1Coastal and Regional Oceanography Lab, School of Mathematics and Statistics,
University of New South Wales, Sydney NSW, Australia
2CSIRO Oceans and Atmosphere, Hobart, Tasmania, Australia
3Sydney Institute of Marine Science, Mosman, NSW 2088, Australia
Received: 29 Oct 2015 – Discussion started: 15 Dec 2015
Abstract. In contrast to physical processes, biogeochemical processes are inherently patchy in the ocean, which affects both the observational sampling strategy and the representativeness of sparse measurements in data assimilating models. In situ observations from multiple glider deployments are analysed to characterize spatial scales of variability in both physical and biogeochemical properties, using an empirical statistical model. We find that decorrelation ranges are strongly dependent on the balance between local dynamics and mesoscale forcing. The shortest horizontal (5–10 km) and vertical (45 m) decorrelation ranges are for chlorophyll a fluorescence, whereas those variables that are a function of regional ocean and atmosphere dynamics (temperature and dissolved oxygen) result in anisotropic patterns with longer ranges along (28–37 km) than across the shelf (8–19 km). Variables affected by coastal processes (salinity and coloured dissolved organic matter) have an isotropic range similar to the baroclinic Rossby radius (10–15 km).
Revised: 20 Feb 2016 – Accepted: 09 Mar 2016 – Published: 31 Mar 2016
Schaeffer, A., Roughan, M., Jones, E. M., and White, D.: Physical and biogeochemical spatial scales of variability in the East Australian Current separation from shelf glider measurements, Biogeosciences, 13, 1967-1975, doi:10.5194/bg-13-1967-2016, 2016.