steering, in terms of
increased energy production, is analyzed and compared with predictions from
the FLORIS code. In addition, the wake steering performance is assessed with
respect to atmospheric stability, which can be estimated using sensing
available on the met mast. Finally, several practical lessons learned are
discussed.</p>
      <p id="d1e382">The paper is organized as follows. Section <xref ref-type="sec" rid="Ch1.S2"/> provides an overview
of the field campaign's layout of turbines and sensors, as well as
meteorological conditions. Section <xref ref-type="sec" rid="Ch1.S3"/> discusses the implemented
controller. Section <xref ref-type="sec" rid="Ch1.S4"/> describes the data collected in terms of
total amount and characteristics. The performance of the controller,
specifically in terms of achieving targeted offsets, is reviewed in
Sect. <xref ref-type="sec" rid="Ch1.S5"/>. Challenges specific to this first phase are
described in Sect. <xref ref-type="sec" rid="Ch1.S6"/>. Finally, Sect. <xref ref-type="sec" rid="Ch1.S7"/>
presents the results.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F1" specific-use="star"><?xmltex \currentcnt{1}?><label>Figure 1</label><caption><p id="d1e400">Layout of the experimental site. Turbine 2 (T2) and Turbine 4 (T4)
have wake steering implemented to benefit Turbine 3 (T3), whereas Turbine 1
(T1) and Turbine 5 (T5) are reference turbines. The position of the installed
meteorological equipment is also shown. Finally, the complexity of the
terrain to the south and the flat terrain to the north are indicated.</p></caption>
        <?xmltex \igopts{width=398.338583pt}?><graphic xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019-f01.png"/>

      </fig>

</sec>
<sec id="Ch1.S2">
  <label>2</label><title>Field campaign</title>
      <p id="d1e417">A subsection of a commercial wind farm was selected as the test site for the
wake steering campaign. The site was chosen to include a set of turbines
for which the main wind directions that generate strong waking conditions would
occur relatively frequently and the turbines were close enough for wake
steering effects to be discernible. The selected wind farm subsection is
shown in Fig. <xref ref-type="fig" rid="Ch1.F1"/>.</p>
      <p id="d1e422">Five turbines (Fig. <xref ref-type="fig" rid="Ch1.F1"/>) are located in one corner of the
farm. Note that there are no turbines to the north or south, making these
wind directions effectively free stream. The five turbines are relatively
closely spaced, especially the three turbines labeled T2, T3, and T4. T2 and
T4 were controlled turbines, and T3 was selected as the downstream turbine to
be evaluated based on the wake impacts of T2 and T4. The wind directions at which T2
(324<inline-formula><mml:math id="M2" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>) and T4 (134<inline-formula><mml:math id="M3" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>) directly wake T3 are indicated in
Fig. <xref ref-type="fig" rid="Ch1.F1"/>. T1 and T5 serve as reference turbines that are uncontrolled
and unaffected by the control turbines during wind conditions under which
controls would be applied. Figure <xref ref-type="fig" rid="Ch1.F2"/> illustrates the
directional conventions for steering applied to the T4 and T3 turbine pair.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F2"><?xmltex \currentcnt{2}?><label>Figure 2</label><caption><p id="d1e451">Illustration of wake steering showing that a positive yaw offset is
meant to indicate a counterclockwise rotation of the controlled turbine.</p></caption>
        <?xmltex \igopts{width=170.716535pt}?><graphic xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019-f02.png"/>

      </fig>

      <p id="d1e461">The terrain of the site is also illustrated in Fig. <xref ref-type="fig" rid="Ch1.F1"/>.
Generally, the terrain to the north is flat, whereas the terrain to the south
is complex (some escarpments can be seen in the southwest in
Fig. <xref ref-type="fig" rid="Ch1.F1"/>, and these extend to the south of T4). The campaign is
divided into the “north” campaign, wherein flows from the north arrive over
flat terrain and T2 is the controlled turbine, and the “south” campaign,
wherein flows from the south arrive over complex terrain and are expected to be
more turbulent.</p>
      <p id="d1e468">The locations of the meteorological equipment are indicated in
Fig. <xref ref-type="fig" rid="Ch1.F1"/>. Based on the simpler terrain and overall wind rose,
the equipment is placed to prioritize the north campaign. A Leosphere
Windcube v2 profiling lidar (shown in Fig. <xref ref-type="fig" rid="Ch1.F1"/>) provides
profiles of wind speed and wind direction calculated nominally every second
but averaged to 1 min intervals. This lidar (similar to that used in
<xref ref-type="bibr" rid="bib1.bibx16" id="altparen.21"/>) samples line-of-sight velocities in four cardinal
directions along a nominally 28<inline-formula><mml:math id="M4" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> azimuth from vertical, followed by a
fifth vertically pointed beam. Range gates were centered every 20 m from
40 m up to 180 m. The sodars used in the campaign are Vaisala Triton Wind
Profilers. The sodars<?pagebreak page275?> provide measurements of wind speed and wind direction
every 20 m up to 200 m.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F3" specific-use="star"><?xmltex \currentcnt{3}?><label>Figure 3</label><caption><p id="d1e489">Total wind rose for the site and for the particular months
encompassing the test based on data collected from
<uri>https://www.nrel.gov/grid/wind-toolkit.html</uri> (last access: 1 May 2019).</p></caption>
        <?xmltex \igopts{width=455.244094pt}?><graphic xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019-f03.png"/>

