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    Geomagnetic Disturbances During the Maule (2010) Tsunami Detected by Four Spatiotemporal Methods
    (Springer Nature Link) Klausner, Virginia; Macedo, Humberto Gimenes; Cezarini, Marina Vedelago; Ojeda-González, Arian; Prestes, Alan; Cândido, Claudia Maria Nicoli; Kherani, Esfhan Alam; Santos, Thiago de Almeida
    Separating tsunamigenic variations in geomagnetic field measurements in the presence of more dominant magnetic variations by magnetospheric and ionospheric currents is a challenging task. The purpose of this article is to survey the tsunamigenic variations in the vertical component (Z) and the horizontal component (H) of the geomagnetic field using four spatiotemporal methods. Spatiotemporal analysis has shown enormous potential and efficiency in retrieving tsunamigenic contributions from geomagnetic field measurements. We select the Maule (2010) tsunami event on the west coast of Chile and examine the geomagnetic measurements from 13 ground magnetometers scattered in the Pacific Ocean covering a wide area from Chile, crossing the Pacific Ocean to Japan. The tsunamigenic magnetic disturbances are possibly due to two types of contributions, one arising from direct ocean motion and the other from atmospheric motion, both associated with tsunami forcing. Moreover, even though the tsunami waves decrease considerably with increasing epicentral distance, the tsunamigenic contributions are retrieved from a magnetic observatory in Australia ( 13,000 km radial distance from the epicenter). These results suggest that various types of tsunamigenic disturbances can be identified well from the integrated analysis framework presented in this work.
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    Modos de ondas magnetohidrodinámicas influenciados por la corriente de desplazamiento
    (Sociedade Brasileira de Física) Ojeda-González, Arian; González-Avilés, José Juan; Luz, Victor Hugo de La; Santos, Lenadro Nunes dos
    En este artículo trabajamos con la ecuación de velocidad de un fluido magneto-conductor utilizando dos aproximaciones: (i) la ley de Ampère y (ii) tomando en cuenta la corrección de Maxwell. Considerando una dirección arbitraria entre el vector de onda y el campo magnético se obtiene una expresión para la velocidad de fase de la onda. Existen tres modos de onda magnetohidrodinámicas (MHD) cuando la corriente de desplazamiento (Jd) no es considerada. Primero, se hace una comparación de los modos de onda entre sí, y después se comparan con los modos obtenidos con y sin la Jd. La comparación, permite discutir las variaciones entre estos modos MHD en los casos teóricos, cuando la velocidad de Alfvén aumenta hasta valores cercanos a la velocidad de la luz. El objetivo principal del art ́ıculo es mostrar la importancia del efecto de la Jd en los modos puro y ra ́pido de ondas MHD, en el caso particular en donde la velocidad de Alfvén es mayor que la velocidad adiaba ́tica de una onda acústica. Encontramos que para el modo lento, la Jd prácticamente no influye en el valor de la velocidad de fase de la onda cuando la velocidad de Alfv ́en aumenta.
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    Principal component analysis in the modeling of HILDCAAs during the Solar Minimum of Cycle 23/24
    (Elsevier) Klausner, Virginia; Lamin, Isabelle Cristine Pellegrini; Ojeda-González, Arian; Macedo, Humberto Gimenes; Cândido, Claudia Maria Nicoli; Prestes, Alan; Cezarini, Marina Vedelago
    In this article, we propose a new approach to model the high-intensity, long-duration, continuous AE (Auroral Electrojet) activity (HILDCAA) by relaxing one of the criteria originally designed, based on the interplanetary features during the unusual Solar Minimum of Cycle 23/24 (SMC23/24). This relaxation does not intend to suppress or modify the original HILDCAAs’ conception, but propose a new view of the same phenomena by enlarging the sample of events, which in turn may improve space weather monitoring and prediction programs. To assess and classify the Alfvénity associated with HILDCAAs, the values of 4h-Windowed Pearson Cross-Correlation (4WPCC) between the IMF components and the solar wind speed components observed in situ at the Lagrangian point L1 (1 AU) were evaluated. The principal component analysis (PCA) was performed on the dataset and, from the first three principal components, which represent 65% of the accumulative percent variance, we applied principal component regression (PCR) in each of the following parameters: the AE index, the Interplanetary Magnetic Field (IMF) components, the plasma density, the solar wind speed, the temperature, the IMF magnitude, and the SYM-H geomagnetic index. Furthermore, we applied Multiple Linear Regression (MLR) to establish a linear model to express the AE index in terms of the PCR-based model parameters. The AE MLR-based model demonstrated to hold a prognosis potential for HILDCAAs. Despite that, this model is only suitable for the SMC23/24. In this sense, this model might be implemented a real-time analysis for short-term HILDCAA prognosis in the near future.