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Polymeric jets throw light on the origin and nature of the forest of solar spicules


Spicules are plasma jets that are observed in the dynamic interface region between the visible solar surface and the hot corona. At any given time, it is estimated that about 3 million spicules are present on the Sun. We find an intriguing parallel between the simulated spicular forest in a solar-like atmosphere and the numerous jets of polymeric fluids when both are subjected to harmonic forcing. In a radiative magnetohydrodynamic numerical simulation with sub-surface convection, solar global surface oscillations are excited similarly to those harmonic vibrations. The jets thus produced match remarkably well with the forests of spicules detected in observations of the Sun. Taken together, the numerical simulations of the Sun and the laboratory fluid dynamics experiments provide insights into the mechanism underlying the ubiquity of jets. The non-linear focusing of quasi-periodic waves in anisotropic media of magnetized plasma as well as polymeric fluids under gravity is sufficient to generate a forest of jets.

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Fig. 1: Large acceleration and anisotropy.
Fig. 2: Comparison of 2D simulations with observations and laboratory experiments.
Fig. 3: The origin of the forest of spicular plasma in the 2D simulations with convection.

Data availability

Source data for Fig. 1a,b,e,f and Extended Data Fig. 6 are provided with this paper. The data for Fig. 2a and Extended Fig. 3a,b can be downloaded from The raw simulation data files in Fortran binary format (about 300 GB in size) used to produce Fig. 2b,c are available from the corresponding author upon reasonable request.

Code availability

The Pencil code is hosted at The run directory for simulation with solar convection represented in Fig. 2b is publicly available at upon request.


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Computing time provided by Nova HPC at IIA as well as Param Yukti facility at JNCASR under National Supercomputing Mission, Govt. of India is gratefully acknowledged. This work has also utilized SahasraT facility at SERC, IISc for computing and CENSe, IISc for rheometry. S.D. and P.C. thank IIA for financial support towards the usage of SahasraT. S.D. also acknowledges the SOLARNET project that has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement no. 824135. M.O.V.S.N. acknowledges a grant RC00226 to study Faraday oscillations in fluids from the Azim Premji University. M.B.K. thanks the Science and Technology Facilities Council (STFC) for the ST/S000518/1 grant. J.L. acknowledges the support from the Leverhulme Trust via grant RPG-2019-371. C.J.N. thanks STFC for the support received to conduct this research through grant nos. ST/P000304/1 and ST/T00021X/1. R.E. is grateful to STFC (grant no. ST/M000826/1), the Royal Society and the President’s International Fellowship Initiative of the Chinese Academy of Sciences (grant no. 2019VMA052) for enabling this research. R.E. also acknowledges the support received from the Higher Education Programme of Excellence for Particle and Astrophysics, Eötvös L. University (Budapest, Hungary). We thank C. Kalelkar for several discussions on polymeric fluids. IRIS is a NASA small explorer mission developed and operated by LMSAL with major contributions to downlink communications funded by ESA and the Norwegian Space Centre. The accelerated solar global p mode observations used to construct Supplementary Video 5 were obtained by the SoHO/MDI instrument. We used the visualisation software Paraview for volume rendering for Supplementary Video 3.

Author information

Authors and Affiliations



P.C. and M.O.V.S.N. conceptualized the study. P.C. prepared the numerical simulation set-up of the solar atmosphere. P.C. and S.D. performed the simulations, analysed the results and prepared the figures and animations with contributions from J.L. on ASDA and spicule statistics and suggestions from R.E. The fluid experiments were designed and conducted by M.O.V.S.N. The experimental data were analysed by M.O.V.S.N. with contributions from P.C., S.D. and M.B.K. The IRIS data analysis was performed by M.B.K. and R.E., who also prepared the corresponding figures with contributions from C.J.N. and J.L. The p mode time series was provided by R.E. The manuscript was drafted by P.C. and M.O.V.S.N. with input from R.E. All authors contributed to the interpretation of the results and worked on the subsequent versions of the manuscript together.

Corresponding author

Correspondence to Piyali Chatterjee.

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Extended data

Extended Data Fig. 1 Signature of polymer stretching.

