Abstract
The most ubiquitous structures in the solar corona are loops, often appearing with approximately semi-circular geometry, obviously representing visible manifestations of closed magnetic field lines. The magnetic field is not directly visible in any wavelength, but our knowledge of its topology and geometry is based on our understanding that some field-aligned coronal structures become filled with hot plasma that radiates in EUV and soft X-rays, and this way illuminates selected bundles of magnetic field lines.
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9.1 Coronal Loops: Stereoscopy and 3-D Geometry
The most ubiquitous structures in the solar corona are loops, often appearing with approximately semi-circular geometry, obviously representing visible manifestations of closed magnetic field lines. The magnetic field is not directly visible in any wavelength, but our knowledge of its topology and geometry is based on our understanding that some field-aligned coronal structures become filled with hot plasma that radiates in EUV and soft X-rays, and this way illuminates selected bundles of magnetic field lines. The super-position of myriads of illuminated loops in multi-polar active regions can lead to EUV and soft X-ray images with fairly complex topology, but in principle can be rendered with a suitable 3-D magnetic field model and hydrostatic 1-D loop models for each field line, as demonstrated for active regions observed with SXT/Yohkoh (Gary 1997; Lundquist et al. 2008), or with full-Sun visualizations (Schrijver et al. 2004).
A number of exercises have been conducted to adjust a theoretical magnetic field model to the observed 2-D projections of coronal loops, such as radial stretching of a potential field (Gary and Alexander 1999), varying the α-parameters in linear force-free field models (Wiegelmann and Neukirch 2002), forward-fitting of a series of submerged dipoles (Sandman and Aschwanden 2011), or varying the α-parameters in vertical current approximations of nonlinear force-free fields (Aschwanden 2013). What became clear even in the pre-STEREO era is that the 3-D geometry of observed coronal loops is not consistent with potential fields, as demonstrated for a sample of ≈ 60 loops in an active region observed with SOHO/EIT and reconstructed with the solar-rotation stereoscopy method (Aschwanden et al. 1999, 2000).
The launch of STEREO in 2006 augmented previous solar rotation-based methods with a new opportunity to conduct true stereoscopy, performed with two identical spacecraft with a suitable separation angle. The very first results from EUVI/STEREO/A and B reported the triangulation of ≈ 50 loops viewed at a spacecraft separation angle of ≈ 12∘ (Feng et al. 2007). The stereoscopic 3-D geometry of only ≈ 10 (out of 50) loops could locally be modeled with a linear force-free model, while no model could fit all triangulated loops, leading to the conclusion that linear force-free models are not adequate to explain the observed 3-D geometry of active region loops. Somewhat earlier on, when the STEREO/A and B had a spacecraft separation angle of 7∘, a number of 30 loop structures (7 complete and 23 partial segments) were stereoscopically triangulated (Fig. 9.1), yielding the height range, stereoscopic height measurement errors, the loop plane inclination angles, and measurements of the coplanarity and circularity of the loops (Aschwanden et al. 2008). The loops were found to have large inclination angles from the vertical (θ ≈ 36∘–73∘), curvature radius variations of 3%–30%, and deviations from planarity by 3%–13% of the loop baselines (Fig. 9.2). The knowledge of the exact 3-D geometry of a loop with respect to the observers line-of-sight has important consequences for determining the correct vertical density scale height (used in hydrostatic models), the aspect angle of loop cross-sections (used in inferring electron densities from optically thin emission measures), the absolute flow speeds (used in siphon flow models), the correct loop length (used in loop scaling laws), as well as the 3-D vectors of the coronal magnetic field (used in testing theoretical magnetic field extrapolation models). Extreme deviations from a semi-circular geometry were found in oscillating loops, which appear to have strong helical twist (Aschwanden 2009). Stereoscopic triangulation of coronal loops is feasible from small (\({\;\overset { >}{\scriptstyle \sim }\;}\)6∘) to large angles (\({\;\overset { <}{\scriptstyle \sim }\;}\)170∘) of the spacecraft separation, but the ambiguity in the identification of corresponding loop pairs becomes more severe for large angles \({\;\overset { >}{\scriptstyle \sim }\;}\)30∘ (Aschwanden et al. 2012).
Statistics of geometric parameters is useful for testing physical scaling laws. For coronal loops, which often ressemble slender long structures, we can measure their length L and their width w. The loop lengths range from the smallest detectable size of L min ≈ 1 Mm to the size of the largest active region, L max \({\;\overset { <}{\scriptstyle \sim }\;}\)250 Mm, so they cover at least two orders of magnitude in scale, generally outlining incomplete segments of magnetic field lines.
9.2 Coronal Loops: Cross-Sectional Widths
The reduction from 3-D to 1-D hydrodynamics in coronal loops requires the definition of a cross-sectional dependence of a flux tube area A(s) as a function of the loop length coordinate s, which is assumed to be constant in the simplest case. Another fundamental assumption is the monolithic structure of coronal loops, which is likely to break down for large loop widths. It is therefore imperative to measure the width of coronal loops with high-resolution instruments and to test their homogeneity (in the case of monolithic loops) or inhomogeneity (in the case of multi-stranded loops).
Cross-sectional widths of coronal loops have been measured with many different instruments (Dunn/SacPeak, Pic du Midi, Skylab, NRAO, VLA, ASE rocket, CSIRO, LMSAL rocket, SXT/Yohkoh, EIT/SOHO, TRACE, EIS/Hinode, CRISP, AIA/SDO, Hi-C, SOT/Hinode, IRIS) and wavelengths (optical, Hα, Lyα, EUV, soft X-rays, and radio). A compilation of 53 studies on loop width measurements is depicted in Fig. 9.3, showing the loop widths (on the x-axis) sorted by increasing widths (on the y-axis). The numbered references are listed in the original paper (Aschwanden and Peter 2017), from which we cite the most recent ones with the highest spatial resolution only (after 2010): Aschwanden and Wülser (2011 [37]); Aschwanden and Boerner (2011 [38]); Aschwanden and Schrijver (2011 [39]); Aschwanden et al. (2013 [43]); Mulu-Moore et al. (2011 [40]); Brooks et al. (2012 [41], 2013 [45], 2016 [51]); Antolin and Rouppe van der Voort (2012 [42]); Peter et al. (2013 [44]); Winebarger et al. (2013 [46], 2014 [49]); Morton and McLaughlin (2013 [47]); Alexander et al. (2013 [48]); Antolin et al. (2015 [50]); Tiwari et al. (2016 [52]); Aschwanden and Peter (2017 [53]).
