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Albert Y. Kuo

Affiliations: 
College of William and Mary, Williamsburg, VA 
Area:
Geophysics, Physical Oceanography
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"Albert Kuo"
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Shen J, Hong B, Kuo AY. (2013) Using timescales to interpret dissolved oxygen distributions in the bottom waters of Chesapeake Bay Limnology and Oceanography. 58: 2237-2248
Yang WC, Lee CH, Chen WB, et al. (2010) A numerical model simulation of cross scale interaction between river plume and coastal flows Proceedings of the International Offshore and Polar Engineering Conference. 3: 1061-1068
Wang CF, Wang HV, Kuo AY. (2008) Mass conservative transport scheme for the application of the ELCIRC model to water quality computation Journal of Hydraulic Engineering. 134: 1166-1171
Wang CF, Hsu MH, Liu WC, et al. (2007) Simulation of water quality and plankton dynamics in the Danshuei River estuary, Taiwan. Journal of Environmental Science and Health. Part a, Toxic/Hazardous Substances & Environmental Engineering. 42: 933-53
Liu WC, Chen WB, Cheng RT, et al. (2007) Modeling the influence of river discharge on salt intrusion and residual circulation in Danshuei River estuary, Taiwan Continental Shelf Research. 27: 900-921
Liu WC, Hsu MH, Kuo AY, et al. (2007) Effect of channel connection on flow and salinity distribution of Danshuei River estuary Applied Mathematical Modelling. 31: 1015-1028
Liu WC, Hsu MH, Kuo AY. (2007) Three-dimensional hydrodynamic and salinity transport modelling of Danshuei River estuarine system and adjacent coastal sea, Taiwan Hydrological Processes. 21: 3057-3071
Hsu MH, Wu CR, Liu WC, et al. (2006) Investigation of turbidity maximum in a Mesotidal Estuary, Taiwan Journal of the American Water Resources Association. 42: 901-914
Liu WC, Liu SY, Hsu MH, et al. (2005) Water quality modeling to determine minimum instream flow for fish survival in tidal rivers. Journal of Environmental Management. 76: 293-308
Liu WC, Hsu MH, Chen SY, et al. (2005) Water column light attenuation in Danshuei River estuary, Taiwan Journal of the American Water Resources Association. 41: 425-435
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