(a) The set up for the polarization experiment for detecting polymeric stretching in 2% Poly Vinyl Alcohol. He-Ne laser light passes through a polarizer and then through the sample region of interest probing the jets, to be collected after an analyzer by an imaging device. By varying the angle of the polarizer-analyzer combination at right angles to each other, the polarization state of the jets can be determined (see Methods). (b) Jets of iodinated 2% aqueous PVA by Faraday excitation at 30 Hz. (c) Similar to (b) but seen through the polarizer set-up in (a) to highlight stretching of polymer threads.

Extended Data Fig. 2 Kelvin-Helmholtz instability and magnetic field.

(a) Contours of temperature in the simulation domain with zero imposed magnetic field shows turbulence generated by the Kelvin-Helmholtz instability. (b) Same as (a) with the addition of a damping term in the horizontal velocity equation to mimic suppression of turbulence in the horizontal direction.

Extended Data Fig. 3 Observed and simulated spicules seen in Si IV and Mg II emission lines.

(a) Spicules seen at the solar limb with the Si IV filter of IRIS. (b) Same as (a) but for IRIS Mg II k filter. (c) Shaded contours of synthetic intensity of Si IV emission synthesized using the CHIANTI package available in the FoMo code, for the simulation run with imposed vertical magnetic field Bimp = 74 G at time, t = 152.50 min from the start are shown in the [x, z]-plane. (d) Same as (c) but for emission at Mg II k also using CHIANTI. The cyan rectangle in panels (a) and (b) indicates the same extent as the simulation domain shown in (c)-(d).

Extended Data Fig. 4 Propagation of shock compression and hyper-sonic regions.

(a) Time-distance map of the Mach number, Ma (blue shaded), and shock compression (red contour lines) for a vertical slit at x = 2.5Mm of panel (a). The regions of plasma compression, V < 0, are found to coincide with acceleration fronts, shown in Fig. 3c, where the spicular plasma is energised to hypersonic speeds. The characteristic curve for acoustic waves is denoted by the solid black line.

Extended Data Fig. 5 Plasma heating processes.

(a) Synthetic Si IV emission from the simulated spicule forest similar to Fig. 3c calculated using CHIANTI. The green contours denote the locations of plasma heating above 103Ks−1 only due to the local compression of plasma, − (γ − 1)TV, where T and V are the plasma temperature and velocity, respectively. The ratio of specific heats denoted, γ = cP/cV, has been calculated using the equation of state for a partially ionized ideal gas. (b) Regions of Mach number, Ma > 1, are indicated by shaded blue contours. Here, the green contours show heating above 103Ks−1 only due to dissipation inside the shocks by ζshock(V)2/cV, where ζshock is the shock viscosity. (c) Strength of various heating sources as function of height in the atmosphere. Horizontally averaged heating profiles, 〈H〉(z) due to local plasma compression (red-dashed), shock dissipation (black-solid), and Ohmic heating (blue dot-dashed).

Extended Data Fig. 6 Comparing height distribution of solar spicules and fluid jets.

(a) Histogram for distribution of \(H=(h-{h}_{\min })/({h}_{\max }-{h}_{\min })\), where h is the maximum height reached by a spicule and \({h}_{\min }\), \({h}_{\max }\) are the minimum and maximum heights of a sample of unique spicules (sample size 216 and counted during 40min of solar time), respectively, as seen in synthetic emission at T = 15, 000 K from the simulation shown in Extended Fig. 3b. (b) The distribution of H from a sample of unique fluid jets (sample size 224 and counted during 10 excitation periods post the central jet ejection) in an experiment with iodinated 2% PVA. Note that only spicules such that 6 < h < 24.9 Mm and fluid jets such that 0.5 < h < 4.5cm have been included in the distribution. The lower limit in the simulation is chosen because individual spicules cannot be discerned if they are below 6Mm, whereas, in the experiment the lower end is set by the container height of 0.5cm. The upper limits are the maximum heights obtained in the experiments. (c) The cumulative distribution function (CDF) to indicate the number of jets above \(h > {h}_{\min }\) for both plasma and polymeric fluid.

Source data

Extended Data Fig. 7 Phase plot of vertical component of velocity, vz versus acceleration, az.

