Periodic Reporting for period 1 - ELISITY (fiEld Line helIcity and Solar eruptivITY)
Reporting period: 2021-03-01 to 2023-02-28
It is well known that solar activity is of magnetic origin. The constant photospheric motions twist and tangle the magnetic field lines, resulting in the build up of energy into the magnetic field. Once this gets distorted enough it can experience a sudden rearrangement of its topology, known as magnetic reconnection, which releases the stored energy in an explosive manner.
A quantity that can measure the geometrical complexity of a magnetic field is magnetic helicity, which, moreover, is conserved in ideal magneto-hydrodynamic (MHD), the theoretical description of the solar atmosphere. A proxy for the density of relative magnetic helicity, the appropriate helicity in the case of the Sun, is relative field line helicity (RFLH), a quantity that can highlight the locations where helicity is more important. Before the start of this project, studies of RFLH were mostly restricted to approximations and/or MHD simulations of the Sun.
The main goal of this project was thus to study in detail the behaviour of RFLH in solar active regions (ARs) during the production and early stages of solar eruptions. Additionally, to determine whether RFLH could be used to define quantities which indicate solar eruptivity.
Apart from RFLH, many other physical parameters of the ARs were estimated, such as various energies and magnetic helicities. The quality of the reconstructed coronal magnetic fields was also assessed with many metrics and only those with high levels of solenoidality were considered in the subsequent study.
The analysis of RFLH was restricted to the times around 28 big flares (above M-class) from seven ARs, and to the regions known as magnetic polarity inversion lines (PILs) where the magnetic field changes sign. The use of RFLH allowed us to estimate the relative magnetic helicity in these PILs, in addition to the other physical parameters. The comparison of the relative helicity of the PILs with their magnetic flux, a quantity known as the R-parameter and whose high values are related with strong solar flares, showed that the helicity-based R values are as good as the magnetic-field-based ones, and sometimes, outperform the traditional ones. Apart from these quantities, many other PIL-deduced parameters were examined as well, but they did not show similar potential in indicating solar eruptivity.
The results of the project were (and will be) published in two international peer-reviewed scientific journals. They were also disseminated through oral and poster presentations, physically or virtually, in eight international scientific conferences, both in Greece and abroad.
The researcher of the project also participated in outreach activities, at schools or with the general public, such as the online ‘Science is Wonderful! 2021’ event, or the ‘2022 European Researchers’ Night’ in Athens, Greece. He also gained experience in teaching activities at the host University and in familiarization with solar observations. More details for the project can be found at its webpage, at the address ‘myweb.uoi.gr/k.moraitis/elisity.html’, where links to individual results are given.
The results of the project have the potential to be further exploited in Space Weather applications that aim at the prediction of solar activity. The work of this project, by showcasing the helicity-based R parameter as a viable eruptivity indicator, is a first step towards this direction.