The graphical representation in Fig. 9.3 divides the loop width measurements into 4 wavelength regimes by color (optical + Hα + Lyα, EUV, soft X-rays, and radio), and ranks the width ranges by the smallest detected width in ascending order. There are several trends visible in Fig. 9.3. Minimum loop widths have been measured from w ≈ 20 Mm down to w min ≈ 0.1 Mm. The finest loop widths have been detected preferentially in EUV, while the loop widths measured in soft X-rays and optical wavelengths tend to be significantly larger, and are found to be largest in radio wavelengths. Since coronal loops in EUV and soft X-rays are produced by optically thin line emission, the density contrast of individual loops is much “crisper” than in structures detected in the optically thick regime of free-free and gyroresonance emission in radio wavelengths.
In Fig. 9.3 we can see also that the smallest loop widths are typically measured approximately at 2–4 pixels above the instrumental pixel sizes, which is partially explained by the point spread function that typically amounts to w psf ≈ 2.5 pixels in most EUV imagers (TRACE, AIA/SDO, STEREO, IRIS, Hi-C). Some additional scatter in the order of w noise ≈ 1 pixel is due to the noise in the background subtraction, so that the observed loop width w is broadened by,
if we add the uncertainties in quadrature. We may ask whether the distribution of loop sizes continues at the low end, if future instruments faciliate higher spatial resolutions. However, several studies with the highest available spatial resolution, with a pixel size of w pixel ≈ 0.1′′≈ 70 km for the Hi-C instrument, have demonstrated that AIA resolves many of the loops, as shown in Fig. 9.4. The smallest loops measured from recent Hi-C studies cover ranges of w = 200–1500 km (Peter et al. 2013), w = 117–667 km (Brooks et al. 2013), w = 150–310 km (Morton and McLaughlin 2013), w = 120–150 km (Brooks et al. 2016), with a most frequent width of w ≈ 500 km (Aschwanden and Peter 2017).
There is no widely accepted theoretical model for the cross-sectional widths of coronal loops. The intrinsic loop widths supposedly reveal the cross-sectional area over which energy is deposited in a magnetic flux tube during an elementary heating event. However, since the basic coronal heating mechanism is still elusive, one can not predict the range of loop widths. Parker’s nanoflare scenario envisions unresolved loop strands, while heating mechanisms with cross-field diffusion in a high-β regime predict monolithic resolved loops (Fig. 8.8). If the latest Hi-C measurements with finite loop widths with a most frequent value of w ≈ 500 km hold up, we have to conclude that nanoflare strands with widths w \({\;\overset { <}{\scriptstyle \sim }\;}\)500 km are negligible in the energy budget of the heating process. The particular value of w ≈ 500 km apparently demarcates two types of granulation in the solar photosphere: the mini-granulation with a width range of w ≈ 100–600 km (Abramenko et al. 2012), and the regular granules which have a Gaussian distribution with a mean of w ≈ 1000 km.
9.3 Coronal Loops: Multi-Strand Structure
Hydrodynamic modeling of coronal loops during the last two decades has been generalized from a single flux-tube concept to a multi-stranded macroscopic loop system, which has a number of consequences: (1) the observed macroscopic loops may indeed consist of finer unresolved strands, in particular for instruments with poor spatial resolution, which makes the measured physical parameters instrument-dependent (Fig. 9.5); (2) modeling a multi-stranded loop system introduces additional degrees of freedom (such as filling factors) that makes the interpretation of observables more ambiguous; and (3) the discrimination between homogeneous (monolithic) single loops and the inhomogeneous (multi-stranded) loop systems is tied to macroscopic versus microscopic coronal heating mechanisms, similar to the dichotomy between large-scale flares (for which we resolve the magnetic reconnection geometry) and nanoflares (which we do not resolve). Observationally, the majority of loops measured with arcsecond resolution instruments (TRACE, AIA) were found to be isothermal (Aschwanden and Nightingale 2005), which is consistent with resolved single loop strands, rather than with multi-stranded loop structures (unless all strands have the same temperature).
Let us review a few lessons we learned from multi-strand loop modeling and observations. The flat temperature profile along coronal loops can be reproduced by both a footpoint-heated monolithic loop or by an ensemble of uniformly heated loops (Reale and Peres 2000), as well as by an ensemble of footpoint-heated loops (Mendoza-Briceno et al. 2002). The discrepancy between the observed decay times of warm loops and the theoretical lifetime inferred from time-dependent hydrostatic simulations can be reconciled with a multi-strand system (Fig. 9.6), while it fails for most monolithic loops (Warren et al. 2002, 2003). Electron density and temperature diagnostics does not discriminate between the spatial form of the heating function in multi-strand (nanoflare) hydrodynamic simulations (Patsourakos and Klimchuk 2005; Sarkar and Walsh 2008, 2009). The temperature of the cold corona (T e ≈ 1.0–1.5 MK) as well as the fuzziness of the warm corona (T e ≈ 2–3 MK) can be reproduced with nanoflare simulations in a multi-strand corona (Reale et al. 2005, 2011; Guarrasi et al. 2010). Multi-strand hydrodynamic simulations produce modest line broadening (e.g., Ne VII and Mg X) that is consistent with observations (Patsourakos and Klimchuk 2006; Taroyan et al. 2006). Nonthermal widths of hot loops (1–4 MK) measured in non-flaring regions did reveal only small nonthermal velocities (v = 17.6 ± 5.3 km s−1) (Brooks et al. 2016). Multi-stranded loop models cannot reproduce both the transition region DEM distribution and the coronal DEM distribution with a unique set of parameters (Susino et al. 2010, 2013; Reale and Ciaravella 2006; Winebarger et al. 2011; Mulu-Moore et al. 2011). Hi-C observations (Fig. 9.4) over-resolve some single loops, which have cross-sectional widths of w ≈ 100–500 km (Peter et al. 2013), implying that most loops with a width of w \({\;\overset { >}{\scriptstyle \sim }\;}\)500 km are likely to be composite or multi-stranded loops (Aschwanden and Peter 2017). Other nanoflare simulations determine filling factors (Jain and Yashiro 2002), spontaneous current sheets in filamentary loop systems (Petrie 2006), statistical models of the inhomogeneous corona (Aschwanden et al. 2007), the effects of filter-ratio analysis on the flat temperature profile in multi-stranded loop models (Bourouaine and Marsch 2010), the multi-thermal and multi-stranded nature of coronal rain (Antolin et al. 2015), or the effects of low-frequency versus high-frequency nanoflare heating (Bradshaw and Klimchuk 2015).