(a) The region around a shorter spicule above an inter granular lane squeezing site used for the calculation at t = 15.33min from the start of tracking. Each dot denotes a Lagrangian particle colored by its instantaneous vertical velocity, vz. The yellow contours are magnetic field lines. (b) vz versus az. (c) vz versus the vertical acceleration only due to the Lorentz force. Note that the particles considered, initially at t = 0 lie in layers 0 < z < 3Mm. Every dots denotes a particle and colored by its instantaneous vertical position. (d) The region where a longer spicule takes birth just above a granule at t = 17.50min. The magnetic field lines are shown by black contours. (e) and (f) are same as (b) and (c), respectively, but, for the case of the longer spicule shown in (d).

Extended Data Fig. 8 Solar atmospheric stratification with convection.

(a) Temperature structure at the time of introduction of Lagrangian particles in the domain for the same run shown in Fig. 3a. The white solid line is the optical depth, τ = 0.1 surface. (b) The density at the same instant as (a). The plasma β = 1 surface is denoted by the black solid line. (c) The vertical velocity, vz corresponding to panels (a) and (b).

Extended Data Table 1 Dynamic similarity. List of non-dimensional parameters with respect to which the two systems can be considered dynamically similar. Here, d and L are the typical width and length of the jets, whereas, U is the typical velocity scale. The Froude number indicates the importance of surface gravity in the dynamics. The expression for Froude number is different for two different scenarios - one for a continuum stratified solar atmosphere and the other for a fluid-air interface (polymeric fluid). The density scale height in the solar chromosphere is denoted, Hρ ~ 150¦km. The peak acceleration of the Faraday excitation (fluid) and chromospheric plasma acceleration, in terms of the local gravity, is given by a/g. Here, g takes value gS ~ 274¦m¦s−2 for the Sun and gE ~ 9.8¦m¦s−2 for the Earth. In the solar plasma, the frequency of driving is f0 = 3.3mHz whereas, in the fluid, f0 = 30¦Hz and τ = L/U is the typical lifetime of the jets. The fluids are 2% and 3% PVA solution
Extended Data Table 2 List of runs. Parameters of the numerical and the table top runs along with the figures and videos where they have been referenced. All the solar MHD simulations are performed with a sponge layer temperature, TSL = 106K. The driving velocity amplitude is V0 at the driving frequency, f0. The wave number k = nπ/L, where n is the number of crests in the horizontal domain of length, L. For the polymeric fluid experiments, A0 denotes the peak acceleration amplitude scaled with local gravity, gE = 9.8 m s−2, c is the polymer concentration expressed either as parts-per-million (ppm) or as weight percentage, νp is the measured kinematic viscosity

Supplementary information

Supplementary information

Supplementary discussion on mathematical connection between polymers and magnetic fields and Supplementary Figs. 1 and 2.

Supplementary Video 1

Response of solar plasma to superposition of frequencies: (a) Synthetic Si-IV emission according to the analytical expression given by Eq.2 from a model driven by a velocity forcing of the form \({v}_{z}/{V}_{0}=\sin (2\pi {f}_{1}t)/4+\sin (2\pi {f}_{2}t)/2+\sin (2\pi {f}_{3}t)/4\) shown in panel (c), where V0 = 1.0kms−1, f1 = 3.0 mHz, f2 = 3.5 mHz, and f3 = 4.0 mHz. The above forcing has only been applied within a layer, − 50 km < z < 0 km. (b) Same as (a) but for temperature (in Kelvin).

Supplementary Video 2

Jet breaking in polymeric fluid (PEO, 1000 ppm, viscoelastic) versus 55% glycerine solution (viscous) at two different frequencies (a) 120 Hz, and (b) 30 Hz with acceleration amplitudes in terms of local gravity indicated. (c) Polymeric fluids (iodinated 2% PVA, 23% jets reaching heights above 1 cm break) may resist droplet ejection by pinching of jets (due to Plateau-Rayleigh instability) as compared to Newtonian fluids (76% Glycerine solution, 53% jet-breakage above 1 cm) of similar viscosity and surface tension. Both fluids are subjected to similar peak forcing of 10.1gE (30 ml fluid in cylindrical container).