      </fig>

      <p id="d1e501">Phase 1 of the field campaign uses an initial deployment of the wake steering
controller and initial collection of data over the summer of 2018 (from
4 May through 11 July 2018). The wind resource is seasonal: in the summer,
southern winds are more probable than northern winds. Figure <xref ref-type="fig" rid="Ch1.F3"/>
shows two wind roses for the site, for which data were obtained using
the NREL Wind Integration National Dataset tool kit at 100 m of height.
Figure <xref ref-type="fig" rid="Ch1.F3"/>a shows the annual wind rose, with winds coming
dominantly from the north-northwest and south-southeast.
Figure <xref ref-type="fig" rid="Ch1.F3"/>b shows the expected wind rose for the months during
which the campaign was run with more frequent south-southeasterly winds.</p>
      <p id="d1e510">Controllers were implemented and running on both T2 and T4. Because the
south-southeasterly winds are more prominent in this season, phase 1 focuses
on the south campaign as most of the collected data correspond to this
direction. The final study will consider the north experiment as well.
Because of this focus on the south campaign, the most relevant components in
Fig. <xref ref-type="fig" rid="Ch1.F1"/> are T4 (controlled turbine), T3 (downstream turbine),
and the south sodar to measure inflow.</p>
</sec>
<sec id="Ch1.S3">
  <label>3</label><title>Controller</title>
      <p id="d1e523">The controller implemented onto T4 was designed by optimizing a FLORIS model
of the site based on wind direction and wind speed. This resulted in a
lookup table, which provides a desired yaw offset for T4 as a function of
wind speed and direction. Figure <xref ref-type="fig" rid="Ch1.F4"/> shows this target offset
function as a function of wind direction for several wind speeds. The
magenta lines indicate the approximate boundary of control and will be reused
in upcoming figures to distinguish controlled and uncontrolled wind
directions. The offset is largest around the peak wake loss direction near
134<inline-formula><mml:math id="M5" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> and decreases as the wind rotates southerly.</p>
      <?pagebreak page276?><p id="d1e537">These offset tables were constrained to be below the load impact limitations
determined by <xref ref-type="bibr" rid="bib1.bibx7" id="text.22"/>. A safe load envelope was
determined to be yaw offset angles no larger than 20<inline-formula><mml:math id="M6" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> during wind
speeds of 12 m s<inline-formula><mml:math id="M7" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> or less. Finally, offsets were restricted to
the counterclockwise direction with respect to the wind (when viewed from
above).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F4"><?xmltex \currentcnt{4}?><label>Figure 4</label><caption><p id="d1e566">Target offset for 8, 9, 10 and 11 m s<inline-formula><mml:math id="M8" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>. The red line
indicates the target offset by wind direction. The magenta vertical lines
indicate the approximate boundaries of the experiment (these vary slightly by
wind speed, but the overall shape is the same). </p></caption>
        <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019-f04.png"/>

      </fig>

      <p id="d1e588">The yaw controllers of the controlled turbines were then modified to
implement this yaw offset strategy. Specifically, the nacelle vane signal fed
into the controller was modified by the specified yaw offset amount in the
lookup table to induce the yaw controller to track an offset. An external
wake steering controller was implemented to determine the offset to apply at
a given moment. The specific setup is shown in Fig. <xref ref-type="fig" rid="Ch1.F5"/>.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F5" specific-use="star"><?xmltex \currentcnt{5}?><label>Figure 5</label><caption><p id="d1e595">Block diagram of wake steering controller implementation. Inputs are
provided by a typical turbine sensor, and the output is a modified vane
signal to supply the turbine yaw controller for wake steering. Note that this
output is toggled on–off hourly. All low-pass filters have a 30 s time
constant.</p></caption>
        <?xmltex \igopts{width=455.244094pt}?><graphic xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019-f05.png"/>

      </fig>

      <p id="d1e604">The controller in Fig. <xref ref-type="fig" rid="Ch1.F5"/> computes a wind speed and wind
direction from sensors available on each turbine. It then filters both of
these signals to remove high-frequency changes. The signals are fed into a
lookup table, which is also filtered, and then the modified offset vane
signal is sent to the turbine yaw controller.</p>
      <p id="d1e609">The offset function is toggled on and off every hour, as indicated in the
diagram. This toggling enables the performance of the wake steering
controller to be compared to a baseline control dataset that includes a
similar composition of wind speeds. The decision to toggle every hour was a
balance between accounting for the slowness of most yaw controllers and the
variation of wind conditions. The optimal toggling period should be studied
in more detail in the future to optimize the usefulness of the data
collected.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F6" specific-use="star"><?xmltex \currentcnt{6}?><label>Figure 6</label><caption><p id="d1e614">Total data collection. The yellow bars indicate the data from
unstable conditions, and the blue bars indicate the data from stable
conditions. The data were collected for both the baseline and controlled
cases.</p></caption>
        <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019-f06.png"/>

      </fig>

</sec>
<sec id="Ch1.S4">
  <label>4</label><title>Data collection</title>
      <p id="d1e632">The phase 1 campaign lasted for approximately 3 months, during which the wake
steering offset controller on T4 was toggled on and off hourly. This section
describes the inflow conditions during this period.</p>
      <p id="d1e635">The inflow conditions are described from the south sodar data. Wind speed and
wind direction are computed by a weighted average of the sodar measurements
at heights that are within the rotor area of the turbine similar to the
rotor-equivalent wind speed <xref ref-type="bibr" rid="bib1.bibx26" id="paren.23"/>. Turbulence intensity
(TI) is estimated at hub height by the sodar as the 10 min standard
deviation of the wind speed divided by the mean wind speed. Finally,
stability is quantified via the Obukhov lengths
<xref ref-type="bibr" rid="bib1.bibx23" id="paren.24"/>. For this case the Obukhov length <inline-formula><mml:math id="M9" display="inline"><mml:mi>L</mml:mi></mml:math></inline-formula> is computed
via
          <disp-formula id="Ch1.E1" content-type="numbered"><label>1</label><mml:math id="M10" display="block"><mml:mrow><mml:mi>L</mml:mi><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mo>-</mml:mo><mml:msubsup><mml:mi>u</mml:mi><mml:mo>∗</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:msubsup><mml:mover accent="true"><mml:mrow><mml:msub><mml:mi mathvariant="italic">θ</mml:mi><mml:mtext>v</mml:mtext></mml:msub></mml:mrow><mml:mo mathvariant="normal">‾</mml:mo></mml:mover></mml:mrow><mml:mrow><mml:mi>K</mml:mi><mml:mi>g</mml:mi><mml:mover accent="true"><mml:mrow><mml:msup><mml:mi>w</mml:mi><mml:mo>′</mml:mo></mml:msup><mml:msubsup><mml:mi mathvariant="italic">θ</mml:mi><mml:mtext>v</mml:mtext><mml:mo>′</mml:mo></mml:msubsup></mml:mrow><mml:mo mathvariant="normal">‾</mml:mo></mml:mover></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>

