Energy Evolution from the Chromosphere to the Heliosphere in the 2021 October 28 Solar Eruption
Pith reviewed 2026-05-20 15:36 UTC · model grok-4.3
The pith
The total energy released in the 2021 October 28 solar eruption matches pre-event stored magnetic energy, with CME kinetic and potential energy dominating the partition.
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
Core claim
We find that the total energy released during the event is consistent with estimates of the pre-event stored magnetic energy, and the CME kinetic + potential energy dominates the energy partition.
What carries the argument
Comprehensive energy budget assembled from remote-sensing, in-situ observations, and scaling laws that converts pre-event magnetic energy into measured components across the chromosphere, corona, and heliosphere.
If this is right
- The CME carries the majority of released energy outward, implying that heliospheric effects are dominated by the ejected plasma and its shock rather than by flare radiation.
- Consistency between total output and stored magnetic energy supports using active-region magnetic budgets to forecast overall eruption scale.
- Flare-related components such as non-thermal electrons, thermal loops, and chromospheric heating together represent a smaller fraction than the CME terms.
- The global EUV wave accounts for a measurable but secondary share of the energy budget.
Where Pith is reading between the lines
- The same energy-partition pattern may hold for other fast CMEs from X-class flares, offering a template for modeling space-weather impacts.
- Future direct measurements of non-thermal ions could test whether the scaling-law estimates used here are generally reliable.
- Solar-wind and heliospheric models may need to weight CME kinetic input more heavily than flare radiation when simulating energy propagation from the Sun.
Load-bearing premise
Scaling laws based on previous observations accurately estimate quantities such as energy in non-thermal ions, energy deposited in the chromosphere, and energy dissipated by the EUV wave for this specific event.
What would settle it
A direct measurement of non-thermal ion energy or EUV-wave dissipation that differs substantially from the values obtained via scaling laws would break the reported consistency between total released energy and pre-event magnetic energy.
Figures
read the original abstract
We perform a detailed study of the energetics for a well-observed solar eruption and flare that occurred on 28 October 2021. This event included a GOES class X1.0 flare, a global EUV wave, and a coronal mass ejection that reached speeds of >2000 km/s. The event was observed from a variety of spacecraft in NASA's Heliophysics System Observatory, including multiple missions near Earth, STEREO-A off the Sun-Earth line, and Solar Orbiter, near the Sun-Earth line at about 0.8 au. Using remote sensing, in situ observations, and in some cases scaling laws based on previous observations, we characterize the following quantities: free magnetic energy, energy in non-thermal electrons, energy in non-thermal ions, bolometric energy, energy deposited in the chromosphere, thermal energy radiated in the flare loops, energy dissipated by the EUV wave, CME kinetic and gravitational potential energy, CME energy flux in the heliosphere, and the energy partition in the CME shock. We find that the total energy released during the event is consistent with estimates of the pre-event stored magnetic energy, and the CME kinetic + potential energy dominates the energy partition.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The manuscript presents a multi-spacecraft analysis of the energy budget for the 28 October 2021 X1.0 flare and associated fast CME (>2000 km/s) and global EUV wave. Combining remote-sensing and in-situ data from missions including Solar Orbiter, STEREO-A, and near-Earth observatories, the authors estimate free magnetic energy, non-thermal electron and ion energies, bolometric and chromospheric radiated energies, EUV-wave dissipation, CME kinetic plus gravitational potential energy, and heliospheric energy flux. They conclude that the summed released energy is consistent with the pre-event stored magnetic energy and that CME kinetic plus potential energy dominates the partition.
Significance. If the component estimates hold, the work supplies one of the more complete end-to-end energy inventories for a fast eruption, linking chromospheric deposition to heliospheric transport and reinforcing the observational picture that CME mechanical energy accounts for the majority of the budget. The multi-mission coverage and explicit inclusion of scaling-law terms for otherwise inaccessible quantities are clear strengths.
major comments (2)
- [Abstract and energy-estimation sections] Abstract and energy-estimation sections: the headline consistency between total released energy and pre-event magnetic energy, together with the claimed CME dominance, rests on the sum of ~10 terms. Three of these (non-thermal ion energy, chromospheric energy deposition, and EUV-wave dissipation) are obtained exclusively from scaling relations calibrated on earlier, typically slower events. No uncertainty propagation or event-specific cross-check is reported for these three terms; a 30–50 % systematic offset in any one of them would render the numerical agreement and the partition indeterminate.
- [Energy estimation sections] The manuscript does not demonstrate that the adopted scaling laws remain valid for a CME speed >2000 km/s and a globally propagating EUV wave; this applicability assumption is load-bearing for the central claim yet is not tested against independent observables available for this event.
minor comments (2)
- Notation for the various energy components could be standardized in a single table to improve traceability between the abstract, methods, and results.
