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P2D - A Two-Dimensional Multi-Spacecraft Solar Wind Persistence Model

Space Physics · Submitted 28 Sep 2026 · 91 references

Pith's verdict: Honest, well-validated extension of persistence modeling; the real open question is whether the spacecraft weighting relations are in-sample, and that's referee-answerable rather than fatal.

T0 · AI review

How this review was made: An AI referee (deepseek/deepseek-v4-flash) read the paper on September 29, 2026 and answered a fixed list of questions about it. T0 is the starting level every paper gets. The levels describe how deeply Pith has checked the paper, never the authors.

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arXiv ID2609.34685 (version 1)
Pith IDZOJV4DZ6, Pith's permanent record of this paper and its review
CitationDaniel Milo\v{s}i\'c, Manuela Temmer, Mathew Owens, Stefan J. Hofmeister, Stephan G. Heinemann. "P2D - A Two-Dimensional Multi-Spacecraft Solar Wind Persistence Model." arXiv:2609.34685 (2026). https://pith.science/paper/ZOJV4DZ6
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Referee report
The paper

The paper claims

The paper builds a two-dimensional persistence model of the solar wind from multi-spacecraft in-situ data, claiming that from Earth's perspective it reconstructs bulk speed with an MAE of 65.41 km/s and density with an MAE of 3.51 cm^-3…

The reading

This paper claims that the solar wind can be reconstructed over a two-dimensional (longitude and radius) map of the inner heliosphere by propagating in-situ speed and density measurements from several spacecraft, using only rigid corotation and a simple inelastic collision scheme, without any magnetohydrodynamic physics. The resulting model, P2D, is said to beat the 27-day persistence benchmark in nearly all speed metrics and in all binary high-speed-stream metrics, to add a density reconstruction that also beats the benchmark, and to be second only to a machine-learning model (AmbSoWi-ML) in point-to-point speed metrics. The central practical claim is that the reconstruction improves most when a spacecraft is positioned between Earth and L5, which the authors take as evidence that the planned Vigil L5 mission would provide a strong basis for persistence forecasts. If correct, P2D offers a computationally trivial forecasting tool whose only inputs are in-situ measurements and whose output can be evaluated at any point in the heliosphere where a spacecraft lies closer to the Sun than the target.

What carries the argument

The load-bearing object is the two-dimensional propagation-and-combine scheme: each spacecraft's in-situ measurements are spread into a radial-longitudinal map by rigid corotation plus ballistic radial advection, and the per-spacecraft reconstructions are merged by weighting each source inversely to an empirical uncertainty both designs and powers the argument: Equation 2 (speed) and Equation 3 (density), the error relations that assign a predicted MAE based on latitudinal and longitudinal separation to the target, and Equation 4, the inverse-uncertainty combination that converts those errors into weights. The work the scheme does is to convert spacecraft separation geometry directly into forecast contribution, so that the model's headline performance follows from the error relations rather than from any physical evolution model.

Extended reading notes

Core claim

The central claim is that solar wind persistence, which is normally exploited as a one-dimensional one-Carrington-rotation echo of near-Earth data, can be organised into a two-dimensional map from which reconstructions at arbitrary targets follow. In-situ speed and density samples from OMNI, STEREO-A, STEREO-B, Parker Solar Probe and Solar Orbiter are each propagated longitudinally at the rigid synodic rotation period of 27.27 days and radially at their own measured speed, with an ideal inelastic collision (Equation 1) preventing streams from overtaking one another inside each spacecraft's map. The per-spacecraft maps are then merged at the target by inverse-uncertainty weighting, where the uncertainty of each source comes from empirical error relations in latitudinal and longitudinal separation to Earth: the speed relation (Equation 2) is taken from the authors' earlier persistence study, and a new density analogue (Equation 3) is fitted in Appendix A. Validated against OMNI at Earth over the full 2008-2026 range and in a restricted 2012-2017 window against other models, P2D reports a speed MAE of 65.41 km/s, a density MAE of 3.51 $cm^{-3}$, a 64% true positive rate and best-in-class binary metrics, while remaining second to AmbSoWi-ML on point-to-point speed metrics. The paper reports that during periods when STEREO-A or STEREO-B lies between Earth and L5, the speed MAE falls to roughly 40-60 km/s, a decrease of about 35% relative to the 27-day persistence benchmark, and attributes the improvement mainly to short propagation paths from the upstream probe.

Load-bearing premise

The load-bearing premise is that the empirical error relations (Equations 2 and 3) correctly predict reconstruction error from latitudinal and longitudinal separation, because they set the spacecraft weights and hence the reported performance; the authors acknowledge these relations are fitted to their own persistence-propagated data, hold only up to roughly 15 degrees of latitudinal separation, and rest on data clustered near 1 AU.

