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Fig 3. Comparison between the observed and modelled along-shelf currents: Ocean Transport Pathways to a World Heritage Fringing Coral Reef: Ningaloo Reef, Western Australia

The University of Western Australia
Xu, Jiangtao ; Lowe, Ryan ; Ivey, Gregory ; Jones, Nicole ; Zhang, Zhenlin
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ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=info:doi10.1371/journal.pone.0145822.g003&rft.title=Fig 3. Comparison between the observed and modelled along-shelf currents: Ocean Transport Pathways to a World Heritage Fringing Coral Reef: Ningaloo Reef, Western Australia&rft.identifier=10.1371/journal.pone.0145822.g003&rft.publisher=Public Library of Science (PLoS)&rft.description=(a) Low-pass filtered along-shelf component of the wind stress (positive towards the northwest) over the year-long study period. (b) Comparison between the observed and modeled low-pass filtered along-shelf currents during the summer period, averaged over depths between 20–30 m. (c) Comparison of the observed and modeled low-pass filtered along-shelf currents during the spring period. The low-pass filter has a half-power period of 38 h to remove inertial oscillations, and in the case of the field data, the tides [30]. Note that the model results based on Xu et al. [18] do not include tides.&rft.creator=Xu, Jiangtao &rft.creator=Lowe, Ryan &rft.creator=Ivey, Gregory &rft.creator=Jones, Nicole &rft.creator=Zhang, Zhenlin &rft.date=2016&rft.relation=http://research-repository.uwa.edu.au/en/publications/57a30c2c-a2a5-4712-bb43-81e2da475dd6&rft.type=dataset&rft.language=English Access the data
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(a) Low-pass filtered along-shelf component of the wind stress (positive towards the northwest) over the year-long study period. (b) Comparison between the observed and modeled low-pass filtered along-shelf currents during the summer period, averaged over depths between 20–30 m. (c) Comparison of the observed and modeled low-pass filtered along-shelf currents during the spring period. The low-pass filter has a half-power period of 38 h to remove inertial oscillations, and in the case of the field data, the tides [30]. Note that the model results based on Xu et al. [18] do not include tides.

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Jiangtao Xu (Creator); Zhenlin Zhang (Creator)

Issued: 2016

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