Hector Gonzalez-Huizar
Current Organizations / Institutes
The organizations/institutes from the scholar's latest article
Hector Gonzalez-Huizar has a total of 9 co-authors. Here are the top co-authors by number of shared publications:
Aaron A. Velasco
Geological Sciences, University of Texas at El Paso, El Paso, Texas, USA
2 shared publications- Maria Christina Mariani
Department of Mathematical Sciences, The University of Texas at El Paso, El Paso, TX 79968, USA
1 shared publication - María Pía Beccar Varela
Department of Mathematical Sciences, University of Texas at El Paso, El Paso, TX 79968, USA
1 shared publication - Osei Kofi Tweneboah
Ramapo Data Science Program, Ramapo College of New Jersey, Mahwah, NJ 07430, USA
1 shared publication - Peter K. Asante
Computational Science Program, University of Texas at El Paso, El Paso, TX 79902, USA
1 shared publication - Raul Ramon Castro
Centro de Investigación Científica y de Educación Superior de Ensenada
1 shared publication
Latest Publications
- Open Access
- 30 June 2020
- Published by MDPI AG in Mathematics
- Vol. 8 (7) , 1046
Self-Similar Models: Relationship between the Diffusion Entropy Analysis, Detrended Fluctuation Analysis and Lévy Models
Financial and geophysical data, like many other low and high frequency time series, are known to exhibit some memory effects. These memory effects may be long or short, permanent or temporal depending on the event that is being modeled. The purpose of this study is to investigate the memory effects characterized by the financial market closing values and volcanic eruption time series as well as to investigate the relation between the self-similar models used and the Lévy process. This paper uses highly effective scaling methods including Lévy processes, Detrended Fluctuation Analysis (DFA) and Diffusion Entropy Analysis (DEA) to examine long-range persistence behavior in time series by estimating their respective parameters. We use the parameter of the Lévy process (α) characterizing the data and the scaling parameters of DFA (H) and DEA (δ) characterizing the self-similar property to generate a relationship between the three (3) aforementioned scaling methods. Findings from the numerical simulations confirm the existence of long-range persistence (long-memory behavior) in both the financial and geophysical time series. Furthermore, the numerical results from this study indicates an approximate inverse relationship between the parameter of the Lévy process and the scaling parameters of the DFA and DEA (i.e., ), which we prove analytically.- 30 June 2020
- Published by MDPI AG in Mathematics
- Vol. 8 (7) , 1046
Open AccessSelf-Similar Models: Relationship between the Diffusion Entropy Analysis, Detrended Fluctuation Analysis and Lévy Models
Financial and geophysical data, like many other low and high frequency time series, are known to exhibit some memory effects. These memory effects may be long or short, permanent or temporal depending on the event that is being modeled. The purpose of this study is to investigate the memory effects characterized by the financial market closing values and volcanic eruption time series as well as to investigate the relation between the self-similar models used and the Lévy process. This paper uses highly effective scaling methods including Lévy processes, Detrended Fluctuation Analysis (DFA) and Diffusion Entropy Analysis (DEA) to examine long-range persistence behavior in time series by estimating their respective parameters. We use the parameter of the Lévy process (α) characterizing the data and the scaling parameters of DFA (H) and DEA (δ) characterizing the self-similar property to generate a relationship between the three (3) aforementioned scaling methods. Findings from the numerical simulations confirm the existence of long-range persistence (long-memory behavior) in both the financial and geophysical time series. Furthermore, the numerical results from this study indicates an approximate inverse relationship between the parameter of the Lévy process and the scaling parameters of the DFA and DEA (i.e., ), which we prove analytically. - 19 May 2012
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 39 (10)
Remote triggered seismicity caused by the 2011, M9.0 Tohoku‐Oki, Japan earthquake
Seismic waves from large earthquakes have been shown to trigger seismicity large distances from a mainshock, and this is termed remotely or dynamically triggered seismicity. We performed a global search for seismicity potentially triggered by the seismic waves from the 2011, M9.0, Tohoku‐Oki, Japan Earthquake. Using seismograms from global seismic networks and an event catalog, we search for earthquakes and tremors instantaneously triggered during the passing of the seismic waves, as well as for statistically significant changes in local and global seismic rates after the passing of the waves. For earthquakes, we find potential cases of instantaneous triggering in the United States, Russia, China, Ecuador and Mexico, while for tremors we find evidence for triggering in Taiwan, Armenia, Cuba and the United States. In addition, we observed a potential case of delayed triggering of larger magnitude earthquakes (including a M5.2) in Baja California, Mexico.
- 19 May 2012
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 39 (10)
Remote triggered seismicity caused by the 2011, M9.0 Tohoku‐Oki, Japan earthquake
Seismic waves from large earthquakes have been shown to trigger seismicity large distances from a mainshock, and this is termed remotely or dynamically triggered seismicity. We performed a global search for seismicity potentially triggered by the seismic waves from the 2011, M9.0, Tohoku‐Oki, Japan Earthquake. Using seismograms from global seismic networks and an event catalog, we search for earthquakes and tremors instantaneously triggered during the passing of the seismic waves, as well as for statistically significant changes in local and global seismic rates after the passing of the waves. For earthquakes, we find potential cases of instantaneous triggering in the United States, Russia, China, Ecuador and Mexico, while for tremors we find evidence for triggering in Taiwan, Armenia, Cuba and the United States. In addition, we observed a potential case of delayed triggering of larger magnitude earthquakes (including a M5.2) in Baja California, Mexico.
- 5 February 2011
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 116 (B2)
Dynamic triggering: Stress modeling and a case study
- 5 February 2011
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 116 (B2)
Dynamic triggering: Stress modeling and a case study