- Figure captions should explicitly state which energy terms are directly measured versus scaled, and list the source references for each scaling relation.
Simulated Author's Rebuttal
We thank the referee for the constructive and detailed report, which identifies key areas where the energy budget analysis can be strengthened. We address each major comment below and outline revisions to improve the robustness of the presented results.
read point-by-point responses
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Referee: [Abstract and energy-estimation sections] Abstract and energy-estimation sections: the headline consistency between total released energy and pre-event magnetic energy, together with the claimed CME dominance, rests on the sum of ~10 terms. Three of these (non-thermal ion energy, chromospheric energy deposition, and EUV-wave dissipation) are obtained exclusively from scaling relations calibrated on earlier, typically slower events. No uncertainty propagation or event-specific cross-check is reported for these three terms; a 30–50 % systematic offset in any one of them would render the numerical agreement and the partition indeterminate.
Authors: We agree that the three terms derived from scaling relations constitute a significant fraction of the budget and that the absence of explicit uncertainty propagation leaves the numerical agreement vulnerable to systematic offsets. In the revised manuscript we will add a dedicated uncertainty subsection that propagates both statistical and systematic uncertainties for these terms, drawing on the published scatter in the original calibration samples. We will also include a sensitivity analysis that varies each of the three terms by ±30 % and ±50 % while holding the directly measured quantities fixed, thereby quantifying how such offsets would affect the total energy balance and the claimed CME dominance. This addition will make the robustness (or lack thereof) of the headline conclusion transparent to readers. revision: yes
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Referee: [Energy estimation sections] The manuscript does not demonstrate that the adopted scaling laws remain valid for a CME speed >2000 km/s and a globally propagating EUV wave; this applicability assumption is load-bearing for the central claim yet is not tested against independent observables available for this event.
Authors: We acknowledge that the manuscript applies the scaling relations without an explicit test of their validity at the extreme speeds and global scale of this eruption. In revision we will expand the methods and discussion sections to (i) summarize the parameter ranges covered by the original calibration studies and note any fast-CME or global-wave events included in those samples, and (ii) perform limited cross-checks against independent observables already present in the multi-spacecraft dataset—for example, comparing the EUV-wave dissipation estimate with the observed wave amplitude and speed derived from STEREO-A and Solar Orbiter EUV imagery, and comparing the non-thermal ion energy with the in-situ energetic-particle fluence measured near 1 au. Where direct quantitative tests remain limited by the available data, we will explicitly state the extrapolation assumption and its potential impact on the energy partition. These additions will document the degree to which the scaling-law applicability can be supported by this event’s own observations. revision: partial
Circularity Check
No significant circularity detected
full rationale
The paper characterizes energies using remote sensing, in situ observations from multiple spacecraft, and scaling laws based on previous observations. No derivation step reduces a claimed prediction or result to a quantity fitted or defined by the paper's own equations. The consistency between total released energy and pre-event magnetic energy is presented as a comparison of independently estimated quantities rather than a self-referential closure. Scaling relations are explicitly attributed to earlier work by other groups, with no load-bearing self-citation chain or ansatz smuggled via prior author work. The central energy partition conclusion therefore rests on external inputs and does not reduce by construction to the study's own fitted values.
Axiom & Free-Parameter Ledger
axioms (1)
- domain assumption Scaling laws based on previous observations can be applied to estimate non-thermal ion energy, chromospheric deposition, and EUV wave dissipation in this event
Lean theorems connected to this paper
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IndisputableMonolith/Foundation/Cost/FunctionalEquation.leanwashburn_uniqueness_aczel unclear?
unclearRelation between the paper passage and the cited Recognition theorem.
Using remote sensing, in situ observations, and in some cases scaling laws based on previous observations, we characterize the following quantities: free magnetic energy, energy in non-thermal electrons, energy in non-thermal ions, bolometric energy, energy deposited in the chromosphere, ... energy dissipated by the EUV wave, CME kinetic and gravitational potential energy...
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IndisputableMonolith/Foundation/BlackBodyRadiationDeep.leanblackBodyRadiationDeepCert unclear?
unclearRelation between the paper passage and the cited Recognition theorem.
we use a scaling law found by (Emslie et al. 2012) for an ensemble of fourteen events... Enti/Ente = 0.34±0.5
What do these tags mean?
- matches
- The paper's claim is directly supported by a theorem in the formal canon.
- supports
- The theorem supports part of the paper's argument, but the paper may add assumptions or extra steps.
- extends
- The paper goes beyond the formal theorem; the theorem is a base layer rather than the whole result.
- uses
- The paper appears to rely on the theorem as machinery.
- contradicts
- The paper's claim conflicts with a theorem or certificate in the canon.
- unclear
- Pith found a possible connection, but the passage is too broad, indirect, or ambiguous to say the theorem truly supports the claim.