9.4 Coronal Loops: Cross-Sectional Temperature
The 1-D flux tube concept of a coronal loop in principle implies a homogeneous electron pressure, density, and temperature across the loop cross-section. In order to verify the cross-sectional temperature structure of coronal loops, multi-wavelength images observed with EIT/SOHO, TRACE, and AIA/SDO have been analyzed in great detail. The main question focused on the discrimination between monolithic (isothermal) and unresolved multi-stranded (multi-thermal) loop cross-sections. Monolithic (macroscopic) loops are by definition homogeneous in temperature and density across their cross-section, and thus require cross-field transport of plasma from a heating source that is spatially resolved with current instrumentation. In contrast, multi-stranded loop cross-sections are inhomogeneous in temperature and density. They display a broad multi-temperature (differential emission measure) distribution, because the unresolved strands are independently heated by microscopic heating sources, as envisioned in the original nanoflare heating scenarios.
How is the temperature structure measured across a coronal loop or multi-stranded loop system ? In the simplest method, a loop segment has to be identified in an image data set with (n λ) multiple wavelengths, which yields a set of fluxes F i, i = 1, …, n λ to which a differential emission measure (DEM) analysis is applied (see Sect. 2.6 and Table 2.3 for an overview of different DEM methods). The outcome of the DEM analysis yields then either a narrow (ΔT∕T) ≪ 1 or a broad DEM distribution (ΔT∕T ≈ 1). Narrow temperature peaks indicate a near-isothermal structure, while broad DEMs imply a multi-thermal distribution. There are a number of systematic effects that can make the results ambiguous. For instance, if an instrument has a poor spatial resolution, a bundle of closely-spaced loop strands appear as a single loop, which constitutes a strong bias for a broad multi-thermal structure. Moreover, if a loop is observed near or beyond the limb, the observed loop flux is likely to be contaminated by large foreground and background fluxes, which creates a bias for broad multi-thermal structures, since the target loop and the background are likely to have different temperatures. Therefore, clean results depend very much on the availability of high-resolution instruments, an accurate DEM inversion method, and careful background modeling. A selection of results on the thermality of loop cross-sections is provided in Table 9.1.
A number of criticisms have been raised concerning the various used DEM analysis methods, such as: (1) over-restricted temperature range, i.e., EIT with T ≈ 1–2 MK (Schmelz et al. 2003); (2) atomic lines missing in the CHIANTI code, e.g., in the 94 Å band (Aschwanden and Boerner 2011; Del Zanna 2013; Landi and Klimchuk 2010); (3) insufficient spatial resolution, i.e. CDS/SOHO data with a point-spread function of 6′′× 8′′ (Schmelz 2002; Schmelz et al. 2001, 2003, 2005, 2007, 2009; Del Zanna 2003; Del Zanna and Mason 2003; Cirtain et al. 2007); (4) the ambiguity of the 2-filter-ratio technique (Weber et al. 2005; Martens et al. 2002); (5) the lack of background subtraction (Schmelz et al. 2001; Schmelz 2002); (6) over-smoothing of the fitted DEM function (Schmelz et al. 2001; Aschwanden 2002; Landi and Feldman 2008); (7) isothermal bias for over-estimates of the photometric uncertainty (Patsourakos and Klimchuk 2007); or (8) the choice of the radiative loss function (Reale and Landi 2012; Sasso et al. 2012). What matters additionally is the dynamical condition of a loop: quiescent active region loops often exhibit a narrow (near-isothermal) DEM (if they are spatially resolved), while flaring loops tend to exhibit broadband (multi-thermal) DEMs (e.g., Warren et al. 2013). A statistical rule-of-thumb was found that elementary loop strands: (i) are near-isothermal (ΔT \({\;\overset { <}{\scriptstyle \sim }\;}\)0.2 MK), (ii) have a small width (w ≤ 2 Mm), and (iii) have a faint contrast (\({\;\overset { <}{\scriptstyle \sim }\;}\)30%) (Aschwanden 2005). Comparing the 27 studies listed in Table 9.1 it appears that isothermal (or near-isothermal) loops are more likely to be detected at “warm coronal temperatures” (T ≈ 1–2 MK), using instruments with the highest spatial resolution (TRACE with 0.5′′ and AIA with 0.6′′ pixels), and after proper background subtraction. Loops or multi-strand loop systems are also detected at hotter (flare-like) temperatures (T ≈ 3–30 MK), with instruments that have soft X-ray coverage (SXT, CDS, EIS, XRT). However, since these instruments have a relatively poor spatial resolution and often were analyzed without background subtraction, we can not decide whether hot loops are isothermal or multi-thermal.
