DISCUSSION AND CONCL isprsarchives XXXVIII 4 C26 21 2012

The kriging variogram’s dependent predictiv in Figure 2. In general, the lower the e location, the better is the prediction of the sp The final spatial model permits us to visual volumes as well as cuts in any plane of the Figure 3. Geospatial representation of Up approximately the upper 500 m of the constituted of UHW and voxels containing black dots. Vertical exaggeration in fig

4. DISCUSSION AND CONCL

This research has explored the potential modelling tools for the study of marine pel review of common GIS indicates that these mostly lack the necessary functions representation of gradual phenomena, primo study of marine ecosystems. However geomodelling tools for representation of t promising, which is illustrated in this paper 3D solution to visualization of a water mass Beaufort Sea, constructed with Paradigm Integration of volumetric representation in a an important advance towards an optimal ma must also include representation and analys static vertical cuts. On the contrary, geomo be adapted to the marine environment b functions for oceanographic research such and analyses. However, all spatial modelling the pelagic environment would also bene spatial data structure that takes into conside nature and fuzzy boundaries of the pelagic en ctive error is presented error for a specific spatial model. alize iso-surfaces and he water mass Figure 3 and enables spatial 3D analyses and intersection. This case study s volumetric representation develope tools can be used to extend usual i pelagic phenomena from 2D st environment. pper Halocline Water on the Mackenzie shelf in summer 2009 e water mass contained within the spatial model. Scale indicat ing more than 60 of UHW are coloured-filled. Visible samp figure is 75 times that of reality. Spatial model was constructed CLUSIONS ial of 3D geospatial pelagic ecosystems. A ese software products ns for volumetric mordial for geospatial ver, performance of f this environment is er by a snap-shot of a ss in the south-eastern m Gocad Figure 3. a GIS environment is marine GIS. This tool lyses functions of 2D modelling tools could by improving basic ch as image treatment ing tools conceived for enefit from including ideration the dynamic environment. Our future research will explor geospatial modelling tools for the ground data in the identification organic carbon fluxes in the Beaufo

5. ACKNOWLED