Reference graph
Works this paper leans on
- [1]
- [2]
-
[3]
Aschwanden, M. J. 2004, in ESA Special Publication, Vol. 575, SOHO 15 Coronal Heating, ed. R. W. Walsh, J. Ireland, D. Danesy, & B. Fleck, 97
work page 2004
- [4]
-
[5]
Aschwanden, M. J., Caspi, A., Cohen, C. M. S., et al. 2017, ApJ, 836, 17
work page 2017
-
[6]
Aschwanden, M. J., Kontar, E. P., & Jeffrey, N. L. S. 2019, Global Energetics of Solar Flares. VIII. The Low-energy
work page 2019
-
[7]
Cutoff, ApJ, 881, 1, DOI:10.3847/1538-4357/ab2cd4
- [8]
-
[9]
Benkhoff, J., Murakami, G., Baumjohann, W., et al. 2021, SSRv, 217, 90
work page 2021
-
[10]
Benz, A. O. 2017, Living Reviews in Solar Physics, 14, 2
work page 2017
-
[11]
Bobra, M. G., Sun, X., Hoeksema, J. T., et al. 2014, SoPh, 289, 3549
work page 2014
-
[12]
Brueckner, G. E., Howard, R. A., Koomen, M. J., et al. 1995, SoPh, 162, 357
work page 1995
-
[13]
Cargill, P. J., Mariska, J. T., & Antiochos, S. K. 1995, ApJ, 439, 1034
work page 1995
- [14]
- [15]
-
[16]
Darnel, J. M., Seaton, D. B., Bethge, C., et al. 2022, Space Weather, 20, e2022SW003044
work page 2022
-
[17]
David, L., Fraschetti, F., Giacalone, J., et al. 2022, ApJ, 928, 66
work page 2022
-
[18]
P., Gedalin, M., Lalti, A., et al
Dimmock, A. P., Gedalin, M., Lalti, A., et al. 2023, A&A, 679, A106
work page 2023
-
[19]
Domingo, V., Fleck, B., & Poland, A. I. 1995, SSR, 72, 81
work page 1995
-
[20]
Emslie, A. G., Dennis, B. R., Holman, G. D., & Hudson, H. S. 2005, Journal of Geophysical Research (Space Physics), 110, A11103
work page 2005
-
[21]
Emslie, A. G., Kucharek, H., Dennis, B. R., et al. 2004, Journal of Geophysical Research (Space Physics), 109, A10104
work page 2004
- [22]
-
[23]
Fagundes, P. R., Pillat, V. G., Tardelli, A., & Muella, M. T. A. H. 2024, Journal of Geophysical Research (Space Physics), 129, e2024JA032597
work page 2024
- [24]
-
[25]
Forbes, T. G., & Priest, E. R. 1984, in Solar Terrestrial Physics: Present and Future, ed. D. Butler & K. Papadopoulos (NASA), 35–39
work page 1984
- [26]
-
[27]
Garcia, H. A. 1994, Solar Phys., 154, 275
work page 1994
-
[28]
Gary, D. E., Chen, B., Dennis, B. R., et al. 2018, ApJ, 863, 83
work page 2018
-
[29]
2022, Radio Science, 57, e2022RS007456
Giersch, O., & Kennewell, J. 2022, Radio Science, 57, e2022RS007456
work page 2022
- [30]
-
[31]
B., Tshisaphungo, M., Katamzi-Joseph, Z
Habarulema, J. B., Tshisaphungo, M., Katamzi-Joseph, Z. T., Matamba, T. M., & Nndanganeni, R. 2022, Space Weather, 20, e2022SW003104
work page 2022
- [32]
-
[33]
Hoeksema, J. T., Abbett, W. P., Bercik, D. J., et al. 2020, ApJS, 250, 28
work page 2020
-
[34]
S., O’Brien, H., Carrasco Blazquez, I., et al
Horbury, T. S., O’Brien, H., Carrasco Blazquez, I., et al. 2020, A&A, 642, A9
work page 2020
- [35]
- [36]
-
[37]
Jakimiec, J., Sylwester, B., Sylwester, J., et al. 1992, A&A, 253, 269
work page 1992
- [38]
-
[39]
Kaiser, M. L. 2005, Advances in Space Research, 36, 1483
work page 2005
- [40]
-
[41]
Klein, K.-L., Musset, S., Vilmer, N., et al. 2022, A&A, 663, A173
work page 2022
-
[42]
A., Patsourakos, S., & Cargill, P
Klimchuk, J. A., Patsourakos, S., & Cargill, P. J. 2008, ApJ, 682, 1351
work page 2008
-
[43]
2023, Wind Magnetic Field Investigation (MFI) Full Resolution Data in RTN
Koval, A., & Szabo, A. 2023, Wind Magnetic Field Investigation (MFI) Full Resolution Data in RTN
