Hidrodinámica del Estero Punta Banda: aprendiendo de un curso

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Transcripción de la presentación:

Hidrodinámica del Estero Punta Banda: aprendiendo de un curso Participantes en el curso de Hidrodinámica de Estuarios y Lagunas Costeras a cargo de: Arnoldo ValleLevinson Universidad de Florida Gainesville, FL arnoldo@ufl.edu José Gómez CICESE Ensenada, BC, Mexico jgomez@cicese.mx

FLUJO DE MAREA EN UN CANAL UNIFORME x y B H (y) A Huijts, et al.(2006, J. Geophys. Res., 111, C12016, doi:10.1029/2006JC003615)

Amplitud Fase

ADCP - Luis Gustavo Alvarez ADCP – Amaia Ruiz de Alegria Mediciones Afuera – Adan Mejia & Xavier Flores CTD – David Rivas CTD – Héctor García Nava Derivadores & Viento – Xavier Flores Arturo Ocampo Erick Rivera Lemus

cm/s Mayo 2014

Viendo hacia adentro

Xavier Flores

cm/s Mayo 2014

Fin de vaciante Profundidad (m) Distancia (m)

Vaciante Profundidad (m) Distancia (m)

Llenante Profundidad (m) Distancia (m)

Flujo Residual (Promedio de los 2 ciclos de marea)

sale entra Viendo hacia afuera

Volumen de flujo de salida ~5 m3/s sale entra Viendo hacia adentro Volumen de flujo de salida ~5 m3/s

Current Tide cm/s o m Mayo 2014

Tidal Residuals in Homogeneous Systems z δ=4L/λ > 0.6-0.7 δ=4L/λ < 0.6-0.7 Li and O’Donnell (2005, JPO, 1826)

Examples of Tidal Residuals Influenced by Bathymetry in a Short Channel OUT OUT IN St Augustine Inlet St. Augustine Inlet location and cross-section of net exchange flow pattern. Red and yellow shades indicate regions of net outflow while blue shades denote regions of inflow.

low E med E high E Ke = B/R; E = Az / (f H2) (wide) (narrow) So in order to address that question, the solution can be examined in terms of the Kelvin number (ratio of width of system vs internal Rossby radius) Three generalities may be drawn for the along-estuary flows (contours): 1) Exchange pattern depends on the width of the system: inflow occupies entire water column for low E and high Ke 2) Two-way exchange is most vigorous with moderate friction (med E) 3) Exchange pattern is independent of width of system for high E: inflow occupies the entire column high E Ke = B/R; E = Az / (f H2) (looking into the estuary; orange is inflow; white is outflow)

sale entra Viendo hacia adentro

Mareas Cabeza m Temperatura (oC) Día desde Abril 2014