Gerry Doyle's homepage Solar Physics

Solar Physics

General Introduction

November 1995 seen the launch of ESA's first cornerstone mission in its Horizon 2000 programme, i.e. the Solar and Heliospheric Observatory (SOHO) while in April 1998 NASA launched TRACE and in September 2007, we had the launch of the Japanese mission Hinode . The objective of these missions is to

the nature of the solar corona

the acceleration of the solar wind, and

the internal structure of the Sun

It is towards the first of these topics that my effort is directed and, in particular, the question of coronal heating.

It has being known for several decades that the solar corona has temperatures in excess of one million degress, however, the mechanism by which this is maintained is still an outstanding problem to-day. There have been many suggestions including, Alfven wave dissipation, turbulent cascades, currents sheets dissipation or nanoflaring and anomalous interruption of field-aligned currents. As of yet, none of these have proven to be entirely satisfactory.

The choice of wavelength region for observing various parts of the solar atmosphere is determined by the range of temperatures required to be studied. For example, in order to study the solar corona and the chromospheric-coronal transition region requires data shortward of 1600A region.

From previous missions we know of plasma structures varying in size from a solar radii to less than 1 arc sec (i.e. 725 km). For coronal heating the most critical are the small scale structures, mostly in the form of loops. Coordinated observations with the above suite of instruments (plus ground-based coverage) has the capacity to provide invaluable and unique data for solar physicists for the next decade which will enable major advancements in this area.

Previous related work

Prior to 1975 the best UV and X-ray observations of the solar corona and the transition region were those based on data obtained during the SKYLAB mission. Since then there have been several important missions including, OSO 8, SMM, various HRTS & NIXT rocket flights and YOHKOH . Based on the data obtained from these missions we know that the intensities of chromospheric lines decreases rapidly outside the chromospheric limb (as determined from say H alpha). In the transition region, intensities persist to much higher altitudes, reaching a maximum at ~3000km but remaining strong to altitudes of ~10,000km. From differential emission measure analysis and using derived electron densities, plane parallel model atmospheres calculations imply a transition region thickness of only ~70km similar to that derived using opacity methods. Thus the observed range of altitudes cannot be explained by plane parallel atmospheres. A possible remedy is to extend the emission by assuming the transition region gas is in thin structures, i.e. to assume filling factors << 1.

In addition to contributing to the picture of a finely structured transition region, HRTS has revealed the presence of a highly dynamic environment. For example, it was shown that transition region line profiles cannot be represented by a single Gaussian but instead showed a very complex velocity structure. In many instances only an average velocity was computed with the loss of relevant information on the dynamics. These multiple velocities were observed in many different locations ranging from sunspots, to active regions and sometimes in the so-called quiet regions. In fact, in `quiet' region, these multiple velocities were observed ~15% of the time and this may be a lower limit. The spectral lines concerned were those of lines formed at temperatures of 80,000 to 100,000K. These lines showed both red- and blue-shifted components and were present at both Sun center and at the limb. Flow velocities were both sub- and supersonic. However, the mechanism causing these flows and whether they extend to coronal temperatures is still a matter of speculation.

Thus the picture emerging from these observations is that the transition region should not be considered as static or stationary. Instead we may have a transition region comprising of an ensemble of small, nearly isothermal loops. The current array of instruments on SOHO has the potential of providing valuable observational data relating to temperatures structures ranging from twenty thousand degrees to over a million degrees. Such data can be used to provide important input not only for heating of the Sun's corona but to the heating of stellar coronae in general.

Proposed programme of work

CDS has two spectrometers; the Normal Incidence Spectrometer covering the wavelength ranges 310 - 380A and 517 - 633A and the Grazing Incidence Spectrometer covering the ranges 155 - 224A, 261 - 346A, 396 - 496A and 662 - 787A. It's spectral resolution is of the order of 17 km/s. On the other-hand, SUMER will cover the wavelength range 800 - 1600A in first order and 500 - 800A in second order with a spectral resolution of 1 km/s. The major part of our proposed programme is to use data from these two instruments, although data from instruments such as EIT will also be used.

With high time resolution data over extended periods we can look at the possibility of detecting loop oscillations. In fact, based on SMM observations, oscillations in the UV continuum at 1370A have already being observed. The observed periods are all in the range 4 to 7 mins, consistent with the range of observed global photospheric periods. These observations were obtained using a 13x13 pixel raster (each raster of 10x10 arc sec) with a cycle time between rasters of 22 sec. It was normally found that only a small numbers of pixels show a periodicity while adjacent pixels were void of any periods. Such structures were therefore small, of the order of 10 to 20 arc sec and the question we wish to ask is why only some regions showed a periodicity. One can argue that these regions were simply resonating with the under-lying photospheric period, however, why only these regions and could this have implications for coronal heating (waves versus reconnection). We therefore plan an observational programme aimed at obtaining data as a function of temperature using both rasters and line profiles modes (the SMM data were taken only in the UV continuum at 1370A and therefore we do not have sufficient information on the temperature and/or height of these oscillations).

The above programme will be directed towards active and non-active regions, in particular loop structures. We plan to look at these structures both on-disk and those approaching the limb. Using high spectral resolution of selected lines with SUMER we can investigate profile changes, with CDS we can perform rasters plus line ratio diagnostics. With this data we can therefore investigate the microscopic transition region structure which has to be related to the local heating mechanism. This will then allow us to investigate how this microscopic structure can explain such characteristics of the transition region as the general redshift of EUV and UV spectral lines, the large-scale temperature stratification and the universal emission measure. On Hinode, we use EIS , SOT and XRT .

The above also involves the use of atomic physics in particular the data required for the various diagnostics line ratios. For this we use data from CHIANTI or ADAS .

The slaves involved in this work are: Rhona Maclean , Eoghan O'Shea , Eamon Scullion , Abhishek Srivastava , David Perez-Suarez and Srividya Subramanian Watch this space!