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J. R. Campos and T. Kretzschmar, “Numerical Understanding of Regional Scale Water Table Behavior in the Guadalupe Valley Aquifer, Baja California, Mexico,” Hydrology and Earth System Sciences Discussions, Vol. 3, No. 3, 2006, pp. 707-730. http://www.hydrol-earth-syst-sci-discuss.net/3/707/2006/hessd-3-707-2006.pdf

has been cited by the following article:

• TITLE: Modeling of the Water Table Level Response Due to Extraordinary Precipitation Events: The Case of the Guadalupe Valley Aquifer

  AUTHORS: Javier González Ramírez, Rogelio Vázquez González

  KEYWORDS: Geohydrologic Model; Precipitation; Recharge; Finite Differences Method

  JOURNAL NAME: International Journal of Geosciences, Vol.4 No.6, August 14, 2013

  ABSTRACT: A two-dimensional algorithm for underground water flow simulation was modified and adapted to the geohydrologic conditions of the Guadalupe valley located in the state of Baja California in northern México. In order to solve the numerical model using the balance equation, the central finite differences with spatial and temporal constant increments method were used. Such model considers a heterogeneous and transient unconfined aquifer. Modeling and calibration processes are presented using the data of water table levels provided by the water level data loggers installed in a monitoring network and precipitation data from climatic stations of both seasons: 2009-2010 and 2010-2011. It was possible to locate, correlate and model specific rainfall-recharge events with the aim of obtaining an estimation of how these events are directly reflected on the water table level of the aquifer and how it reacts against simulated extraordinary events.