          <disp-formula id="Ch1.E2" content-type="numbered"><label>2</label><mml:math id="M11" display="block"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mo>∗</mml:mo></mml:msub><mml:mo>=</mml:mo><mml:mo>|</mml:mo><mml:msup><mml:mover accent="true"><mml:mrow><mml:msup><mml:mi>u</mml:mi><mml:mo>′</mml:mo></mml:msup><mml:msup><mml:mi>w</mml:mi><mml:mo>′</mml:mo></mml:msup></mml:mrow><mml:mo mathvariant="normal">‾</mml:mo></mml:mover><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mo>+</mml:mo><mml:msup><mml:mover accent="true"><mml:mrow><mml:msup><mml:mi>v</mml:mi><mml:mo>′</mml:mo></mml:msup><mml:msup><mml:mi>w</mml:mi><mml:mo>′</mml:mo></mml:msup></mml:mrow><mml:mo mathvariant="normal">‾</mml:mo></mml:mover><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:msup><mml:mo>|</mml:mo><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>/</mml:mo><mml:mn mathvariant="normal">4</mml:mn></mml:mrow></mml:msup><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
        where <inline-formula><mml:math id="M12" display="inline"><mml:mi>K</mml:mi></mml:math></inline-formula> is the von Kármán constant assumed to be 0.4, <inline-formula><mml:math id="M13" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mo>∗</mml:mo></mml:msub></mml:mrow></mml:math></inline-formula> is the
frictional velocity, <inline-formula><mml:math id="M14" display="inline"><mml:mi>g</mml:mi></mml:math></inline-formula> is gravity, <inline-formula><mml:math id="M15" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">θ</mml:mi><mml:mtext>v</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is virtual<?pagebreak page277?> potential
temperature calculated with the met tower pressure at 2.5 m, and <inline-formula><mml:math id="M16" display="inline"><mml:mi>u</mml:mi></mml:math></inline-formula>, <inline-formula><mml:math id="M17" display="inline"><mml:mi>v</mml:mi></mml:math></inline-formula>,
and <inline-formula><mml:math id="M18" display="inline"><mml:mi>w</mml:mi></mml:math></inline-formula> are meteorological coordinates of wind speed components in the
west–east, south–north, and vertical planes; the <inline-formula><mml:math id="M19" display="inline"><mml:msup><mml:mi/><mml:mo>′</mml:mo></mml:msup></mml:math></inline-formula> indicates
perturbations. Fluxes were calculated using a Reynolds decomposition based on
a 30 min average. Using the classification scheme of
<xref ref-type="bibr" rid="bib1.bibx27" id="text.25"/>, the data were divided into stable, neutral,
and unstable conditions. This division is simplified here so that “stable”
is defined as <inline-formula><mml:math id="M20" display="inline"><mml:mrow><mml:mi>L</mml:mi><mml:mo>&lt;</mml:mo><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1000</mml:mn></mml:mrow></mml:math></inline-formula> m and all other data are categorized as “not
stable.”<?xmltex \hack{\newpage}?></p>
      <p id="d1e854">The total amount of data collected is summarized in
Fig. <xref ref-type="fig" rid="Ch1.F6"/>. The amount of data collected between the
“baseline” set, i.e., controller off, and “controlled,” i.e., controller
on, is comparable. The data are broken into stable and unstable
atmospheric conditions to show that toggling ensures that both sets are similarly
composed of atmospheric conditions.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F7" specific-use="star"><?xmltex \currentcnt{7}?><label>Figure 7</label><caption><p id="d1e862">Atmospheric conditions observed by the sodar at hub height over the
duration of the test campaign. </p></caption>
        <?xmltex \igopts{width=426.791339pt}?><graphic xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019-f07.png"/>

      </fig>

      <p id="d1e871">Atmospheric conditions are described in Fig. <xref ref-type="fig" rid="Ch1.F7"/>. In
Fig. <xref ref-type="fig" rid="Ch1.F7"/>a, the wind directions observed over the course of
the campaign (as measured by the south sodar at hub height) are illustrated.
If data are restricted to points occurring in the range in which the
experimental controller is active (in terms of wind speed and direction) and
further limited by the removal of fault-coded data or faulty sensing, the data
are reduced to Fig. <xref ref-type="fig" rid="Ch1.F7"/>b. The distribution of wind speeds making
up Fig. <xref ref-type="fig" rid="Ch1.F7"/>b are then shown in Fig. <xref ref-type="fig" rid="Ch1.F7"/>c.
Finally, Fig. <xref ref-type="fig" rid="Ch1.F7"/>d illustrates the recorded TI within the
dataset remaining in Fig. <xref ref-type="fig" rid="Ch1.F7"/>b. The box sizes in
Fig. <xref ref-type="fig" rid="Ch1.F7"/>d indicate the amount of data, and the data are
subdivided into stable and unstable categories to show that lower wind
speeds are more likely to be higher-turbulence,<?pagebreak page278?> unstable conditions, whereas
higher wind speeds tend to be low-turbulence stable conditions. The black
line in Fig. <xref ref-type="fig" rid="Ch1.F7"/>d will be used to describe the typical TI
in the FLORIS model and will be discussed again later.</p>
</sec>
<sec id="Ch1.S5">
  <label>5</label><title>Controller assessment</title>
      <p id="d1e901">We first analyze the phase 1 data by considering the performance of the
controller in terms of its ability to produce a specific offset by wind speed
and wind direction. The exact function of the turbine yaw controller is not
known. Therefore, it was difficult to know in advance how effective the
method shown in Fig. <xref ref-type="fig" rid="Ch1.F5"/> would be in delivering the desired
offsets.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F8" specific-use="star"><?xmltex \currentcnt{8}?><label>Figure 8</label><caption><p id="d1e908">Comparison of observed yaw offset (green line) versus target (dashed
red line) segregated by wind speeds. Note that the achieved offset is computed as
the difference between the sodar-measured wind direction and the turbine
nacelle heading. Points indicate median offset, with box size indicating
the number of points in a bin and bands indicating the 95 % confidence interval of
the median.</p></caption>
        <?xmltex \igopts{width=398.338583pt}?><graphic xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019-f08.png"/>

      </fig>

      <p id="d1e917">Figure <xref ref-type="fig" rid="Ch1.F8"/> assesses the performance of this offset controller.
Binned by wind speed, the figure shows the median maintained offset. The
offset here is computed by comparing the nacelle position of T4 with the
measurement of wind direction recorded by the south sodar. Generally, the
offsets are achieved reasonably well; however, there is a tendency toward
undershoot. The undershoot could be an artifact of temporal averaging over
periods with and without offset, which biases computed offsets toward zero.
However, we suspect that the undershoot is actually occurring because of the
fact that the actual controller is tracking an offset that is zero for most
directions, except for a small band about the main waking direction. As the
wind speed and direction drift in and out of controlled areas, the averaging
effect biases the offset toward zero. This bias could be accounted for in
future controller design.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F9"><?xmltex \currentcnt{9}?><label>Figure 9</label><caption><p id="d1e925">Time series data of T4 operation showing the sources of lag in yaw
offset control. The figure shows that following the wind direction entering
the range at which a <inline-formula><mml:math id="M21" display="inline"><mml:mrow><mml:mn mathvariant="normal">20</mml:mn><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> offset would be optimal at the 2 min
mark, the offset is not actually achieved until 3 min later.</p></caption>
        <?xmltex \igopts{width=241.848425pt}?><graphic xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019-f09.png"/>

