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<result><vid>129884</vid><uid>453</uid><title>Renewable energy impact assessment</title><log>Edited by HilaryA.</log><status>1</status><comment>0</comment><promote>0</promote><sticky>0</sticky><ds_switch></ds_switch><nid>21466</nid><type>generic_information_page</type><language>und</language><created>1628775028</created><changed>1633357856</changed><tnid>0</tnid><translate>0</translate><revision_timestamp>1633357856</revision_timestamp><revision_uid>58</revision_uid><field_description><und is_array="true"><item><value>&lt;p&gt;Tidal and wave energy devices remove energy from the tidal current and wave fields, respectively, and this disturbance may alter the hydrodynamics, both near- and far-field. Offshore wind structures are obstructions to the flow and any change in the near sea surface wind field could also change the low flow fields and water column structure. Any significant disturbance to the hydrodynamics within a region may alter the levels of mixing and could have an effect on the local density structure, including the levels of stratification, potentially affecting the whole ecosystem. Numerical hydrodynamic models, such as the Scottish Shelf Model (SSM), are the best tools we have to assess the potential impacts of new large developments before they are implemented.&lt;/p&gt;&#13;
</value><format>full_html</format><safe_value>&lt;p&gt;Tidal and wave energy devices remove energy from the tidal current and wave fields, respectively, and this disturbance may alter the hydrodynamics, both near- and far-field. Offshore wind structures are obstructions to the flow and any change in the near sea surface wind field could also change the low flow fields and water column structure. Any significant disturbance to the hydrodynamics within a region may alter the levels of mixing and could have an effect on the local density structure, including the levels of stratification, potentially affecting the whole ecosystem. Numerical hydrodynamic models, such as the Scottish Shelf Model (SSM), are the best tools we have to assess the potential impacts of new large developments before they are implemented.&lt;/p&gt;
</safe_value></item></und></field_description><field_infomration_images><und is_array="true"><item><fid>188648</fid><uid>453</uid><filename>PFOW tidal amplitude change</filename><uri>public://pfow_tidal_amplitude_change.png</uri><filemime>image/png</filemime><filesize>207824</filesize><status>1</status><timestamp>1628784669</timestamp><type>image</type><field_tags><und is_array="true"><item><tid>772</tid></item><item><tid>887</tid></item><item><tid>2084</tid></item><item><tid>1449</tid></item></und></field_tags><field_file_image_alt_text><und is_array="true"><item><value>Predicted change in semi-diurnal tidal amplitude around Orkney due to 1.4 GW tidal stream energy extraction</value><format/><safe_value>Predicted change in semi-diurnal tidal amplitude around Orkney due to 1.4 GW tidal stream energy extraction</safe_value></item></und></field_file_image_alt_text><field_file_image_title_text><und is_array="true"><item><value>Predicted changes from the PFOW to semi-diurnal tidal amplitude resulting from two tidal stream turbine layouts which both extract a mean power of 1.4 GW (adapted from O'Hara Murray and Gallego, 2017).</value><format/><safe_value>Predicted changes from the PFOW to semi-diurnal tidal amplitude resulting from two tidal stream turbine layouts which both extract a mean power of 1.4 GW (adapted from O&amp;#039;Hara Murray and Gallego, 2017).</safe_value></item></und></field_file_image_title_text><_drafty_revision_requested>FIELD_LOAD_CURRENT</_drafty_revision_requested><rdf_mapping/><title>Predicted changes from the PFOW to semi-diurnal tidal amplitude resulting from two tidal stream turbine layouts which both extract a mean power of 1.4 GW (adapted from O'Hara Murray and Gallego, 2017).</title><alt>Predicted change in semi-diurnal tidal amplitude around Orkney due to 1.4 GW tidal stream energy extraction</alt><metadata><height>531</height><width>800</width></metadata><height>531</height><width>800</width></item></und></field_infomration_images><field_infomration_data_link/><field_information_map_link/><field_theme><und is_array="true"><item><tid>1964</tid></item></und></field_theme><field_google_plus_gallery/><field_tags/><field_footer_text><und is_array="true"><item><value>&lt;p&gt;The SSM has been used for a number of studies of the potential impact of large tidal stream arrays around Scotland. O'Hara Murray and Gallego (2017) used the Pentland Firth and Orkney Waters (PFOW) sub-model to examine how large tidal stream developments in the Pentland Firth could impact tidal processes in the region. It was found that smaller developments, totalling around 1 GW mean extracted power, are unlikely to lead to significant changes in the physical marine environment, whereas larger developments, &amp;gt; 1.5 GW mean extracted power, could significantly change the flow. This work also highlighted that thought needs to be put into where large tidal stream developments take place, in order to maximise the power outputs as well as minimise the environmental consequences. This was further discussed in a paper by Waldman et al. (2019) on the future policy implications of tidal energy array interactions. The wider SSM has been used for extensive studies of the impact of potential large tidal stream arrays around Scotland on physical processes, including stratification (De Dominicis et al., 2017) for present day and future climate change scenarios (De Dominicis et al., 2018).&lt;/p&gt;&#13;
