Lots of attempt have been made to analyze sediment transport processes within submarine canyons using numerical modeling technique. What other importance could the said modeling serve?
Numerical modelling has many advantages. It allows for examination of different processes that may influence circulation within canyons where it is difficult to make extensive measurements. It also allows for selecting regions to where measurements can be undertaken.
The difficulty with sediment transport processes is that in some regions the canyons are a conduit to transport sediment offshore (e.g. those in the Mediterranean) in contrast others are upwelling favorable and support a large ecosystems (oasis) in the ocean (e.g. Australia). Often they may support both depending on the oceanography.
Here are some papers that may interest you some modelling some observations:
Trotter JA, Pattiaratchi CB, Montagna P, Taviani M, Falter J, Thresher R, Hosie AM, Haig D, Foglini F, Hua Q & McCulloch MT. 2019. First ROV exploration of the Perth Canyon: canyon setting, faunal observations, and anthropogenic impacts. Frontiers in Marine Science, 6, art. 173, doi: 10.3389/fmars.2019.00173.
de Vos A, Pattiaratchi CB & Harcourt R. 2014. Inter-annual variability in blue whale distribution off southern Sri Lanka between 2011 and 2012. Journal of Marine Science and Engineering, 2(3), 534–550.
Rennie SJ, Pattiaratchi CB & McCauley RD. 2009. Numerical simulation of the circulation within the Perth submarine canyon, Western Australia. Continental Shelf Research, 29(16), 2020–2036.
Rennie S, Hanson CE, McCauley RD, Pattiaratchi CB, Burton C, Bannister J, Jenner C & Jenner M-N. 2009. Physical properties and processes in the Perth Canyon, Western Australia: links to water column production and seasonal pygmy blue whale abundance. Journal of Marine Systems, 77(1–2), 21–44.
Poulos SE, Lykousis V, Collins MB, Rohling EJ & Pattiaratchi CB. 1999. Sedimentation processes in a tectonically active environment: the Kerkyra—Kefalonia submarine valley system (NE Ionian Sea). Marine Geology, 160, 25–44.
Ferentinos G, Collins MB, Pattiaratchi CB & Taylor PG. 1985. Mechanisms of sediment transport and dispersion in a tectonically active submarine valley/canyon system: Zakynthos straits, NW Hellenic trench. Marine Geology, 65(3–4), 243–269.
Additionally, numerical modeling allows for assuming many scenarios
and study the response of your system to these different changes in important parameters that affected the system, and by using the numerical models, we can examine the characteristics in places located far away that we cant make measurements there.