      </fig>

      <p id="d1e946">In addition to a steady bias toward smaller-than-targeted offsets, we also
noticed a dynamic issue in the controller design. The dynamic design of wind farm
controllers is a field of active research <xref ref-type="bibr" rid="bib1.bibx5" id="paren.26"/>.
In the initial design phase, it was assumed that, to avoid excessive yawing
behaviors, we should low-pass filter the wind speed and wind direction
inputs to the lookup table, as well as the resultant offset sent to the yaw
controller. We did not account for the fact that the yaw controller itself
acts as a lag filter between changes in wind direction and changes in nacelle
yaw position, so the yaw offset control system as a whole is probably too
slow and a general tendency toward overlagging changes in wind direction was
observed. This is illustrated in Fig. <xref ref-type="fig" rid="Ch1.F9"/>. At
approximately 2 min, the wind direction crosses into the region in which a
20<inline-formula><mml:math id="M22" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> offset would be dictated by the static optimal lookup table. The
low-pass filtering, however, causes the offset target to lag until the third
minute to reach 20<inline-formula><mml:math id="M23" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>. Then, the filtering of the offset achieves
20<inline-formula><mml:math id="M24" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> around the fourth minute. Further, the turbine is observed to
begin yawing around the fourth minute and completes this action in the<?pagebreak page279?> fifth
minute, 3 min after the offset could have been optimally applied. Some lag
is unavoidable and potentially desirable to avoid adding too much additional
yaw activity to the turbine, but based on this result, the controllers used
in the upcoming phase 2 will be designed dynamically and the filter
constants adjusted to account for this.</p>
</sec>
<sec id="Ch1.S6">
  <label>6</label><title>Challenges in this campaign</title>
      <p id="d1e989">This phase 1 campaign revealed several challenges that could inform future
campaigns, including our future phases. Despite these challenges, the wake
steering controller did produce the desired result of increasing power at the
downstream turbine.</p>
      <p id="d1e992">A first set of challenges corresponds to the site conditions for the south
campaign. The topography is complex, but the version of FLORIS used in the
design and analysis has no terrain-modeling capabilities. This mismatch
between the modeling assumptions and reality introduces a degree of uncertainty.
Second, T4 and T3 are spaced such that T3 is in the near-wake region of T4.
The version of FLORIS used does not contain a well-tuned near-wake model.
Finally, as shown in Fig. <xref ref-type="fig" rid="Ch1.F6"/>, the collected data are only
about one-third composed of stable atmospheric conditions because of the
summer season and longer days. Stable, low-turbulence conditions would be
more favorable to wake steering and may occur more frequently in the winter
season.</p>
      <p id="d1e997">A second set of challenges arises from more practical considerations.
Specifically, the only sensor that could be used for the south experiment to
measure the inflow is the south sodar, as it is the only one to the south of
T4. The south sodar, in comparison to other instruments, was shown to<?pagebreak page280?> measure
the inflow well; however, it delivers data only once every 10 min, and this
frequency is too coarse for the data analysis because 10 min will include a
diverse mix of wind directions and offsets. The turbine data are delivered at
a frequency of 1 Hz, and through trial and error, a compromise of
down-sampling the turbine data to 1 min periods while up-sampling the sodar
data was selected (this up-sampling is done through a “zero-order hold”,
wherein the data for each minute bin are assigned the 10 min average).
However, in the upcoming north campaign, more frequent data are available
from the lidar and can be used.</p>
      <p id="d1e1000">Finally, the controller design, wherein we influence the yaw controller
without fully understanding its behavior, is a major challenge. If the yaw
controller could be directly modified, the delays shown in
Fig. <xref ref-type="fig" rid="Ch1.F9"/> could be reduced and performance improved.</p>
</sec>
<sec id="Ch1.S7">
  <label>7</label><title>Results</title>
      <p id="d1e1013">The first step in performing the analysis was selecting a reference for
comparing the power of T3 and T4. In previous work, e.g.,
<xref ref-type="bibr" rid="bib1.bibx10" id="text.27"/>, a reference uncontrolled turbine was preferred as
it would provide a reference power that includes the effects not only of wind
speed, but also shear, veer, and TI. For this reason, both T1 and T5 were
considered, but a significant amount of noise and noncorrelation was
observed,
likely because both turbines are far downstream from T4. Ideally, the
reference would be parallel to the upstream turbine on a line perpendicular
to the controlled wind directions. In addition, the complex terrain varies
from T1 to T5.</p>
      <p id="d1e1019">For this reason, a synthetic reference turbine power was used based on the
measurements of the south sodar. The wind speeds at heights corresponding to
the turbine rotor were collected and applied to a weighted average, called
<inline-formula><mml:math id="M25" display="inline"><mml:mrow><mml:msub><mml:mi>U</mml:mi><mml:mtext>sodar</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>, wherein the weights were proportional to the sector of
rotor area the heights correspond with, similar to a rotor-effective wind
speed calculation <xref ref-type="bibr" rid="bib1.bibx26" id="paren.28"/>. The hypothetical power of a
reference turbine could then be computed using
          <disp-formula id="Ch1.E3" content-type="numbered"><label>3</label><mml:math id="M26" display="block"><mml:mrow><mml:msub><mml:mi>P</mml:mi><mml:mtext>sodar</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.5</mml:mn><mml:mi mathvariant="italic">ρ</mml:mi><mml:mi>A</mml:mi><mml:msub><mml:mi>C</mml:mi><mml:mtext>p</mml:mtext></mml:msub><mml:msubsup><mml:mi>U</mml:mi><mml:mtext>sodar</mml:mtext><mml:mn mathvariant="normal">3</mml:mn></mml:msubsup><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
        where <inline-formula><mml:math id="M27" display="inline"><mml:mrow><mml:msub><mml:mi>C</mml:mi><mml:mtext>p</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is derived from the <inline-formula><mml:math id="M28" display="inline"><mml:mrow><mml:msub><mml:mi>C</mml:mi><mml:mtext>p</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> lookup table included in
FLORIS, <inline-formula><mml:math id="M29" display="inline"><mml:mi mathvariant="italic">ρ</mml:mi></mml:math></inline-formula> is the average observed density, and <inline-formula><mml:math id="M30" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula> is the rotor area.
This estimated sodar power was then compared with the measured power of T4
when the turbine is not intentionally operating in the offset condition
(Fig. <xref ref-type="fig" rid="Ch1.F10"/>). The plot shows that correspondence is very close
except for near rated.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F10"><?xmltex \currentcnt{10}?><label>Figure 10</label><caption><p id="d1e1110">Sodar available power fit. The data from T4 are shown in black and
the sodar estimate is shown in red. The red boxes refer to the wind speed
bins and the size refers to the amount of data in each bin.</p></caption>
        <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019-f10.png"/>