9.5 Coronal Loops: Flows
Plasma flows in coronal loops require a generalization of static models (with velocity v = 0) in the 1-D hydrodynamic equations, enabling the calculation of simple steady-flow solutions (v = const), as well as siphon-flow solutions, which are driven by a pressure imbalance between the loop footpoints. An essential feature of steady flow solutions is their acceleration with increasing height (because the electron density decreases due to gravitational stratification and momentum conservation), which can exceed the sound speed and become supersonic and form stationary shocks. There is a wealth of flow patterns that can occur in the solar corona, such as blueshifted upflows, redshifted downflows, siphon flows, turbulent flows, shocks generated by critical or supersonic flows, reconnection inflows, reconnection outflows, etc. In the following we will review new measurements (Table 9.2) and hydrodynamic modeling after 2000, which were mostly obtained with EIS/Hinode and AIA/SDO.
The interpretation of the Dopplershift of flows depends very much on the heliographic position. Near disk center we expect a maximum blueshift for upflows, which should vanish when seen near the limb. Such a center-to-limb pattern in the directivity was indeed observed in upflows (v ≈ 20 km s−1) near the footpoints of active region loops with EIS/Hinode (Hara et al. 2008; Doschek et al. 2008), persistent for at least a day (Doschek et al. 2008), and extending into the heliosphere and solar wind (Doschek et al. 2008). The center-to-limb variation introduces systematic changes in the line shift, from which the inclination and angular spread can be measured (Démoulin et al. 2013; Baker et al. 2017). Besides persistent blueshifted upflows (Patsourakos et al. 2014), persistent redshifts were observed near loop footpoints in active regions too (Del Zanna 2008). This apparent co-spatial co-existence of blueshifted outflows and redshifted downflows was disentangled as two different temperature regimes: redshifted emission at transition region temperatures and blueshifted emission at coronal temperatures (Tripathi et al. 2009; Warren et al. 2011; Kamio et al. 2011). This dichotomy of flows was called “coronal contra-flow” or “chromosphere-corona mass cycle” (McIntosh et al. 2012). The emission in the blue wing was found to propagate upward fast (v = 50–150 km s−1) and to contribute a few percents to the total emission only, while the “draining” of cooler material descends slowly (v ≈ 10 km s−1) while radiatively cooling (McIntosh et al. 2012), forming a complex near-cospatial mass cycle. Upflows with velocities of v = 48 km s−1 forming loops with life times of 4 hrs were also observed in optical wavelengths (Singh et al. 2005). Strong blueshifts of v ≈ 20–40 km s−1 were measured in the solar corona during a total eclipse (Raju et al. 2011). Other velocity measurements in upflows and downflows were reported also by Brosius (2005), Brosius and Landi (2005), Tripathi et al. (2012a), Orange et al. (2013), Kano et al. (2014), see compilation in Table 9.2. Most of the observed upflow events have been interpreted as a result of a local magnetic reconnection process that triggers chromospheric evaporation. Using magnetic extrapolations in the upflow regions, it was found that flows occur in thin, fan-like structures rooted in quasi-separatrix layers, between over-pressure active region loops and neighboring under-pressure loops (Démoulin et al. 2013).
On the theoretical side, 1-D hydrodynamic simulations have been carried out to calculate steady-flow solutions, but observational evidence is scarce. It was found that a sufficiently large heating asymmetry can produce the observed loop over-density (Winebarger et al. 2002), but very short pressure scale heights are needed, so that most of the warm (T = 1–2 MK) EUV loops cannot be explained by flows (Patsourakos et al. 2014). A transient motion along a cool loop observed with TRACE and SUMER has been modeled in terms of a siphon flow model, but the transient lasted only a few minutes, which is much shorter than expected for quasi-steady siphon flows (Doyle et al. 2006). The observed flows in a loop structure located in the penumbra of a sunspot were found to match theoretical predictions of chromospheric and coronal siphon flows, with accelerating upflowing plasma at one footpoint with low field strength and decelerating downflowing plasma at the other end (Fig. 9.7), possibly forming a tube shock (Bethge et al. 2012). High-velocity flows can be generated by the generalized magneto-Bernoulli mechanism (Mahajan et al. 2002). Multi-species hydrodynamic simulations show the Coulomb coupling of the electrons and ions induces drag that counteracts the tendency of ions to settle into gravitational stratification (Lenz 2004). Ions and protons couple well in the line-forming region (Byhring et al. 2008). The coronal helium is found not to “drain”, leading to extreme increases of the helium abundance from the upper chromosphere to the corona (Killie et al. 2005).
9.6 Coronal Loops: Catastrophic Cooling
Hot coronal loops (T e \({\;\overset { >}{\scriptstyle \sim }\;}\)3 MK) mostly cool by conductive energy loss, while radiative energy loss dominates later on (in warm loops with T e ≈ 1–3 MK). At even lower loop temperatures (T e < 1 MK), radiative losses are no longer balanced by gains through heat conduction or in-situ heating, and therefore the radiatively-driven thermal instability sets in. This phase of the loop evolution is called “catastrophic cooling” or “condensation”. During this condensation phase, cold plasma blobs collapse and fall from the corona back to the chromosphere, a phenomenon that is also called “coronal rain”, which is observed in active regions, post-flare loops, eruptive filaments, and prominences (see examples in Fig. 9.8).