Editorial extensions

If this is right

  • P2D outperforms the 27-day persistence benchmark in nearly every speed metric and in all binary high-speed-stream metrics, so a persistence argument alone, organised in two dimensions, is a stronger baseline than the conventional one-dimensional corotation echo.
  • A spacecraft stationed between Earth and L5 cuts the speed MAE by roughly 35% relative to the benchmark, which is the paper's concrete quantitative case for planning future L5 missions such as Vigil as the backbone of persistence forecasts.
  • Because the reconstruction needs only one spacecraft closer to the Sun than the target, the same scheme can yield forecasts at any heliospheric point with such coverage, including other planets such as Mars.
  • The two-dimensional maps supply ambient-solar-wind context in which coronal mass ejection propagation can be studied and in which combined speed-and-density output enables dynamic-pressure and drag-force calculations.
  • With science-level data and zero lead time the model is computationally trivial, running roughly 45 seconds per spacecraft-year at 0.5-degree resolution, so operational deployment reduces to a data-availability question rather than a computing one.

Reading between the lines

Editorial extensions of the paper, not claims the author makes directly.

  • The headline 65.41 km/s figure is earned on a 2012-2017 window in which PSP and SolO do not contribute, while the 35% improvement figure comes from the full-range analysis during favorable 2023-2026 geometry; the two headline numbers describe different conditions and should not be conflated.
  • The density reconstruction has a low point-to-point correlation (CC 0.21) yet very accurate CIR density-peak timing (mean error under an hour), so the model is probably capturing stream-interface timing far better than amplitude; users of dynamic-pressure estimates should trust its timing, not its magnitude.
  • If the empirical error relations are confirmed to extrapolate beyond their fitted range, the same inverse-uncertainty weighting formalism would transfer directly to forecast targets other than Earth, making the model a generic heliospheric interpolation tool rather than an Earth-specific forecast.
  • The 2D output is a natural cheap boundary condition for more physical models: feeding its multi-probe maps into data-assimilation or HD/MHD schemes could replace magnetogram-driven inputs with purely in-situ-driven evolution.
Original abstract

The background solar wind is a key component in space weather forecasting, as it contains geoeffective high-speed streams and provides the medium through which coronal mass ejections propagate and evolve in interplanetary space. Due to the solar rotation and the slow evolution of large-scale solar wind structures, solar wind properties exhibit an autocorrelation with a period of roughly 27 days, particularly at solar minimum. We made use of this property to develop a solar wind persistence model with input from multiple spacecraft (Solar Orbiter, Parker Solar Probe, STEREO-A, STEREO-B and the OMNI database). The model ballistically propagates in-situ data from the position of their measurement radially away from the Sun, as well as longitudinally with the solar rotation rate, producing 2D maps of solar wind parameters. These can be extracted at any point in the heliosphere for a solar wind reconstruction. From Earth's perspective, the reconstruction performs with an MAE of 65.41 km/s and 3.51/cm^3 for speed and density, respectively. During high-speed streams, the peak hit rate is 50% and 48% for speed and density. It performs best during times when there are spacecraft located between Earth and Lagrange point L5. During these times, the mean absolute error of the predicted solar wind speed decreases by roughly 35% in comparison to the benchmark 27-day persistence model. Therefore, future L5 missions like Vigil are expected to provide a robust basis for reliable persistence forecasts.

The compiled record

The paper's own sentences, arranged, kept beside the review and separate from it. Each label is drawn from a closed vocabulary; the number beside it is the probability the classifier gave that label. Numbers in the tables are the authors', checked by code. No sentence in this record was written by a model.

Compiled by classifier-1.13.0 via TypeSafe API, question bank abstract-p1-20260923, 2026-09-29: 1 request, 7,659 input tokens.

What the abstract itself states, as probabilities: claims first 0.04 · states limitation 0.80 · human participants 0.01 · controlled comparison 0.92 · randomized assignment 0.01 · states quantitative result 0.99 · compares with prior results 0.97 · mentions code or data availability 0.03.

The abstract, sentence by sentence

arXiv listing abstract v1. Results and the main claim are underlined; .