      </fig>

      <p id="d1e1120">To analyze the effect of the wake steering implementation on the control and
downstream turbine, the following method of analysis is used. First, the data
are limited to include only periods in which both turbines were operating
normally and the quality of the sodar estimate was above a certain
threshold according to quality flags reported by the sodar at each range. Next, all
the data, including the power of T3 and the sodar reference power, are binned
into wind direction bins every 2<inline-formula><mml:math id="M31" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> (with 1<inline-formula><mml:math id="M32" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> of overlap between
adjacent bins as this was found useful in clarifying trends in the available
data) and according to whether the wake steering controller was toggled on
(controlled) or off (baseline).</p>
      <?pagebreak page281?><p id="d1e1141">Then for each bin, an energy ratio is computed, which involves a weighted
summation of all the power measurements <inline-formula><mml:math id="M33" display="inline"><mml:mrow><mml:msup><mml:mi>P</mml:mi><mml:mtext>Test</mml:mtext></mml:msup></mml:mrow></mml:math></inline-formula> of the test turbine
(the determination of the weights <inline-formula><mml:math id="M34" display="inline"><mml:mi>w</mml:mi></mml:math></inline-formula> will be detailed later), i.e., T3, and
the reference turbine, i.e., sodar estimate <inline-formula><mml:math id="M35" display="inline"><mml:mrow><mml:msup><mml:mi>P</mml:mi><mml:mtext>Ref</mml:mtext></mml:msup></mml:mrow></mml:math></inline-formula>, and then
a ratio of the two.
          <disp-formula id="Ch1.E4" content-type="numbered"><label>4</label><mml:math id="M36" display="block"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mtext>Energy</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msubsup><mml:mo>∑</mml:mo><mml:mrow><mml:mi>i</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow><mml:mi>N</mml:mi></mml:msubsup><mml:msub><mml:mi>w</mml:mi><mml:mi>i</mml:mi></mml:msub><mml:msubsup><mml:mi>P</mml:mi><mml:mi>i</mml:mi><mml:mtext>Test</mml:mtext></mml:msubsup></mml:mrow><mml:mrow><mml:msubsup><mml:mo>∑</mml:mo><mml:mrow><mml:mi>i</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow><mml:mi>N</mml:mi></mml:msubsup><mml:msub><mml:mi>w</mml:mi><mml:mi>i</mml:mi></mml:msub><mml:msubsup><mml:mi>P</mml:mi><mml:mi>i</mml:mi><mml:mtext>Ref</mml:mtext></mml:msubsup></mml:mrow></mml:mfrac></mml:mstyle></mml:mrow></mml:math></disp-formula></p>
      <p id="d1e1237">Note that this method is different from a power ratio method in which a power
ratio is computed for each set of points and then averaged.
          <disp-formula id="Ch1.E5" content-type="numbered"><label>5</label><mml:math id="M37" display="block"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mtext>Power</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mn mathvariant="normal">1</mml:mn><mml:mi>N</mml:mi></mml:mfrac></mml:mstyle><mml:munderover><mml:mo movablelimits="false">∑</mml:mo><mml:mrow><mml:mi>i</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow><mml:mi>N</mml:mi></mml:munderover><mml:mfenced close=")" open="("><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msubsup><mml:mi>P</mml:mi><mml:mi>i</mml:mi><mml:mtext>Test</mml:mtext></mml:msubsup></mml:mrow><mml:mrow><mml:msubsup><mml:mi>P</mml:mi><mml:mi>i</mml:mi><mml:mtext>Ref</mml:mtext></mml:msubsup></mml:mrow></mml:mfrac></mml:mstyle></mml:mfenced></mml:mrow></mml:math></disp-formula>
        It is also different from the slope method used in
<xref ref-type="bibr" rid="bib1.bibx10" id="text.29"/>.</p>
      <p id="d1e1293"><disp-formula id="Ch1.E6" content-type="numbered"><label>6</label><mml:math id="M38" display="block"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mtext>Slope</mml:mtext></mml:msub><mml:mo>:</mml:mo><mml:munder><mml:mo movablelimits="false">min⁡</mml:mo><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mtext>Slope</mml:mtext></mml:msub></mml:mrow></mml:munder><mml:mo>|</mml:mo><mml:mo>|</mml:mo><mml:msub><mml:mi mathvariant="bold-italic">P</mml:mi><mml:mtext>Test</mml:mtext></mml:msub><mml:mo>-</mml:mo><mml:msub><mml:mi>R</mml:mi><mml:mtext>Slope</mml:mtext></mml:msub><mml:msub><mml:mi mathvariant="bold-italic">P</mml:mi><mml:mtext>Ref</mml:mtext></mml:msub><mml:mo>|</mml:mo><mml:msub><mml:mo>|</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
        where <inline-formula><mml:math id="M39" display="inline"><mml:mrow><mml:msub><mml:mi>R</mml:mi><mml:mrow><mml:mo>[</mml:mo><mml:mi mathvariant="normal">…</mml:mi><mml:mo>]</mml:mo></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula> is the ratio computed through the different methods,
<inline-formula><mml:math id="M40" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="bold-italic">P</mml:mi><mml:mtext>Test</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M41" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="bold-italic">P</mml:mi><mml:mtext>Ref</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> are vectors of all observed
powers for the reference and test turbines, <inline-formula><mml:math id="M42" display="inline"><mml:mrow><mml:msubsup><mml:mi>P</mml:mi><mml:mi>i</mml:mi><mml:mtext>Ref</mml:mtext></mml:msubsup></mml:mrow></mml:math></inline-formula> is a
single-minute average, and <inline-formula><mml:math id="M43" display="inline"><mml:mi>N</mml:mi></mml:math></inline-formula> is the total number of points in a given wind
direction bin.</p>
      <p id="d1e1406">The energy ratio (Eq. <xref ref-type="disp-formula" rid="Ch1.E4"/>) is used for a few reasons. First,
changes in relative energy production are more directly related to changes in
revenue. Second, the power ratio is an average of ratios instead of the ratio
of averages proposed in the energy ratio (Eq. <xref ref-type="disp-formula" rid="Ch1.E5"/>). The power
ratio is more sensitive to small changes in power at low wind speeds that
do not contribute meaningfully to changes in energy production, which is the
ultimate goal. The slope method (Eq. <xref ref-type="disp-formula" rid="Ch1.E6"/>) of
<xref ref-type="bibr" rid="bib1.bibx10" id="text.30"/> was able to achieve a weighting of higher wind