Recent observations of coronal rain with the CRISP instrument at SST in the H-α and Ca II H wavelengths quantify the dynamics (average falling speeds of v ≈ 70 km s−1 and mass drain rate of dm∕dt ≈ (1.5–5) × 109 g s−1), geometric shapes (average lengths of L ≈ 710 km and widths of w ≈ 310 km), trajectories (along the magnetic field, with fall times of τ ≈ 1–10 min), and thermodynamic properties (average temperatures T e < 7000 K) and densities (n e ≈ (0.2–2.5) × 1011 cm−3) of the condensations (Antolin and Rouppe van der Voort 2012; Antolin et al. 2015). The formation of flare-driven coronal rain was observed in 5 phases: heating, evaporation, conductive cooling for ≈ 2 min, radiative enthalpy cooling for 1.3 hrs, and catastrophic cooling during 0.6–2.0 min, leading to rain strands with periods of 55–70 s (Scullion et al. 2016). These measurements confirm that the acceleration is largely below the effective gravity along loops, and that the trajectories follow the coronal magnetic field. The maximum descending speed was found to be correlated with the ratio of electron densities inside and outside the falling blobs (Oliver et al. 2016). While the falling of coronal condensations is easiest observed above the limb, the phenomenon is also found “on-the-disk”, with similar physical parameters (Antolin et al. 2012; Ahn et al. 2014), which could explain also part of the ubiquitous redshifts observed on the disk. Combining the CRISP/SST measurements with AIA and IRIS, coronal rain is found to be highly multi-thermal and multi-stranded, with a high degree of co-spatiality in the multi-wavelength (optical and EUV) emissions (Antolin et al. 2015). The funneling effect of the upward diverging magnetic field streamlines the coronal rain into a more continuous and persistent stream at low altitudes, just before it impacts the chromosphere (Antolin et al. 2015).
Recent numerical 1-D hydrodynamic simulations of the condensation of plasma in cool (T e < 1 MK) short loops (L = 10 Mm) exhibit a cyclic pattern of chromospheric evaporation, condensation, motion of the condensation region to either side of the loop, and finally loop reheating with a period of 1–2 hrs (Müller et al. 2003). It is found that the radiatively-driven thermal instability occurs about an order of magnitude faster than the Rayleigh-Taylor instability, which can occur in a loop with a density inversion at its apex also (Müller et al. 2003). Simulations with different heating functions reveal that the process of catastrophic cooling is not initiated by a drastic decrease of the total loop heating rate, but rather results from a loss of equilibrium at the loop apex as a natural consequence of (even steady) footpoint heating (Müller et al. 2004; Peter et al. 2012). In the case of repetitive impulsive heating, the cycle period to maintain a short loop at coronal temperatures is very sensitive to the loop length, for instance T cycle ≈ 3 min for L = 5–10 Mm (Mendoza-Briceno et al. 2002).
Much longer cycles, with periods of T = 3.8–9.0 hrs (lasting over several days), where found in some active region loops, which were interpreted in terms of thermal non-equilibrium evaporation and condensation cycles also (Froment et al. 2015, 2017). The time evolution of plasma temperatures T(t) and emission measure EM, as well as phase diagrams of T − EM, are shown in Fig. 9.9 for three cases (with mean periods of 3.8, 5.0, and 9.0 hours).
Periodically repeating heating-condensation cycles were found to be coupled with transverse kink-mode oscillations in some active region loops (Kohutova and Verwichte 2016, 2017a,b; Verwichte and Kohutova 2017; Verwichte et al. 2017), see Fig. 9.10.
9.7 Coronal Loops: Heating Function
The heating function term E h(s, t) in the hydrodynamic energy equation has (a generally unknown) time and spatial dependence. In 1-D hydrodynamic flux tube models (with loop length coordinate s), which is often approximated assuming an adiabatic state, the energy balance is given by (e.g., Rosner et al. 1978),
Here E h is the volumetric heating rate, E c is the conductive energy loss rate, and E r is the radiative energy loss rate. The three most common spatial heating functions of loops are the uniform, footpoint, and apex heating functions. The spatial shape of the nonuniform heating function is generally parameterized with an exponential function (e.g., Serio et al. 1981), and the time dependence has been approximated with a Gaussian function,
were t m is the time of maximum heating, τ heat the gaussian width of the heating time interval, s H is the heating scale height, and H 0 is the volumetric heating rate at the footpoint.
One obvious case we can rule out at this stage is the uniform heating function (constant in space and time), because it would not be able to explain the observed over-density of cool loops in EUV (Lenz et al. 1999; Aschwanden et al. 1999, 2000). None of the heating function approximations fits the observed density profiles derived from DEM forward-fitting or inversions, which created a new conundrum that violated previous steady-state models. Besides the over-density with respect to the RTV steady-state solution, EUV loops were found to reveal super-hydrostatic scale heights and exceptionally flat temperature profiles. These critical loop properties led to the diagnostic decision tree as shown in Fig. 9.11. The ratio of the radiative to the conductive cooling time,
was found to vary over orders of magnitude for cool and hot coronal loops (Fig. 9.12), but can be reproduced with simulations of impulsively heated loop strands (Klimchuk 2006, 2009).
Another case that is unlikely is the loop apex heating scenario. Although a statistical temperature increase is generally observed in the corona above the limb, which has been interpreted in terms of a temperature profile of a single loop that is heated from the top (Reale 2002), this temperature gradient is more naturally explained in terms of the hydrostatic weighting bias in an inhomogeneous solar corona (Aschwanden and Nitta 2000). Consequently, only the case of footpoint heating survives as a realistic spatial heating function of coronal loops.
For the temporal dependence, delta-functions, rectangular, triangular, or Gaussian functions have been employed. Fortunately we have additional constraints that restrict the time-dependence of the heating function in loops, namely the observed life time (or decay time) of a loop, which has to match the cooling time as obtained in hydrodynamic simulations. However, hydrodynamic simulations of the time evolution of coronal loops exhibited that the simulated life times of loops were found to be always shorter than the observed life times (Warren et al. 2002, 2003), which led to the conclusion that a sequence of subsequentially (overlapping and superimposed) heating episodes only can explain the observed time evolution of active region loops (Fig. 9.6), so that an active region loop consists of a collection of small-scale strands (or filaments) that are impulsively heated and are cooling through the EUV passbands (Warren et al. 2002, 2003; Winebarger et al. 2003; Mulu-Moore et al. 2011). While the decay time discrepancy is based on multi-stranded loops observed with TRACE, it has not been tested yet whether monolithic loops with finer widths exhibit the same decay time discrepancy, such as the finest loops discovered in Hi-C data down to w ≈ 100–500 km (Peter et al. 2013; Brooks et al. 2013; Aschwanden and Peter 2017; see Figs. 9.4 and 9.5). Multi-stranded hydrodynamic models have also difficulty to reproduce the diffuse hot plasma in an active region (Warren et al. 2010a). On the other side, steady-state heating was found to be consistent with hot loops observed with XRT in the core of active regions, as well as with “moss” structures at the footpoint of high-temperature loops (Warren et al. 2010b).
