Differences of the Solar Magnetic Activity Signature in Velocity and Intensity Helioseismic Observations

Differences of the Solar Magnetic Activity Signature in Velocity and Intensity Helioseismic Observations

Abstract

The high-quality, full-disk helioseismic observations continuously collected by the spectrophotometer GOLF and the three photometers VIRGO/SPMs onboard the SoHO spacecraft for 17 years now (since April 11, 1996, apart from the SoHO “vacations”) are absolutely unique for the study of the interior of the Sun and its variability with magnetic activity. Here, we look at the differences in the low-degree oscillation p-mode frequencies between radial velocity and intensity measurements taking into account all the known features of the p-mode profiles (e.g., the opposite peak asymmetry), and of the power spectrum (e.g., the presence of the higher degrees 4 and 5 in the signal). We show that the intensity frequencies are higher than the velocity frequencies during the solar cycle with a clear temporal dependence. The response between the individual angular degrees is also different. Time delays are observed between the temporal variations in GOLF and VIRGO frequencies. Such analysis is important in order to put new constraints and to better understand the mechanisms responsible for the temporal variations of the oscillation frequencies with the solar magnetic activity as well as their height dependences in the solar atmosphere. It is also important for the study of the stellar magnetic activity using asteroseismic data.

1Observations

We analyzed more than 6000 days of continuous observations collected by the space-based instruments Global Oscillations at Low Frequency [?] and Variability of Solar Irradiance and Gravity Oscillations [?] onboard the Solar and Heliospheric Observatory (SoHO) spacecraft. GOLF is a resonant scattering spectrophotometer measuring the Doppler wavelength shift - integrated over the solar surface - in the D1 and D2 Fraunhofer sodium lines at 589.6 and 589.0 nm respectively. The GOLF velocity time series were obtained following [?]. VIRGO is composed of three sunphotometers (SPMs) at 402 nm (blue), 500 nm (green), and 862 nm (red). The analyzed period covers more than 16 years between 1996 and 2012. The overall duty cycles of the GOLF and VIRGO time series are 95.4% and 95.2% respectively.

2Analysis

The datasets were split into contiguous 365-day subseries, with a four-time overlap. The power spectrum of each subseries was fitted by pair to extract the mode parameters [?] using a standard likelihood maximization function (power spectrum with a with 2 degree of freedom (d.o.f.) statistics ). Each mode component was parameterized using an asymmetric lorentzian profile [?], the asymmetry being assumed to be the same within a = 0 – 2 and a =1 – 3 pair of modes. The higher angular degrees = 4 and = 5 were included in the fitted model when visible (mainly between 2.5 and 3.3 mHz). Mean values of daily measurements of the 10.7-cm radio flux were used as a proxy of the solar surface activity.

3Results

The extracted mean frequencies between 2.5 and 3.5 mHz of the = 0, 1, and 2 modes, , are calculated on each 365-day segment for the different datasets. The panel a) of Figure 1 shows measured using the observations collected by GOLF and VIRGO (blue channel) as a function a time. The intensity frequencies are observed to be higher than the velocity frequencies, mainly during the solar maximum and minimum. Similar variations are observed between the three VIRGO/SPMs all over the solar cycle. Panels b) and c) show the frequency differences between the VIRGO/SPMs and GOLF, and between the three VIRGO/SPMs. We can see that intensity frequencies are systematically higher by about 30 nHz than the velocity frequencies over the solar cycle with a clear temporal dependence. This is in agreement with the ring-diagram analysis of the MDI velocity and continuum data performed by [?], although they found larger systematic differences of the order of 5 – 10 Hz. This is in sharp contrast with the comparison of the p-mode frequencies measured from the three VIRGO/SPMs.

The cross correlations between the GOLF and the VIRGO/SPMs frequencies, as well as the 10.7-cm radio flux, and between the three VIRGO/SPMs are also computed. The obtained time delays are given in Table 1. Negative time delays of over 30 days are observed between frequencies from GOLF and VIRGO. Higher delays are also observed between GOLF and VIRGO when compared to the 10.7-cm radio flux. Delays between the three VIRGO/SPMs are close to zero.

Figure 2 shows the mean frequencies between 2.5 and 3.5 mHz, , , and , for the angular degrees = 0, 1, and 2 individually. The main differences between intensity and velocity frequencies are at = 0 and = 1. Indeed, the intensity = 0 and 1 p-mode frequencies are observed to be higher than the velocity frequencies. The differences are larger during solar maximum, mainly in the case of the = 1 mode, where they can be over 100 nHz. On the other hand, the = 2 frequencies show almost no difference between intensity and velocity measurements.

Figure 1: (a) Temporal variations of the mean frequencies [2.5 – 3.5mHz] of the \ell = 0, 1, and 2 modes, \langle \nu_{\ell=0,1,2}\rangle, obtained with the velocity GOLF and intensity VIRGO/SPM blue channel measurements. (b) Frequency differences between the VIRGO/SPMs and GOLF frequencies. (c) Same as (b) but between the VIRGO/SPMs.
(a) Temporal variations of the mean frequencies [2.5 – 3.5mHz] of the \ell = 0, 1, and 2 modes, \langle \nu_{\ell=0,1,2}\rangle, obtained with the velocity GOLF and intensity VIRGO/SPM blue channel measurements. (b) Frequency differences between the VIRGO/SPMs and GOLF frequencies. (c) Same as (b) but between the VIRGO/SPMs.
(a) Temporal variations of the mean frequencies [2.5 – 3.5mHz] of the \ell = 0, 1, and 2 modes, \langle \nu_{\ell=0,1,2}\rangle, obtained with the velocity GOLF and intensity VIRGO/SPM blue channel measurements. (b) Frequency differences between the VIRGO/SPMs and GOLF frequencies. (c) Same as (b) but between the VIRGO/SPMs.
Figure 1: (a) Temporal variations of the mean frequencies [2.5 – 3.5mHz] of the = 0, 1, and 2 modes, , obtained with the velocity GOLF and intensity VIRGO/SPM blue channel measurements. (b) Frequency differences between the VIRGO/SPMs and GOLF frequencies. (c) Same as (b) but between the VIRGO/SPMs.

