Articles | Volume 14, issue 10
Geosci. Model Dev., 14, 6177–6195, 2021
https://doi.org/10.5194/gmd-14-6177-2021
Geosci. Model Dev., 14, 6177–6195, 2021
https://doi.org/10.5194/gmd-14-6177-2021

Model description paper 15 Oct 2021

Model description paper | 15 Oct 2021

S2P3-R v2.0: computationally efficient modelling of shelf seas on regional to global scales

Paul R. Halloran et al.

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Cited articles

Amante, C. and Eakins, B. W.: ETOPO1 1 Arc-Minute Global Relief Model: Procedures, Data Sources and Analysis, NOAA Tech. Memo., NESDIS NGDC-24, https://doi.org/10.1594/PANGAEA.769615, 2009. 
Australian Institute of Marine Science (AIMS): NRSYON: Northern Australia Automated Marine Weather and Oceanographic Stations, Sites: [Yongala], https://doi.org/10.25845/5c09bf93f315d, 2020. 
Bahamondes Dominguez, A. A., Hickman, A. E., Marsh, R., and Moore, C. M.: Constraining the response of phytoplankton to zooplankton grazing and photo-acclimation in a temperate shelf sea with a 1-D model – towards S2P3 v8.0, Geosci. Model Dev., 13, 4019–4040, https://doi.org/10.5194/gmd-13-4019-2020, 2020. 
Barnes, M. K., Tilstone, G. H., Suggett, D. J., Widdicombe, C. E., Bruun, J., Martinez-Vicente, V., and Smyth, T. J.: Temporal variability in total, micro- and nano-phytoplankton primary production at a coastal site in the Western English Channel, Prog. Oceanogr., 137 (Part B), 470–483​​​​​​​, https://doi.org/10.1016/j.pocean.2015.04.017, 2015. 
Beaman, R.: Project 3DGBR: a high-resolution depth model for the Great Barrier Reef and Coral Sea, MTSRF Final Report Project 2.5i.1a, Reef and Rainforest Research Centre MTSRF Final Report Marine and Tropical Sciences Research Facility, James Cook University, available at: https://www.deepreef.org/images/stories/publications/reports/Project3DGBRFinal_RRRC2010.pdf (last access: 1 July 2021), ​​​​​​​2010. 
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This paper describes the latest version of a simple model for simulating coastal oceanography in response to changes in weather and climate. The latest revision of this model makes scientific improvements but focuses on improvements that allow the model to be run simply at large scales and for long periods of time to explore the implications of (for example) future climate change along large areas of coastline.