Special cases of the heating function have been simulated: the explosive heating scenario with very fast heating to high temperatures, which leads to near-saturated thermal conduction (Bradshaw and Cargill 2006, 2013); simulations with nonuniform loop cross-section areas, nonuniform heating, asymmetric loop shapes, and asymmetric heating (Mikic et al. 2013); periodic and overlapping heating pulses that mimic quasi-steady heating (Testa et al. 2005); heating pulses in a multi-stranded system randomly distributed in time (Patsourakos and Klimchuk 2006; Guarrasi et al. 2010); or turbulent heating rates (Chae et al. 2002).
9.8 Coronal Loops: The 0-D EBTEL Code
The hydrodynamics of the solar corona is generally simplified in terms of one-dimensional (1-D) flux tubes that represent rigid conduits for plasma flows, since the plasma-β parameter is less than unity in most coronal regions, which implies that the magnetic pressure exceeds the thermal pressure and thus forms impenetrable flux tubes without cross-field transport. The reduction of the coronal hydrodynamics to a 1-D problem can further be simplified to a 0-D problem, since thermal conduction and flows tend to smooth out plasma gradients along the magnetic field. An efficient 0-D hydrodynamic code, called the “enthalpy-based thermal evolution of loops” (EBTEL) code has been developed that approximately describes the evolution of the average temperature, pressure, density, and differential emission measure (DEM) distribution inside a coronal loop strand, where the enthalpy plays a major role in the energy budget (Klimchuk et al. 2008; Cargill et al. 2012a,b). The motivation for creating such an efficient hydrodynamic code came from the desire to model coronal loops as a superposition of thousands of (observationally unresolved) miniature loops, also called “elemental loop strands”, as they are invoked in nanoflare heating models.
We outline the derivation of the 0-D hydrodynamic EBTEL model according to Klimchuk et al. (2008). The 1-D time-dependent hydrodynamic equation for energy conservation is,
where E is the combined thermal and kinetic energy density (defined as E = P∕(γ − 1) in terms of the adiabatic index γ in Cargill et al. 2012a),
s is the spatial coordinate along the magnetic field, n is the electron number density, T is the electron temperature, P is the total pressure, v is the bulk velocity, F c is the conductive heat flux, Q is the volumetric heating rate (equivalent to E H(s, t) in Sect. 9.7), g ∥ is the gravity component along the magnetic field, and Λ(T) is the optically thin radiative loss function. The usual assumptions of 1-D hydrodynamic codes are applied, such as symmetric loops and constant loop cross-sections, which are still a matter of debate. Furthermore, neglecting the kinetic energy (assuming subsonic flows) and gravity terms (for loops shorter than the gravitational scale height), we obtain,
Integrating Eq. (9.8.3) over the loop length L and applying a vanishing velocity and heat flux at the apex due to the loop symmetry, we obtain,
where L is the coronal loop half length, the quantities 〈P〉 and 〈Q〉 indicate spatial averages along the coronal loop section, P 0 is the pressure and v 0 is the velocity at the footpoint of the loop (at the base of the corona), (5∕2)P 0 v 0 is the enthalpy flux, F 0 is the heat flux, and R c ≈〈n 2〉Λ(〈T〉)L is the radiative cooling rate per unit cross-sectional area in the corona. A similar averaging can be applied to the transition region,
where l is the length from the coronal base to the apex, and R tr is the radiative cooling rate in the transition region. Assuming that the enthalpy flux is proportional to the temperature, therefore being much smaller at the top of the chromosphere than in the corona, i.e., l ≪ L, it can be ignored in Eq. (9.8.5), leading to,
In static equilibrium, the heat flux and radiative power is balanced, i.e., |F 0| = R tr, which yields with Eqs. (9.8.4) and (9.8.6),
This equation reflects the energetics of the combined corona and transition region system, with a source term 〈Q〉 and loss term (R c + R tr)∕L.
After we quantified the pressure evolution ∂〈P〉∕∂t we want to derive the density evolution ∂〈n〉∕∂t, which is obtained by setting the time derivative of the electron column density 〈n〉L equal to the flux of electrons through the coronal base, i.e., ∂(〈n〉L)∕∂t = J 0 ≈ nv, and using the ideal gas law P = 2k B nT,
where the constants refer to the temperature ratios c 2 = 〈T〉∕T a and c 3 = T 0∕T a, T a being the apex temperature, and T 0 the coronal base temperature. The classical expression for the heat flux is
Combining then Eqs. (9.8.7) and (9.8.8) with the ideal gas law leads then to the temperature evolution ∂〈T〉∕∂t,
Similarly, the plasma velocity at the base of the corona can be obtained from the electron flux J 0,
The numerical EBTEL code uses the three evolutionary equations for the pressure (Eq. 9.8.7), the density (Eq. 9.8.8), and the temperature (Eq. 9.8.10) to calculate the time evolutions P(t), n(t), T(t) in incremental time steps, starting from some initial conditions at time t = 0. An example of such a time-dependent 0-D solution is shown in Fig. 9.13, which is compared with a classical 1-D hydrodynamic solution using the Adaptive Refined Godunov Solver (ARGOS) code (Antiochos et al. 1999), demonstrating an agreement within ≈ 20% in most time steps. The EBTEL code contains some variable parameters that can be adjusted based on 1-D hydrodynamic simulations, such as c 1 = R tr∕R c = 4.0, c 2 = 〈T〉∕T a = 0.87, and c 3 = T 0∕T a = 0.5. Modifications of the EBTEL code include the energy flux and particle flux of nonthermal electron beams (Klimchuk et al. 2008). Generally, the differential emission measure (DEM) distributions computed with the EBTEL code, using the scenario of strong evaporation (by thermal conduction only) and strong condensation (when the heat flux is much less than the radiative losses), are not valid when nonthermal particles are important, such as in the case of beam-driven evaporation during solar flares. A key advantage of the 0-D EBTEL code is that it requires about four orders of magnitude less computation time than traditional 1-D hydrodynamic codes (such as ARGOS).