speeds through slope fitting. However, the energy ratio was finally thought
to be more directly related to annual energy production, the overall quantity
of interest. The energy ratio represents the increase or decrease in energy
produced for a specific wind direction bin.</p>
      <p id="d1e1418">In computing the energy ratio, a wind-speed-based weighting strategy helps to
more quickly converge the analysis and reduce changes in energy ratios due to
variations in the compositions of wind speeds for the two controllers within
each wind direction bin with respect to differences due to changes in
controller. The main idea is that for each wind direction, the power values
collected are binned according to wind speed (as measured by the sodar) and
the total energy for the baseline and controlled cases is the weighted sum
of the powers; the weight is the number of points the other control
setting has in this wind speed bin out of the total. For example, if there
are 10 samples of baseline taken at 13 m s<inline-formula><mml:math id="M44" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> and 5 of controlled, the
baseline points are weighted by <inline-formula><mml:math id="M45" display="inline"><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>/</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:math></inline-formula> and the controlled by <inline-formula><mml:math id="M46" display="inline"><mml:mrow><mml:mn mathvariant="normal">2</mml:mn><mml:mo>/</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:math></inline-formula>, so the
final energy ratios to be compared are more approximately even in terms of
the wind speed distributions represented. If the bins are perfectly balanced,
there are an equivalent number of baseline and controlled points at each wind
speed, and the weights have no effect.</p>
      <p id="d1e1458">In addition to computing a single energy ratio for each bin, the process is
bootstrapped, whereby the data are randomly sampled with replacement and
the energy ratio recomputed 1000 times or more depending on the amount of
data. The results of these bootstrap iterations are then used to compute
95 % confidence intervals, and these are indicated in the plots of the energy
ratio as semi-transparent bands.</p>
      <p id="d1e1461">The method of computing energy ratios is now included within the open-source
FLORIS model (<uri>https://floris.readthedocs.io</uri>, last access: 1 May 2019).</p>
      <p id="d1e1467">Note that all wind speeds are used in this calculation, including those
(greater than 12 m s<inline-formula><mml:math id="M47" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>) in which the 0<inline-formula><mml:math id="M48" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> offset is actually
targeted, even in the controller on mode. With the 10 min sodar rate and
the lag of the controller, it is difficult to draw an exact line where the
controller stops impacting the individual turbine yaw controller. Including
all wind speeds also corresponds to the final change in energy.</p>
      <p id="d1e1491">The energy ratio calculation is repeated on several differently defined
FLORIS models of the site to provide a point of comparison. An “aligned”
case simulates every observed wind speed and direction in the baseline field
data with all turbines perfectly aligned to the flow, while a baseline
case uses the actual small offsets observed. An “optimal” case simulates
all the wind speeds and directions in the controlled field data using the
exact offset requested by the control strategy, while the controlled case applies
the actual achieved offset. These four settings are summarized in
Table <xref ref-type="table" rid="Ch1.T1"/>. For each of the FLORIS models and for each 1 min
wind speed and direction observed in the field, a matching FLORIS simulation
was run, the power of T3 and T4 tabulated, and the energy ratio computed.
When considering gains in energy, FLORIS optimal gain refers to the
change from aligned to optimal, whereas FLORIS controlled gain
refers to the change from baseline to controlled.</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T1" specific-use="star"><?xmltex \currentcnt{1}?><label>Table 1</label><caption><p id="d1e1499">FLORIS model definitions for comparison. The columns yaw 4 and yaw 3
determine what sets the yaw angle for each turbine (aligned is always 0<inline-formula><mml:math id="M49" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>), with
optimal being the true optimal; “from baseline” means applying
the observed yaw angles from the baseline data of the field campaign. Wind
conditions are similarly defined.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="4">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="left"/>
     <oasis:colspec colnum="3" colname="col3" align="left"/>
     <oasis:colspec colnum="4" colname="col4" align="left"/>
     <oasis:thead>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Model</oasis:entry>
         <oasis:entry colname="col2">Yaw 4</oasis:entry>
         <oasis:entry colname="col3">Yaw 3</oasis:entry>
         <oasis:entry colname="col4">Wind conditions</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>
         <oasis:entry colname="col1">Aligned</oasis:entry>
         <oasis:entry colname="col2">Aligned</oasis:entry>
         <oasis:entry colname="col3">Aligned</oasis:entry>
         <oasis:entry colname="col4">From baseline data</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Baseline</oasis:entry>
         <oasis:entry colname="col2">From baseline</oasis:entry>
         <oasis:entry colname="col3">From baseline</oasis:entry>
         <oasis:entry colname="col4">From baseline data</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Optimal</oasis:entry>
         <oasis:entry colname="col2">Optimal</oasis:entry>
         <oasis:entry colname="col3">Aligned</oasis:entry>
         <oasis:entry colname="col4">From controlled data</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Controlled</oasis:entry>
         <oasis:entry colname="col2">From controlled</oasis:entry>
         <oasis:entry colname="col3">From controlled</oasis:entry>
         <oasis:entry colname="col4">From controlled data</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table></table-wrap>