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&lt;h3&gt;References&lt;/h3&gt;&#13;
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&lt;p&gt;De Dominicis, M., O’Hara Murray, R., &amp;amp; Wolf, J. (2017). Multi-scale ocean response to a large tidal stream turbine. Renewable Energy, 114, 1160–1179. &lt;a href="https://doi.org/10.1016/j.renene.2017.07.058"&gt;https://doi.org/10.1016/j.renene.2017.07.058&lt;/a&gt;&lt;/p&gt;&#13;
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&lt;p&gt;De Dominicis, M., Wolf, J., &amp;amp; O’Hara Murray, R. (2018). Comparative Effects of Climate Change and Tidal Stream Energy Extraction in a Shelf Sea. Journal of Geophysical Research: Oceans, 123(7), 5041–5067. &lt;a href="https://doi.org/10.1029/2018JC013832"&gt;https://doi.org/10.1029/2018JC013832&lt;/a&gt;&lt;/p&gt;&#13;
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&lt;p&gt;O’Hara Murray, R. B., &amp;amp; Gallego, A. (2017). A modelling study of the tidal stream resource of the Pentland Firth, Scotland. Renewable Energy, 102(B), 326–340. &lt;a href="https://doi.org/10.1016/j.renene.2016.10.053"&gt;https://doi.org/10.1016/j.renene.2016.10.053&lt;/a&gt;&lt;/p&gt;&#13;
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&lt;p&gt;Waldman, S., Weir, S., O’Hara Murray, R. B., Woolf, D. K., &amp;amp; Kerr, S. (2019). Future policy implications of tidal energy array interactions. Marine Policy, 108, 103611. &lt;a href="https://doi.org/10.1029/2018JC013832"&gt;https://doi.org/10.1016/J.MARPOL.2019.103611&lt;/a&gt;&lt;/p&gt;&#13;
</value><format>full_html</format><safe_value>&lt;p&gt;The SSM has been used for a number of studies of the potential impact of large tidal stream arrays around Scotland. O'Hara Murray and Gallego (2017) used the Pentland Firth and Orkney Waters (PFOW) sub-model to examine how large tidal stream developments in the Pentland Firth could impact tidal processes in the region. It was found that smaller developments, totalling around 1 GW mean extracted power, are unlikely to lead to significant changes in the physical marine environment, whereas larger developments, &amp;gt; 1.5 GW mean extracted power, could significantly change the flow. This work also highlighted that thought needs to be put into where large tidal stream developments take place, in order to maximise the power outputs as well as minimise the environmental consequences. This was further discussed in a paper by Waldman et al. (2019) on the future policy implications of tidal energy array interactions. The wider SSM has been used for extensive studies of the impact of potential large tidal stream arrays around Scotland on physical processes, including stratification (De Dominicis et al., 2017) for present day and future climate change scenarios (De Dominicis et al., 2018).&lt;/p&gt;
&lt;h3&gt;References&lt;/h3&gt;
&lt;p&gt;De Dominicis, M., O’Hara Murray, R., &amp;amp; Wolf, J. (2017). Multi-scale ocean response to a large tidal stream turbine. Renewable Energy, 114, 1160–1179. &lt;a href="https://doi.org/10.1016/j.renene.2017.07.058"&gt;https://doi.org/10.1016/j.renene.2017.07.058&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;De Dominicis, M., Wolf, J., &amp;amp; O’Hara Murray, R. (2018). Comparative Effects of Climate Change and Tidal Stream Energy Extraction in a Shelf Sea. Journal of Geophysical Research: Oceans, 123(7), 5041–5067. &lt;a href="https://doi.org/10.1029/2018JC013832"&gt;https://doi.org/10.1029/2018JC013832&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;O’Hara Murray, R. B., &amp;amp; Gallego, A. (2017). A modelling study of the tidal stream resource of the Pentland Firth, Scotland. Renewable Energy, 102(B), 326–340. &lt;a href="https://doi.org/10.1016/j.renene.2016.10.053"&gt;https://doi.org/10.1016/j.renene.2016.10.053&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;Waldman, S., Weir, S., O’Hara Murray, R. B., Woolf, D. K., &amp;amp; Kerr, S. (2019). Future policy implications of tidal energy array interactions. Marine Policy, 108, 103611. &lt;a href="https://doi.org/10.1029/2018JC013832"&gt;https://doi.org/10.1016/J.MARPOL.2019.103611&lt;/a&gt;&lt;/p&gt;
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