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En la desembocadura del rio Jemapa en Veracruz se observa le formacin de un dbil dipalo (estructura formada par dos v6rtices contrarrotatorios). Los hidr610gos

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En la desembocadura del rio Jemapa en Veracruz se observa le formacin de un dbil dipalo (estructura formada par dos v6rtices contrarrotatorios). Los hidr610gos y oceengrafos que son ingenieros mecSnicos estimaron que la forme anelltica de la vorticidad es En un punto especifico p = (0.873, 0.314) se tiene una trampe pera peces que se ve afecteda por le vorticidad del dipolo. Como la forma analitica es solo una estimaci6n, deben calcular la vorticidad apraximada con un mtodo de interpolacin bilineal. Par la betimetria del luger, slo es posible calocer elgunos pares de sensores. Si -stos se colocan con separaclones Ax = Ay = 0.25 km en una malla de 4 x 4 km2 centrada en el centro del dipolo, cuSl es el valor, con redondeo a 4 decimales, de la vonicidad en el punto p? 0.5 -2.5

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