Abstract:The active region, AR0554, was observed with NIS/CDS on board SoHO to examine the extent and range of oscillations from a range of features. Among all the NIS spectral lines analysed, significant oscillations were found in Si xii 520 Å, Mg x 625 Å, O v 629 Å, and He i 522 Å. The periods of the strongest oscillations in these lines were ≈10−20 min. After the dominant 10−20 min oscillations were filtered out from these lines, only O v 629 Å showed significant (i.e. above the 95% significance level) shorter-perio… Show more
“…Figure 7 demonstrates such an example: the P700-filtered wavelet spectrum shows that there are only two major period bands, 200-300 s and 400-500 s, for the oscillations before 30 min while the spectrum of the oscillations between 30 and 60 min extends from 100 s to 700 s. When the modes of periods longer than 300 s are filtered out, the strongest oscillation in the P300-filtered signal often shows a periodicity ≈3 min, and the oscillation is most significant for the time interval 30-65 min of the observing sequence, which corresponds to the transit time interval for the MMF across our CDS pixel. This result echoes the conclusion by Lin et al (2005) that 3-min oscillations can exist outside of a sunspot in regions with strong magnetic fields.…”
Context. While moving magnetic features have been studied extensively at the photospheric level, the effect they have on the upper atmosphere remains largely unknown, and it is this which we seek to address in this work. Aims. In this work we aim to investigate the chromospheric and transition-region dynamics associated with a moving magnetic monopole by using spectral time-series and images. Methods. Cross correlation was applied to images taken by different instruments and at different times in order to spatially correlate brightenings seen at transition region temperatures with moving magnetic features seen in magnetograms. We used wavelet analysis to examine and compare the periodicities of time-series signals in different regions.Results. Oscillations with a multitude of frequencies are found in the chromospheric and transition-region brightenings associated with a moving magnetic monopole. The region of the brightenings shows a tendency to be blue-shifted when compared to the average motion of the entire field of view. The results indicate the presence of waves and/or flows carrying energy from the monopole to the higher atmosphere. Conclusions. We studied the influence of a moving magnetic monopole, as recorded by magnetograms, up to transition region temperatures. This suggests that the magnetic monopole, despite being small, can influence dynamics in the upper atmospheric layers.
“…Figure 7 demonstrates such an example: the P700-filtered wavelet spectrum shows that there are only two major period bands, 200-300 s and 400-500 s, for the oscillations before 30 min while the spectrum of the oscillations between 30 and 60 min extends from 100 s to 700 s. When the modes of periods longer than 300 s are filtered out, the strongest oscillation in the P300-filtered signal often shows a periodicity ≈3 min, and the oscillation is most significant for the time interval 30-65 min of the observing sequence, which corresponds to the transit time interval for the MMF across our CDS pixel. This result echoes the conclusion by Lin et al (2005) that 3-min oscillations can exist outside of a sunspot in regions with strong magnetic fields.…”
Context. While moving magnetic features have been studied extensively at the photospheric level, the effect they have on the upper atmosphere remains largely unknown, and it is this which we seek to address in this work. Aims. In this work we aim to investigate the chromospheric and transition-region dynamics associated with a moving magnetic monopole by using spectral time-series and images. Methods. Cross correlation was applied to images taken by different instruments and at different times in order to spatially correlate brightenings seen at transition region temperatures with moving magnetic features seen in magnetograms. We used wavelet analysis to examine and compare the periodicities of time-series signals in different regions.Results. Oscillations with a multitude of frequencies are found in the chromospheric and transition-region brightenings associated with a moving magnetic monopole. The region of the brightenings shows a tendency to be blue-shifted when compared to the average motion of the entire field of view. The results indicate the presence of waves and/or flows carrying energy from the monopole to the higher atmosphere. Conclusions. We studied the influence of a moving magnetic monopole, as recorded by magnetograms, up to transition region temperatures. This suggests that the magnetic monopole, despite being small, can influence dynamics in the upper atmospheric layers.
“…Indeed, the strong magnetic field regions (sunspots, magnetic network cores) show predominantly 3-min oscillations in the chromosphere. Note that some observations also show the 3-min oscillations in the solar corona above sunspots (De Moortel et al 2002) and other magnetic structures (Lin et al 2005). These oscillations can be excited as a consequence of consecutive shocks due to chromospheric 3-min oscillations.…”
Section: Discussion and Summarymentioning
confidence: 86%
“…Propagating acoustic waves are frequently seen in the solar corona as periodic variations of spectral line intensity (De Moortel et al 2000, Marsh et al 2003, Lin et al 2005, 2006, Srivastava et al 2008, Wang et al 2009. As these waves are often observed within the frequency range corresponding to the acoustic waves in the solar photosphere/chromosphere, this logically leads to the idea of penetration of the photospheric acoustic oscillations into the corona.…”
Aims. We aim to study excitation of the observed ∼5-min oscillations in the solar corona by localized pulses that are launched in the photosphere. Methods. We solve the full set of nonlinear one-dimensional Euler equations numerically for the velocity pulse propagating in the solar atmosphere that is determined by the realistic temperature profile. Results. Numerical simulations show that an initial velocity pulse quickly steepens into a leading shock, while the nonlinear wake in the chromosphere leads to the formation of consecutive pulses. The time interval between the arrivals of two neighboring pulses to a detection point in the corona is approximately 5 min. Therefore, the consecutive pulses may result in the ∼5-min oscillations that are observed in the solar corona. Conclusions. The ∼5-min oscillations observed in the solar corona can be explained in terms of consecutive shocks that result from impulsive triggers launched within the solar photosphere by granulation and/or reconnection.
“…Tsiropoula et al (2009) reported 5 min oscillations in the dark mottle and network boundaries, and suggested the upward propagating waves at the network boundary, and standing waves at the mottle region. In the previous studies, 3 min oscillations are widely reported in the TR spectral line formed above the sunspots, and interpreted as a signature of upward propagating waves (e.g., Gurman et al 1982;Brynildsen et al 1999;Maltby et al 2001;Fludra 2001;O'Shea et al 2002;Brynildsen et al 2003Brynildsen et al , 2004Lin et al 2005;Sych et al 2012). Jess et al (2008) studied the velocity oscillations in the bright active region at the TR height and reported high frequency oscillations with a dominant period of 26 ± 4 sec.…”
In the present paper, we use Si IV 1393.755 Å spectral line observed by the Interface Region Imaging Spectrograph (IRIS) in the quiet-Sun to determine physical nature of the solar transition region (TR) oscillations. We analyze the properties of these oscillations using wavelet tools (e.g., power, cross-power, coherence, and phase difference) along with the stringent noise model (i.e., power-law + constant). We estimate the period of the intensity and Doppler velocity oscillations at each chosen location in the quiet-Sun (QS) and quantify the distribution of the statistically significant power and associated periods in one bright and two dark regions. In the bright TR region, the mean periods in intensity and velocity are 7 min, and 8 min respectively. In the dark region, the mean periods in intensity and velocity are 7 min, and 5.4 min respectively. We also estimate the phase difference between the intensity and Doppler velocity oscillations at each location. The statistical distribution of phase difference is estimated, which peaks at -119°± 13°, 33°± 10°, 102°± 10°in the bright region, while at -153°± 13°, 6°± 20°, 151°± 10°in the dark region. The statistical distribution reveals that the oscillations are caused by propagating slow magnetoacoustic waves encountered with the TR. Some of these locations may also be associated with the standing slow waves. Even, in the given time domain, several locations exhibit presence of both propagating and standing oscillations at different frequencies.
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