Table 1: Time delays (in days) between velocity GOLF and intensity VIRGO/SPMs observations, with the 10.7-cm solar radio flux (F10.7), and between the three VIRGO channels.
Cross-correlation between: Time delay (days)
GOLF – VIRGO Blue
GOLF – VIRGO Green
GOLF – VIRGO Red
GOLF – F10.7
VIRGO Blue – F10.7
VIRGO Green – F10.7
VIRGO Red – F10.7
VIRGO Blue – VIRGO Green
VIRGO Blue – VIRGO Red
VIRGO Red – VIRGO Green
Figure 2: Temporal variations of the mean frequencies [2.5 – 3.5mHz] of the individual \ell = 0, 1, and 2 modes, \langle \nu_{\ell=0}\rangle, \langle \nu_{\ell=1}\rangle, and \langle \nu_{\ell=2}\rangle, observed with the velocity GOLF and intensity VIRGO/SPM blue channel measurements.
Temporal variations of the mean frequencies [2.5 – 3.5mHz] of the individual \ell = 0, 1, and 2 modes, \langle \nu_{\ell=0}\rangle, \langle \nu_{\ell=1}\rangle, and \langle \nu_{\ell=2}\rangle, observed with the velocity GOLF and intensity VIRGO/SPM blue channel measurements.
Temporal variations of the mean frequencies [2.5 – 3.5mHz] of the individual \ell = 0, 1, and 2 modes, \langle \nu_{\ell=0}\rangle, \langle \nu_{\ell=1}\rangle, and \langle \nu_{\ell=2}\rangle, observed with the velocity GOLF and intensity VIRGO/SPM blue channel measurements.
Figure 2: Temporal variations of the mean frequencies [2.5 – 3.5mHz] of the individual , 1, and 2 modes, , , and , observed with the velocity GOLF and intensity VIRGO/SPM blue channel measurements.

4Conclusions

More than 6000 days of the radial velocity GOLF and photometric VIRGO/SPMs helioseismic observations are analyzed. Asymmetric lorentzian profiles are used to describe the solar acoustic oscillations in order to extract the p-mode parameters. Contiguous subseries of 365 days are used. The fitted velocity and intensity eigenfrequencies are compared. Systematic differences in the temporal variations of the p-mode frequencies up to 100 nHz are observed between the velocity GOLF and intensity VIRGO/SPMs observations. These differences are more important for the = 0 and 1 modes and they appear to be larger during the solar maximum of the activity cycle. The = 2 frequencies show almost no difference. Preliminary study of the coherence functions between velocity and intensity data confirm these results; a detailed comparison is in progress. Also, cross-correlation analysis shows negative time lags between the GOLF and VIRGO frequencies of about 30 days. Moreover, the temporal variations in GOLF and VIRGO frequencies are observed to be ahead of 10.7-cm solar radio flux by about 60 and 90 days respectively. Time lags between the VIRGO channels are close to zero.

The VIRGO instrument observes the solar oscillations at the base of the photosphere, whereas GOLF observes a few hundred kilometers higher in the atmosphere [?]. The observed differences could arise from a height dependence of the p-mode frequency variations with solar activity. Moreover, are the differences observed at = 0 indirectly showing the Sun’s radius varying? Also, these frequency differences might be larger in stars more active than the Sun. Nevertheless, there are few possible misleading origins for these differences between velocity and intensity observations. For instance, we cannot rule out probable interplays between the fitted peak asymmetry and the solar background and their variations with magnetic activity. Then, different realization noises between intensity and velocity measurements might impact the fitted frequencies as well. Finally, the asymmetric lorentzian profile [?] used to describe the p-mode oscillations might not be correct or one or more parameters might be missing in the description of the peak asymmetry.

The GOLF and VIRGO instruments onboard SoHO are a cooperative effort of many individuals, to whom we are indebted. SoHO is a project of international collaboration between ESA and NASA. The 10.7-cm radio flux data were obtained from the National Geophysical Data Center. This work has been partially supported by the CNES/GOLF grant at the SAp CEA-Saclay.

Comments 0
Request Comment
You are adding the first comment!
How to quickly get a good reply:
  • Give credit where it’s due by listing out the positive aspects of a paper before getting into which changes should be made.
  • Be specific in your critique, and provide supporting evidence with appropriate references to substantiate general statements.
  • Your comment should inspire ideas to flow and help the author improves the paper.

The better we are at sharing our knowledge with each other, the faster we move forward.
""
The feedback must be of minimum 40 characters and the title a minimum of 5 characters
   
Add comment
Cancel
Loading ...
11328
This is a comment super asjknd jkasnjk adsnkj
Upvote
Downvote
""
The feedback must be of minumum 40 characters
The feedback must be of minumum 40 characters
Submit
Cancel

You are asking your first question!
How to quickly get a good answer:
  • Keep your question short and to the point
  • Check for grammar or spelling errors.
  • Phrase it like a question
Test
Test description