      <p id="d1e1607">The energy ratios can be computed from these FLORIS models. The comparison of
the aligned and optimal case should present an upper bound on performance if
exact offsets and alignments held, whereas the baseline and controlled cases
show what we expect from this dataset.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F11"><?xmltex \currentcnt{11}?><label>Figure 11</label><caption><p id="d1e1612">Energy ratio for T3 for field data and the baseline and controlled
FLORIS cases (see Table <xref ref-type="table" rid="Ch1.T1"/>). An energy ratio of 0.5 corresponds
to a production of 50 % of the total expected based on the measured
inflow without considering wakes. The vertical magenta lines indicate the
region where control is applied and a difference between the baseline and
controlled is expected. The size of the circles at each point indicates the number of
points in the bin, while the bands indicate 95 % confidence as computed
by bootstrapping. </p></caption>
        <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019-f11.png"/>

      </fig>

<sec id="Ch1.S7.SS1">
  <label>7.1</label><title>Turbine 3 analysis</title>
      <p id="d1e1630">Figure <xref ref-type="fig" rid="Ch1.F11"/> shows the energy ratios by wind direction for T3. The
wake loss is deeper than FLORIS expects (T3 is producing less than 40 %
of the energy of the reference at nadir); however, as mentioned, this is a
difficulty of current near-wake models and the subject of active research.
Still, the gain in energy production in the wind direction for which the
controller is active is observed. Note that as described earlier, to clarify
trends, the wind direction bins are every 2<inline-formula><mml:math id="M50" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> but are 3<inline-formula><mml:math id="M51" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> wide
(overlapping with adjacent) to increase the number of points available per bin.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F12"><?xmltex \currentcnt{12}?><label>Figure 12</label><caption><p id="d1e1655">Change in the energy ratio of T3 from field data. Expectations from
FLORIS using the actually achieved controlled offsets
(controlled <inline-formula><mml:math id="M52" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula> baseline) and optimal (optimal <inline-formula><mml:math id="M53" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula> aligned) are shown to
indicate comparison with expectations given control values and what is
optimally expected.</p></caption>
          <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019-f12.png"/>

        </fig>

      <?pagebreak page282?><p id="d1e1678">The difference between the baseline and controlled cases for both the field
data and FLORIS quantifies the impact of yaw control on power production
(Fig. <xref ref-type="fig" rid="Ch1.F12"/>). In the 10<inline-formula><mml:math id="M54" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> sector between 140 and
150<inline-formula><mml:math id="M55" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> the average gain in energy is 14.6 %. Compared to FLORIS
predictions, the field results compare favorably to the estimations from
FLORIS. The data outside of the control bands, while noisy, indicate an
average around 0, underlining the significance of the nonzero apparent
average in the control region.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F13" specific-use="star"><?xmltex \currentcnt{13}?><label>Figure 13</label><caption><p id="d1e1704">Energy ratio of T3, as in Fig. <xref ref-type="fig" rid="Ch1.F11"/>, divided into stable
and unstable conditions.</p></caption>
          <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019-f13.png"/>

        </fig>

      <p id="d1e1715">Figure <xref ref-type="fig" rid="Ch1.F13"/> segregates stable conditions from
unstable conditions and repeats the analysis of Figs. <xref ref-type="fig" rid="Ch1.F11"/>
and <xref ref-type="fig" rid="Ch1.F12"/>. The gain in stable conditions is more
consistently realized (as indicated by the bands) and the peak gain is
higher than in unstable conditions. This distinct improvement in stable
conditions could be because wake steering is more effective in stable
conditions. Additionally, in stable conditions, atmospheric inflow is more
homogeneous and therefore easier to measure. Upcoming winter measurements
from the north for phase 2 will consist of more stable measurements due to
the longer nights and may shed more light on the role of atmospheric
stability in wake steering.<?xmltex \hack{\newpage}?></p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F14"><?xmltex \currentcnt{14}?><label>Figure 14</label><caption><p id="d1e1727">Energy ratio of the summed energy of T3 and T4.</p></caption>
          <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019-f14.png"/>

        </fig>

</sec>
<sec id="Ch1.S7.SS2">
  <label>7.2</label><title>Aggregate analysis</title>
      <p id="d1e1744">Finally, the previously mentioned analysis is repeated, but using the
aggregated power of T4 and T3, so that the losses in energy coming from
offsetting the yaw of T4 are deducted from the gains made downstream
(Fig. <xref ref-type="fig" rid="Ch1.F14"/> shows the energy ratios and
Fig. <xref ref-type="fig" rid="Ch1.F15"/> shows the difference between them). The
aggregated energy gains appear to be somewhat more than the current version
of FLORIS expects (a net gain of 4.1 % over the same 10<inline-formula><mml:math id="M56" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> region
from 140 to 150<inline-formula><mml:math id="M57" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>), but this could again be connected to difficulty
measuring the near wake.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F15"><?xmltex \currentcnt{15}?><label>Figure 15</label><caption><p id="d1e1771">Combined change in energy ratio for T3 and T4.</p></caption>
          <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://wes.copernicus.org/articles/4/273/2019/wes-4-273-2019-f15.png"/>

        </fig>

</sec>
</sec>
<sec id="Ch1.S8" sec-type="conclusions">
  <label>8</label><title>Conclusions</title>
      <p id="d1e1789">We present the initial results from the first phase of a field campaign
evaluating wake steering at a commercial wind farm. For two closely spaced
turbines, an approximate 14 % increase in energy was measured on the
downstream turbine over a 10<inline-formula><mml:math id="M58" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula> sector with a 4 % increase in energy
when accounting for losses of the upstream turbine. The gains in energy were
compared to predictions made using the FLORIS<?pagebreak page283?> model used to design the
applied controllers. The overall gains were consistent with predictions from
FLORIS.</p>
      <p id="d1e1801">This initial stage of the wake steering campaign identified several areas for
improvement in future work, such as aspects of dynamic controller design,
time filtering, and uncertainty quantification. Difficulties with this
particular south campaign, including complex terrain and summer atmospheric
conditions, were identified as possible sources of improvement as the
campaign moves to northern winter conditions. Additionally, near-wake
modeling presented a challenge in accurately modeling the wake losses and
therefore may have realized a less-than-optimal controller. Still, the
overall gains in energy were in line with prior expectations from FLORIS.</p>
      <p id="d1e1804">All together, the authors hope that the results presented might therefore
represent a baseline for the possibility of gains from wake steering. Better
modeling and controls, simpler site conditions, and the exploitation of
vortex modeling and larger arrays of turbines all present hopeful avenues for
continued improvements. An upcoming companion paper on the second phase of
the experiment will review results,<?pagebreak page284?> including the opportunities for improvement
identified in this paper.</p>
</sec>

      
      </body>
    <back><notes notes-type="dataavailability"><title>Data availability</title>

      <p id="d1e1811">Currently, the data are not publicly available; however, if
in the future portions of the data become available, this would be through the DOE A2e data portal
at <uri>https://a2e.energy.gov/about/dap</uri>.</p>
  </notes><notes notes-type="authorcontribution"><title>Author contributions</title>

      <p id="d1e1821">All coauthors were involved in writing and editing the paper.
The design of the controller and analysis of data were performed by PF,
JK, KD, ES, PM, JKL, KF, CB, RM, and PM. The implementation of experiments at
the site was done by JR, AS, JvD, HL, JS, MS, BR, CG, and
DB.</p>
  </notes><notes notes-type="competinginterests"><title>Competing interests</title>

      <p id="d1e1827">The authors declare that they have no conflict of
interest.</p>
  </notes><notes notes-type="disclaimer"><title>Disclaimer</title>

      <p id="d1e1833">The views expressed in the article do not necessarily represent
the views of the DOE or the U.S. Government.</p>
  </notes><notes notes-type="financialsupport"><title>Financial support</title>

      <p id="d1e1839">Funding provided by the U.S. Department of Energy Office of
Energy Efficiency and Renewable Energy Wind Energy Technologies Office.</p>
  </notes><notes notes-type="reviewstatement"><title>Review statement</title>

