Analysis of persistence in fluctuation of the Cauca river through the Hurst coefficient

D. A. Prada; M. P. Sanabria; A. F. Torres; A. Acevedo; J. Gómez

doi:10.1088/1742-6596/1002/1/012011

Analysis of persistence in fluctuation of the Cauca river through the Hurst coefficient

D. A. Prada
, M. P. Sanabria
, A. F. Torres
, A. Acevedo
, J. Gómez

Research output: Contribution to scientific journal › Conference and proceedings › peer-review

Abstract

Study the continuous changes in the fluctuations in the levels of watersheds, it is of great importance because it allows you to adjust predictions about behaviors that can lead to floods or droughts. The Cauca River is one of the most important rivers in Colombia due to its 1350km long, its drainage area of 59.074km ² which represents 5% of the national territory. The Government entity Cormagdalena records daily levels of the Cauca River to the height of La Mojana in the rods. From these data, we developed a series of time on which normal test were applied to calculate the coefficient of Hurst and the fractal dimension to determine the persistence associated with this behavior.

Original language	English
Article number	012011
Journal	Journal of Physics: Conference Series
Volume	1002
Issue number	1
DOIs	https://doi.org/10.1088/1742-6596/1002/1/012011
State	Published - 5 Apr 2018
Event	1st Multi-Campus Meeting on Basic Science - Medellin, Colombia Duration: 29 Sep 2017 → 29 Sep 2017

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Publisher Copyright:
© Published under licence by IOP Publishing Ltd.

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Scientific events with a public engagement component

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10.1088/1742-6596/1002/1/012011

Cite this

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title = "Analysis of persistence in fluctuation of the Cauca river through the Hurst coefficient",

abstract = "Study the continuous changes in the fluctuations in the levels of watersheds, it is of great importance because it allows you to adjust predictions about behaviors that can lead to floods or droughts. The Cauca River is one of the most important rivers in Colombia due to its 1350km long, its drainage area of 59.074km 2 which represents 5\% of the national territory. The Government entity Cormagdalena records daily levels of the Cauca River to the height of La Mojana in the rods. From these data, we developed a series of time on which normal test were applied to calculate the coefficient of Hurst and the fractal dimension to determine the persistence associated with this behavior.",

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AU - Sanabria, M. P.

AU - Torres, A. F.

AU - Acevedo, A.

AU - Gómez, J.

N1 - Publisher Copyright: © Published under licence by IOP Publishing Ltd.

PY - 2018/4/5

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N2 - Study the continuous changes in the fluctuations in the levels of watersheds, it is of great importance because it allows you to adjust predictions about behaviors that can lead to floods or droughts. The Cauca River is one of the most important rivers in Colombia due to its 1350km long, its drainage area of 59.074km 2 which represents 5% of the national territory. The Government entity Cormagdalena records daily levels of the Cauca River to the height of La Mojana in the rods. From these data, we developed a series of time on which normal test were applied to calculate the coefficient of Hurst and the fractal dimension to determine the persistence associated with this behavior.

AB - Study the continuous changes in the fluctuations in the levels of watersheds, it is of great importance because it allows you to adjust predictions about behaviors that can lead to floods or droughts. The Cauca River is one of the most important rivers in Colombia due to its 1350km long, its drainage area of 59.074km 2 which represents 5% of the national territory. The Government entity Cormagdalena records daily levels of the Cauca River to the height of La Mojana in the rods. From these data, we developed a series of time on which normal test were applied to calculate the coefficient of Hurst and the fractal dimension to determine the persistence associated with this behavior.

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T2 - 1st Multi-Campus Meeting on Basic Science

Y2 - 29 September 2017 through 29 September 2017

ER -

Analysis of persistence in fluctuation of the Cauca river through the Hurst coefficient

Abstract

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