Supplementary Video 3

Nonlinear development in numerical and table-top experiment: volume rendering of synthetic emission at 15000 K for a three-dimensional numerical simulation of solar plasma forced at the lower boundary with a periodic forcing with a velocity amplitude of 1.32 km s−1 and an imposed magnetic field of 10 G (left panel). A polymeric fluid (iodinated 3% PVA solution) subjected to Faraday excitation at 30 Hz and a peak acceleration of 10.1gE (right panel). Both the numerical and the table-top experiments show nonlinear development in about five oscillation periods.

Supplementary Video 4

Mechanism of formation of fluid jets: View of the free surface of iodinated 3% PVA, as seen at an angle of 20 from the vertical, to show the mechanism for jet forest formation by collision of ridges of neighbouring polygonal cells formed due to interacting surface gravity waves (via nonlinear mode coupling).

Supplementary Video 5

Response of polymeric fluid to frequency scaled solar p-modes: Iodinated 2% PVA (30 ml) placed in a circular container of 0.1 m diameter and responding to frequency-scaled quasi-periodic solar acoustic modes (p-modes from SOHO/MDI) such that the dominant FFT peak lies at 30 Hz. The peak acceleration reaches up to 5gE. Imaged at 500 fps.

Supplementary Video 6

Synthetic emission at a temperature of 80000 K calculated using the analytical expression of Eq. (2) (top panel) and AIA 17.1 nm emission from our numerical simulation (bottom panel). Magnetic fields are shown by red curves.

Supplementary Video 7

Faraday excitation experiment with paint: Initially separate red (15 ml) and white (15 ml) paint in a circular container of diameter 0.1 m responding to a 30 Hz harmonic Faraday excitation with a peak acceleration of 7gE imaged at 1000 fps. We observe the abundant formation of jet forest, some of which exhibit rotation as visualized by twisted motion of the red and white threads of paint.

Supplementary Video 8

Lagrangian tracking of the plasma in the spicule forest: (a) 540000 particles are initially distributed uniformly in six differently coloured layers, each with 1 Mm thickness except the bottom one which is 0.5 Mm thick, between − 0.5 < z < 5 Mm. (b) and (c) Particles are tracked by local acceleration and vertical velocity to show acceleration fronts energizing the spicular plasma. Black curves in (b) show magnetic field lines whereas the black contours in (c) denote regions of shock. (d) Spicule formation driven by granular collapse in convective plumes, P1 and P2. (e) Spicule formation driven by solar global oscillations and magnetic reconnection (denoted by the white rectangle).

Supplementary Video 9

Determination of \({A}_{\min }\) in A0 versus f0 phase space: Part I (solar atmosphere): Spicules formed in response to wave driving of the form \(2\pi {f}_{0}{V}_{0}\sin (2\pi {f}_{0}t)\cos (5\pi x/L)\), with (a) V0 = 0.5 kms−1, (b) V0 = 0.35 and (c) 0.25 kms−1, respectively. The dashed line indicates the 7 Mm height. Note that the forest of jet criteria is satisfied for cases (a) and (b) only. Part II (Polymeric fluid): Jets formed in response to Faraday excitation with peak accelerations, A0 as (a) 4.1gE, (b) 3.6gE, (c) 4.3gE, and (d) 4.7gE. The dotted line denotes the 1.3 cm mark on the scale. Only (c) and (d) satisfy the forest of jets criteria.

Source data

Source Data Fig. 1

Contains: Data points f0 vs A0 in csv format for threshold acceleration in solar atmosphere necessary for spicule formation (Fig. 1a). Data points f0 vs A0 in csv format for threshold acceleration in PEO necessary for jet formation (Fig. 1b) Anisotropy varying with magnetic field in solar atmospheric simulation (Fig. 1e). Anisotropy varying with polymer concentration in experiment with PEO (Fig. 1f).

Source Data Extended Data Fig. 6

Height values for 216 spicules from two different data sets. Set 1 for 136 unique spicules and set 2 for 80 unique spicules sampled from two different simulation runs with convection (Extended Data Fig 6a). Also includes height values for 224 unique jets from iodinated 2% Poly Vinyl Alcohol solution subjected to harmonic vibration at 30 Hz (Extended Data Fig. 6b).

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Dey, S., Chatterjee, P., O. V. S. N., M. et al. Polymeric jets throw light on the origin and nature of the forest of solar spicules. Nat. Phys. 18, 595–600 (2022).

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