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Journal Article

Zhang Y, Witter RC, Priest GR. 2011. Tsunami–tide interaction in 1964 Prince William Sound tsunami. Ocean Modelling.

Rodrigues M, Oliveira A, Queiroga H, Fortunato AB, Zhang Y. 2009. Three-dimensional modeling of the lower trophic levels in the Ria de Aveiro (Portugal). Ecological Modelling. 220(9-10):1274-1290.

Rodrigues M, Oliveira A, Costa M, Fortunato AB, Zhang Y. 2009. Sensitivity analysis of an ecological model applied to the Ria de Aveiro.. Journal of Coastal Research. (Special Issue 56):448-452.

Zhang Y, Baptista AM. 2008. SELFE: A semi-implicit Eulerian–Lagrangian finite-element model for cross-scale ocean circulation. Ocean Modelling. 21(3-4):71-96.

Burla M, Baptista AM, Zhang Y, Frolov S. 2010. Seasonal and interannual variability of the Columbia River plume: A perspective enabled by multiyear simulation databases. Journal of Geophysical Research. 115(C00B16)

Witter RC, Jaffe B, Zhang Y, Priest GR. 2012. Reconstructing hydrodynamic flow parameters of the 1700 tsunami at Cannon Beach, Oregon, USA.. Natural Hazards. 63(1)

Zhang Y, Witter RC, Priest GP. 2011. Nonlinear Tsunami-Tide Interaction in 1964 Prince William Sound. Ocean Modeling.

Roland LA, Zhang Y, Wang HV, Maderich V, Brovchenko I. 2012. A fully coupled wave-current model on unstructured grids. Journal of Geophysical Research.

Frolov S, Baptista AM, Zhang Y, Seaton C. 2009. Estimation of ecologically significant circulation features of the Columbia River estuary and plume using a reduced-dimension Kalman filter. Continental Shelf Research. 29(2):456-466.

Zhang Y, Baptista AM. 2008. An Efficient and Robust Tsunami Model on Unstructured Grids. Part I: Inundation Benchmarks. Pure and Applied Geophysics. 165(11-12):2229-2248.

Azevedo A., Oliveira A, Fortunato AB, Zhang Y, Baptista AM. 2014. A cross-scale numerical modeling system for management support of oil spill accidents. Marine Pollution Bulletin. 80(1-2):132-147.

Priest GR, Goldfinger C, Wang K, Witter RC, Zhang Y, Baptista AM. 2009. Confidence levels for tsunami-inundation limits in northern Oregon inferred from a 10,000-year history of great earthquakes at the Cascadia subduction zone. Natural Hazards. 54(1):27-73.