Improvements of the EBTEL model include gravitational stratification, a physically motivated treatment of radiative cooling (Cargill et al. 2012a), and nonequilibrium ionization (Bradshaw and Klimchuk 2011). Comparisons of the EBTEL code with other 0-D hydrodynamic models (Kuin and Martens 1982; Kopp and Poletto 1993; Cargill 1994; Fisher and Hawley 1990; Aschwanden and Tsiklauri 2009) have been conducted in Cargill et al. (2012b). Applications of the EBTEL code to solar flare data involves EIS/Hinode and AIA/SDO observations (e.g., Raftery et al. 2009; Ugarte-Urra and Warren 2014; Viall and Klimchuk 2012).
9.9 Coronal Loops: 1-D Hydrodynamics
1-D hydrodynamic codes have been the work horse for modeling of coronal loops or prominences for several decades. The one-dimensionality is a natural consequence of the fact that coronal plasma can only follow the magnetic field lines in the low plasma-β corona. All parameters in 1-D flux tubes have a dependence on the 1-D spatial coordinate s, as well as on the time t, such as the electron temperature T(s, t), the electron density n(s, t) or mass density ρ(s, t) = m p n(s, t), the velocity v(s, t), the heating rate Q(s, t), the conductive flux F c(s, t), the pressure P(s, t), the internal energy E(s, t) = (3∕2)P(s, t) + (1∕2)ρ(s, t)v 2(s, t), and the radiative loss rate E r(s, t) = n 2(s, t)Λ(T(s, t). A hydrodynamic code, such as the ARGOS code (Antiochos et al. 1999), solves the time evolution of these parameters from the transport equations for mass, momentum, and energy in a 1-D plasma,
where the conductive flux F c is,
with κ = 9.2 × 10−7 (erg s−1 cm−1 K−7∕2) the classical Spitzer conductivity. The least known parameter is the spatio-temporal heating function Q(s, t), for which various parameterizations have been used to mimic uniform, footpoint, or apex heating (Sect. 9.7). There exist also various parameterizations of the radiative loss function Λ(T), usually approximated by piece-wise power law functions. While numerical codes have been designed to solve the coupled equation system of Eqs. (9.9.1–9.9.4), attempts have been made to simplify the analytical function that approximates the radiative loss function (e.g., Landini and Landi 2002; Dudik et al. 2009; Martens 2010; Bradshaw 2008), to specify various shapes of the spatial heating function (Serio et al. 1981), to quantify analytical approximations of the numerical solutions (Aschwanden and Tsiklauri 2009), or to include nonequilibrium ionization (e.g., Bradshaw and Mason 2003, Bradshaw 2008).
The radiative loss function Λ(T) is generally approximated with piece-wise power law functions, following the initial characterization by Rosner et al. (1978). An alternative form is used by Landini and Landi (2002),
with C ≈ 2 × 1012 K5∕2 cm3 s−1 erg−1, based on radiative loss calculations in an optically thin plasma using the Arcetri Spectral Code in the 104–108 K temperature range (Landi and Landini 1999). Similarly, Martens (2010) characterizes the radiative loss function with a power law function
where χ 0 = 1012.41 is in cgs-units, while the heating function is rendered with a similar power law relation,
This parameterization makes the energy equation (Eq. 9.9.3) integrable and an analytical solution is obtained for the hydrostatic temperature profile T(s) and the RTV-type scaling law \(P_0 L \propto T_{max}^3\), for a selection of heating functions Q(s), as well as for a loop cross-section that is expanding with height (Martens 2010). A similar power law approach is used in analytical models of static coronal loops by Dudik et al. (2009), namely
with a coefficient of σ = −1∕2 (Kuin and Martens 1982). In numerical models one can also interpolate the values calculated with an atomic data base, e.g., CHIANTI (see Sect. 2.3).
An analytical approximation of the temperature profile T(s) can be obtained by neglecting the radiative loss during the initial heating phase (Aschwanden and Tsiklauri 2009), so that the heating rate Q(s) essentially balances the conductive loss rate ∇F c(s), which yields a differential equation of second order in the spatial coordinate s,
This second-order differential equation can be turned into an double-integral equation by expressing it as an explicit function of T(s),
which yields the following solution for the case of uniform heating,
The evolution of the electron density n(t) in the loop can be understood in terms of the Neupert effect, which in essence states that the accumulated density in a heated loop is an integral function of the heating rate, because the chromospheric evaporation rate into the coronal loop is a function of the chromospheric heating rate or energy input. If we neglect cooling during the heating phase, free energy is continuously added to the loop in form of evaporating material, which increases the density in the loop monotonously, peaking at the end of the heating phase. Parameterizing the heating function Q(t) with a Gaussian function yields a Gaussian temperature profile T(t) ∝ Q(t), while the density function follows the integral of the Gaussian function, \(n(t) \propto \int Q(t) ds\), which predicts a maximum of the density function n(t) at approximately the half decay time of the heating function, as sketched in Fig. 9.14. The analytical approximations of the temperature T(t) and density profiles n(t) have been found to agree well with numerical hydrodynamic simulations (Aschwanden and Tsiklauri 2009), as shown in Fig. 9.14. A typical characteristic of the temperature-density phase diagram (Fig. 9.14, right panel) is the hysteresis curve of the density peak lagging behind the temperature peak, following the Jakimiec power law relationship,
which was found to scale approximately with a power law slope of ≈ 2, as found in many earlier hydrodynamic simulations (e.g., Jakimiec et al. 1992; Serio et al. 1981; Sylwester et al. 1993).