      <p id="d1e1845">This paper was edited by Sandrine Aubrun and reviewed by two
anonymous referees.</p>
  </notes><ref-list>
    <title>References</title>

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S., Hamidi, A., Iungo, G. V., Kaushik, A., Kosović, B., Langan, P., Lass,
A., Lavin, E., Lee, J. C.-Y., McCaffrey, K. L., Newsom, R. K., Noone, D. C.,
Oncley, S. P., Quelet, P. T., Sandberg, S. P., Schroeder, J. L., Shaw, W. J.,
Sparling, L., Martin, C. S., Pe, A. S., Strobach, E., Tay, K., Vanderwende,
B. J., Weickmann, A., Wolfe, D., and Worsnop, R.: Assessing State-of-the-Art
Capabilities for Probing the Atmospheric Boundary Layer: The XPIA Field
Campaign, B. Am. Meteorol. Soc., 98, 289–314,
<ext-link xlink:href="https://doi.org/10.1175/BAMS-D-15-00151.1" ext-link-type="DOI">10.1175/BAMS-D-15-00151.1</ext-link>, 2017.</mixed-citation></ref>
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Medici, D. and Alfredsson, P.: Measurements on a wind turbine wake: 3D
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behind yawed wind turbine models, J. Phys. Conf. Ser., 854, 012032,
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    <!--<article-title-html>Initial results from a field campaign of wake steering applied at a commercial wind farm – Part 1</article-title-html>
<abstract-html><p>Wake steering is a form of wind farm control in which turbines use
yaw offsets to affect wakes in order to yield an increase in total energy
production. In this first phase of a study of wake steering at a commercial
wind farm, two turbines implement a schedule of offsets. Results exploring
the observed performance of wake steering are presented and some
first lessons learned. For two closely spaced turbines, an approximate
14&thinsp;% increase in energy was measured on the downstream turbine over a
10° sector, with a 4&thinsp;% increase in energy production of the
combined upstream–downstream turbine pair. Finally, the influence of
atmospheric stability over the results is explored.</p></abstract-html>
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Howland, M. F., Bossuyt, J., Martinez-Tossas, L. A., Meyers, J., and
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under uniform inflow conditions, J. Renew. Sustain. Energ., 8, 043301,
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Lundquist, J. K., Wilczak, J. M., Ashton, R., Bianco, L., Brewer, W. A.,
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S., Hamidi, A., Iungo, G. V., Kaushik, A., Kosović, B., Langan, P., Lass,
A., Lavin, E., Lee, J. C.-Y., McCaffrey, K. L., Newsom, R. K., Noone, D. C.,
Oncley, S. P., Quelet, P. T., Sandberg, S. P., Schroeder, J. L., Shaw, W. J.,
Sparling, L., Martin, C. S., Pe, A. S., Strobach, E., Tay, K., Vanderwende,
B. J., Weickmann, A., Wolfe, D., and Worsnop, R.: Assessing State-of-the-Art
Capabilities for Probing the Atmospheric Boundary Layer: The XPIA Field
Campaign, B. Am. Meteorol. Soc., 98, 289–314,
<a href="https://doi.org/10.1175/BAMS-D-15-00151.1" target="_blank">https://doi.org/10.1175/BAMS-D-15-00151.1</a>, 2017.
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Martínez-Tossas, L. A., Annoni, J., Fleming, P. A., and Churchfield, M.
J.: The aerodynamics of the curled wake: a simplified model in view of flow
control, Wind Energ. Sci., 4, 127–138,
<a href="https://doi.org/10.5194/wes-4-127-2019" target="_blank">https://doi.org/10.5194/wes-4-127-2019</a>, 2019.
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Medici, D. and Alfredsson, P.: Measurements on a wind turbine wake: 3D
effects and bluff body vortex shedding, Wind Energy, 9, 219–236, 2006.
</mixed-citation></ref-html>
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Niayifar, A. and Porté-Agel, F.: A new analytical model for wind farm
power prediction, J. Phys. Conf. Ser., 625, 012039,
<a href="https://doi.org/10.1088/1742-6596/625/1/012039" target="_blank">https://doi.org/10.1088/1742-6596/625/1/012039</a>, 2015.
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NREL: FLORIS, Version 1.0.0, available at:
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Park, J., Kwon, S.-D., and Law, K. H.: A data-driven approach for cooperative
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Stull, R. B.: An introduction to boundary layer meteorology, vol. 13,
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Vollmer, L., Steinfeld, G., Heinemann, D., and Kühn, M.: Estimating the
wake deflection downstream of a wind turbine in different atmospheric
stabilities: an LES study, Wind Energ. Sci., 1, 129–141,
<a href="https://doi.org/10.5194/wes-1-129-2016" target="_blank">https://doi.org/10.5194/wes-1-129-2016</a>, 2016.
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Wagenaar, J., Machielse, L., and Schepers, J.: Controlling wind in ECN's
scaled wind farm, Proc. Europe Premier Wind Energy Event, Copenhage, Denmark,
16–19 April 2012, ECN, 685–694, 2012.

</mixed-citation></ref-html>
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Wagner, R., Cañadillas, B., Clifton, A., Feeney, S., Nygaard, N., Poodt,
M., St Martin, C., Tüxen, E., and Wagenaar, J.: Rotor equivalent wind
speed for power curve measurement–comparative exercise for IEA Wind Annex
32, J. Phys. Conf. Ser., 524, 012108, <a href="https://doi.org/10.1088/1742-6596/524/1/012108" target="_blank">https://doi.org/10.1088/1742-6596/524/1/012108</a>,
2014.
</mixed-citation></ref-html>
<ref-html id="bib1.bib27"><label>Wharton and Lundquist(2012)</label><mixed-citation>
Wharton, S. and Lundquist, J. K.: Atmospheric stability affects wind turbine
power collection, Environ. Res. Lett., 7, 014005,
<a href="https://doi.org/10.1088/1748-9326/7/1/014005" target="_blank">https://doi.org/10.1088/1748-9326/7/1/014005</a>, 2012.
</mixed-citation></ref-html>
<ref-html id="bib1.bib28"><label>White et al.(2018)</label><mixed-citation>
White, J., Ennis, B., and Herges, T. G.: Estimation of Rotor Loads Due to
Wake Steering, in: 2018 Wind Energy Symposium, Kissimmee, Florida, 8–12
January 2018, <a href="https://doi.org/10.2514/6.2018-1730" target="_blank">https://doi.org/10.2514/6.2018-1730</a>, 2018.
</mixed-citation></ref-html>--></article>