work page 2023
-
[44]
Coordinates, NASA Space Physics Data Facility, DOI:10.48322/S1KF-0B54
- [45]
-
[46]
Krimchansky, A., Machi, D., Cauffman, S. A., & Davis, M. A. 2004, in Sensors, Systems, and Next-Generation Satellites VIII, ed. R. Meynart, S. P. Neeck, & H. Shimoda, Vol. 5570, International Society for Optics and Photonics (SPIE), 155 – 164
work page 2004
-
[47]
Krucker, S., Hurford, G. J., Grimm, O., et al. 2020, A&A, 642, A15
work page 2020
- [48]
-
[49]
Lario, D., Ho, G. C., Decker, R. B., et al. 2003, in American Institute of Physics Conference Series, Vol. 679, Solar Wind Ten, ed. M. Velli, R. Bruno, F. Malara, & B. Bucci, 640–643 Energy evolution from the chromosphere to the heliosphere35
work page 2003
- [50]
-
[51]
Lepping, R. P., Ac˜ una, M. H., Burlaga, L. F., et al. 1995, SSRv, 71, 207
work page 1995
- [52]
-
[53]
Liu, M., Issautier, K., Meyer-Vernet, N., et al. 2021, A&A, 650, A14
work page 2021
- [54]
- [55]
-
[56]
Liu, Y., Richardson, J. D., & Belcher, J. W. 2005, Planet. Space Sci., 53, 3
work page 2005
-
[57]
G., M¨ uller-Mellin, R., et al
Liu, Y., Luhmann, J. G., M¨ uller-Mellin, R., et al. 2008, ApJ, 689, 563
work page 2008
-
[58]
Long, D. M., Baker, D., Williams, D. R., et al. 2015, ApJ, 799, 224
work page 2015
-
[59]
Long, D. M., Bloomfield, D. S., Chen, P. F., et al. 2017, SoPh, 292, 7
work page 2017
-
[60]
Longcope, D. W., Des Jardins, A. C., Carranza-Fulmer, T., & Qiu, J. 2010, Solar Phys., 267, 107
work page 2010
- [61]
- [62]
-
[63]
Muhr, N., Veronig, A. M., Kienreich, I. W., et al. 2014, SoPh, 289, 4563 M¨ uller, D., St. Cyr, O. C., Zouganelis, I., et al. 2020, AAP, 642, A1 M¨ uller-Mellin, R., B¨ ottcher, S., Falenski, J., et al. 2008, SSRv, 136, 363
work page 2014
-
[64]
Ogilvie, K. W., & Desch, M. D. 1997, Advances in Space Research, 20, 559
work page 1997
-
[65]
Ogilvie, K. W., Chornay, D. J., Fritzenreiter, R. J., et al. 1995, SSRv, 71, 55
work page 1995
-
[66]
Ogilvie, K. W., Fitzenreiter, R. J., Lazarus, A. J., Kasper, J. C., & Stevens, M. 2021, Wind Solar Wind Experiment (SWE) 92-sec Definitive Solar Wind Proton Data, NASA Space Physics Data Facility, DOI:10.48322/NASD-J276
-
[67]
J., Bruno, R., Livi, S., et al
Owen, C. J., Bruno, R., Livi, S., et al. 2020, A&A, 642, A16
work page 2020
-
[68]
Papaioannou, A., Kouloumvakos, A., Mishev, A., et al. 2022, A&A, 660, L5
work page 2022
-
[69]
J., Smyrli, A., & Van Doorsselaere, T
Pascoe, D. J., Smyrli, A., & Van Doorsselaere, T. 2019, ApJ, 884, 43
work page 2019
- [70]
-
[71]
Pesnell, W. D., Thompson, B. J., & Chamberlin, P. C. 2012, Sol. Phys., 275, 3
work page 2012
- [72]
-
[73]
Poletto, G., & Kopp, R. A. 1986, in The Lower Atmospheres of Solar Flares, ed. D. F. Neidig (National Solar Observatory), 453–465
work page 1986
-
[74]
Qiu, J., Liu, W.-J., & Longcope, D. W. 2012, ApJ, 752, 124
work page 2012
-
[75]
Qiu, J., & Longcope, D. W. 2016, ApJ, 820, 14
work page 2016
- [76]
-
[77]
Reeves, K. K., Freed, M. S., McKenzie, D. E., & Savage, S. L. 2017, ApJ, 836, 55
work page 2017
-
[78]
K., T¨ or¨ ok, T., Miki´ c, Z., Linker, J., & Murphy, N
Reeves, K. K., T¨ or¨ ok, T., Miki´ c, Z., Linker, J., & Murphy, N. A. 2019, ApJ, 887, 103
work page 2019
- [79]
- [80]
discussion (0)
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