Callaghan, David P; Leon, Javier X; Saunders, Megan I (2015): Results of wave modelling for Moreton Bay, Southeast Queensland, and a reef lagoon off Lizard Island, Great Barrier Reef, Australia. PANGAEA, https://doi.org/10.1594/PANGAEA.841223, Supplement to: Callaghan, DP et al. (2015): Wave modelling as a proxy for seagrass ecological modelling: Comparing fetch and process-based predictions for a bay and reef lagoon. Estuarine, Coastal and Shelf Science, 153, 108-120, https://doi.org/10.1016/j.ecss.2014.12.016
Always quote citation above when using data! You can download the citation in several formats below.
The distribution, abundance, behaviour, and morphology of marine species is affected by spatial variability in the wave environment. Maps of wave metrics (e.g. significant wave height Hs, peak energy wave period Tp, and benthic wave orbital velocity URMS) are therefore useful for predictive ecological models of marine species and ecosystems. A number of techniques are available to generate maps of wave metrics, with varying levels of complexity in terms of input data requirements, operator knowledge, and computation time. Relatively simple "fetch-based" models are generated using geographic information system (GIS) layers of bathymetry and dominant wind speed and direction. More complex, but computationally expensive, "process-based" models are generated using numerical models such as the Simulating Waves Nearshore (SWAN) model. We generated maps of wave metrics based on both fetch-based and process-based models and asked whether predictive performance in models of benthic marine habitats differed. Predictive models of seagrass distribution for Moreton Bay, Southeast Queensland, and Lizard Island, Great Barrier Reef, Australia, were generated using maps based on each type of wave model. For Lizard Island, performance of the process-based wave maps was significantly better for describing the presence of seagrass, based on Hs, Tp, and URMS. Conversely, for the predictive model of seagrass in Moreton Bay, based on benthic light availability and Hs, there was no difference in performance using the maps of the different wave metrics. For predictive models where wave metrics are the dominant factor determining ecological processes it is recommended that process-based models be used. Our results suggest that for models where wave metrics provide secondarily useful information, either fetch- or process-based models may be equally useful.
Median Latitude: -21.016950 * Median Longitude: 149.384700 * South-bound Latitude: -27.365000 * West-bound Longitude: 145.459400 * North-bound Latitude: -14.668900 * East-bound Longitude: 153.310000
Datasets listed in this publication series
- Callaghan, DP; Leon, JX; Saunders, MI (2015): Wind and ocean swell wave model (SWAN) results for coastal waters of Lizard Island, Queensland, Australia. https://doi.org/10.1594/PANGAEA.841221
- Callaghan, DP; Leon, JX; Saunders, MI (2015): Wind and ocean swell wave model (SWAN) results for coastal waters of Moreton Bay, Queensland, Australia. https://doi.org/10.1594/PANGAEA.841222