The Cluster data from the CIS and FGM instruments are subjected to complex Morlet wavelet transform technique to investigate the mgnetic diffusivity of magnetic reconnection in the dayside magnetopause during 10:25-11:33 UT on 26 January 2001. The analysis of the computed parameter magnetic diffusivity (ç) bring out new features such as period doubling and chaos in the reconnection site.
Copy the following to cite this article:
R. G; S. Simi, "Wavelet analysis of Magnetic Diffusivity at magnetopause of Earth using CLUSTER data", Journal of Ultra Scientist of Physical Sciences, Volume 22, Issue 3, Page Number 675-679, 2018Copy the following to cite this URL:
R. G; S. Simi, "Wavelet analysis of Magnetic Diffusivity at magnetopause of Earth using CLUSTER data", Journal of Ultra Scientist of Physical Sciences, Volume 22, Issue 3, Page Number 675-679, 2018Available from: http://ultraphysicalsciences.org/paper/944/