While most hydrodynamic simulations of coronal loops assume ionization equilibrium, this assumption has been scrutinized by solving the detailed ionization balance equation for each ion of the fifteen most abundant elements of the solar atmosphere for the case of a cooling loop (Bradshaw and Mason 2003). The ionization balance equation for each ion is,
where Y i denotes the fractional population of ion level i of element Y , the coefficients I i and R i are the ionization and recombination rates from/to ion level i, n is the electron number density, t is the time, and s is the spatial location along the loop. Significant deviations from equilibrium are found in the coronal and footpoint regions of the loop, especially in low-density coronal regions that cause the recombination rate to be rarer. For another case of a loop subjected to transient heating near the apex, an up to 5 times lower plasma emissivity is found in equilibrium compared with nonequilibrium emissivity, almost entirely due to the response of the coronal Fe ions (Bradshaw and Mason 2003).
9.10 Coronal Loops: Magnetic Modeling
Some new developments of magnetic field modeling in active regions are described in Sect. 8.1. It was realized that none of the magnetic field extrapolation methods warrants that the theoretically calculated field lines match the the observed geometry of coronal loops, as observed in EUV or in soft X-rays. Since the plasma β-parameter in the solar corona is generally less than unity, coronal loops visible in EUV or soft X-rays are supposed to trace the coronal magnetic field. There are two new strategies that take the observed loop geometry into account: (i) stereoscopic triangulation (which became feasible with the STEREO mission), and (ii) automated loop tracing in EUV and soft X-ray images, which both provide stringent constraints for 3-D modeling of the coronal magnetic field.
Since it was recognized that the photosphere and lower chromosphere are generally not force-free (Metcalf et al. 1995), the force-free extrapolation of coronal magnetic field lines from a non-force-free lower boundary, which is the modus vivendi for non-linear force-free field (NLFFF) codes using photospheric magnetograms (or vector data), the accuracy of NLFFF codes became questionable. A refinement of the NLFFF optimization method was proposed by introducing a weighting function that minimizes the force balance between the non-force-free photosphere and the force-free lower boundary of the computation box, which is a magneto-hydrostatic approach (Wiegelmann 2004). Well-posed boundaries are studied in Amari et al. (2006). A method of preprocessing was developed which drives the observed non-force-free data towards suitable boundary conditions for force-free extrapolation codes, minimizing the force balance and the torque-free condition (Wiegelmann et al. 2006; Metcalf et al. 2008; Wiegelmann et al. 2012). A benchmark test of 9 different NLFFF codes (including optimization, magneto-frictional, Grad-Rubin based, and Green’s function-based methods) has been arranged in Schrijver et al. (2006), which demonstrated that the agreement is always best in the lower central region of the volume, where the field and electrical currents are strongest and the effects of boundary conditions weakest, while the solutions in the outer domains show a high sensitivity on the specific boundary conditions. The fastest-converging and best-performing model for these analytical test cases turned out to be the Wheatland et al. (2000) optimization algorithm, as implemented by Wiegelmann (2004). A similar benchmark test with 6 different NLFFF codes was carried out by Metcalf et al. (2008), revealing differences in the free energy by about a factor of 2 for the different codes. The non-force-free boundary problem, however, can be circumvented with force-free codes that fit coronal loop features, rather than photospheric data, for instance with stereoscopic loop detection codes (Aschwanden 2013a), or with automated loop tracing codes (Aschwanden et al. 2014). The most comprehensive benchmark test of 12 NLFFF codes was carried out by De Rosa et al. (2009), using Hinode/SOT-SP, Hinode/XRT, EUV/STEREO, and MDI/SOHO observations. The following critical requirements for successful NLFFF modeling were assessed: (i) sufficiently large areas of vector magnetic field data are needed, (ii) the uncertainties in the boundary data need to be incorporated in the NLFFF algorithms, and (iii) a more realistic physical model is needed to approximate the photosphere-to-corona interface (De Rosa et al. 2009). It was shown that the incorporation of measurement errors implemented into the various NLFFF codes significantly improves the quality of NLFFF solutions from imperfect boundary conditions (Wiegelmann and Inhester 2010; Wiegelmann et al. 2012).
Using various methods of potential field methods (potential field source surface (PFSS), unipolar charges, dipolar models) and non-potential force-free field methods (NLFFF), it was shown that all these theoretical magnetic field models exhibit a misalignment of order ≈ 20∘–40∘ with respect to the observed loop directions measured in EUVI/STEREO images, compared either with their 2-D projections, or with the 3-D coordinates as triangulated from stereoscopic observations (Sandman et al. 2009; Aschwanden and Sandman 2010; Sandman and Aschwanden 2011). A residual misalignment of ≈ 11∘–17∘ has been attributed to the non-potentiality of active regions (Aschwanden and Sandman 2010).
Newly developed NLFFF codes include: a magneto-hydrostatic approach (Flyer et al. 2004); a Grad-Rubin method based on partial derivatives instead of finite differences (Song et al. 2006); NLFFF codes in spherical geometry instead of Cartesian geometry (Wiegelmann 2007); the so-called flux insertion method based on the geometry of observed Hα filaments (Van Ballegooijen 2004; Van Ballegooijen et al. 2007; Bobra et al. 2008; Titov et al. 2014); the vertical current approximation VCA-NLFFF code (Aschwanden 2013b,c, 2016; Aschwanden and Malanushenko 2013); and a stereoscopic triangulation code using automatically traced coronal loops (Aschwanden et al. 2014). An example of a VCA-NLFFF solution with automatically traced loops is shown in Fig. 9.15.
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Aschwanden, M.J. (2019). Coronal Loops. In: New Millennium Solar Physics. Astrophysics and Space Science Library, vol 458. Springer, Cham. https://doi.org/10.1007/978-3-030-13956-8_9
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