The background solar wind is a key component in space weather forecasting, as it contains geoeffective high-speed streams and provides the medium through which coronal mass ejections propagate and evolve in interplanetary space. Due to the solar rotation and the slow evolution of large-scale solar wind structures, solar wind properties exhibit an autocorrelation with a period of roughly 27 days, particularly at solar minimum. We made use of this property to develop a solar wind persistence model with input from multiple spacecraft (Solar Orbiter, Parker Solar Probe, STEREO-A, STEREO-B and the OMNI database). The model ballistically propagates in-situ data from the position of their measurement radially away from the Sun, as well as longitudinally with the solar rotation rate, producing 2D maps of solar wind parameters. These can be extracted at any point in the heliosphere for a solar wind reconstruction. From Earth's perspective, the reconstruction performs with an MAE of 65.41 km/s and 3.51/cm^3 for speed and density, respectively. During high-speed streams, the peak hit rate is 50% and 48% for speed and density. It performs best during times when there are spacecraft located between Earth and Lagrange point L5. During these times, the mean absolute error of the predicted solar wind speed decreases by roughly 35% in comparison to the benchmark 27-day persistence model. Therefore, future L5 missions like Vigil are expected to provide a robust basis for reliable persistence forecasts.

background contribution method result interpretation main claim

What the classifier reports for each sentence. The number is the probability it gave the label.
#sentencerolethe authors' own workstates the main conclusionstrength
s0 The background solar wind is a key component in space weather forecasting, as it contains geoeffective high-speed streams and provides the medium through which coronal mass ejections propagate and evolve in interplanetary space. background 1.00 0.04 0.03 asserted 1.00
s1 Due to the solar rotation and the slow evolution of large-scale solar wind structures, solar wind properties exhibit an autocorrelation with a period of roughly 27 days, particularly at solar minimum. background 1.00 0.07 0.02 asserted 0.99
s2 We made use of this property to develop a solar wind persistence model with input from multiple spacecraft (Solar Orbiter, Parker Solar Probe, STEREO-A, STEREO-B and the OMNI database). method 0.53 0.96 0.05 asserted 1.00
s3 The model ballistically propagates in-situ data from the position of their measurement radially away from the Sun, as well as longitudinally with the solar rotation rate, producing 2D maps of solar wind parameters. method 1.00 0.88 0.05 asserted 1.00
s4 These can be extracted at any point in the heliosphere for a solar wind reconstruction. method 0.60 0.60 0.04 asserted 0.95
s5 From Earth's perspective, the reconstruction performs with an MAE of 65.41 km/s and 3.51/cm^3 for speed and density, respectively. result 1.00 0.95 0.10 asserted 1.00
s6 During high-speed streams, the peak hit rate is 50% and 48% for speed and density. result 1.00 0.91 0.05 asserted 1.00
s7 It performs best during times when there are spacecraft located between Earth and Lagrange point L5. result 0.91 0.87 0.10 asserted 1.00
s8 During these times, the mean absolute error of the predicted solar wind speed decreases by roughly 35% in comparison to the benchmark 27-day persistence model. result 0.99 0.92 0.17 asserted 1.00
s9 Therefore, future L5 missions like Vigil are expected to provide a robust basis for reliable persistence forecasts. future work 0.52 0.14 0.68 hedged possibility 0.79

What kind of paper the classifier reports this is: method or tool 1.00 · evidence from analysis of existing data 0.64.

What was examined, and what was not

sources read
  • arXiv listing abstract v1
not examined
  • full text
  • figures and tables
  • references and citing sentences
  • relations to other papers
levels run
  • P abstract
not run
  • S sections
  • T body sentences
  • C citations
  • R cross-paper relations

Every quoted sentence on this record is the authors'. Every label is from Pith's closed vocabulary, with the probability shown beside it. Every number in the measurements table is the authors', checked by code. Record as JSON

Figures
Figure 1. Data availability of all involved spacecraft. OMNI (King and Papitashvili, 2005) is a database providing solar wind data measured at L1 by the Advanced Composition Explorer (ACE, Stone et al., 1998) and the Wind (Ogilvie et al., 1995) spacecraft. The data are numerically propagated to a modeled position of Earth’s bowshock, and hourly averaged. The time shift is being performed using the in-situ measured velocity vector and the plane of the phase front (King and Papitashvili, 2005). We use its data for the entire investigated time range, from 1 February, 2007 to 31 December, 2025…
Figure 2. The 4 steps of the P2D workflow. Each polar plot shows a two-dimensional map of solar wind speed with the big colored dots representing different spacecraft. Panel 1: OMNI data (blue) being propagated in longitude (HEEQ) for one Carrington rotation. Panel 2: OMNI data being propagated across longitude (HEEQ) and radial distance. Panel 2.5: OMNI (blue), STEREO-A (black), PSP (red) and SolO data (yellow) being propagated across longitude (HEEQ) and radial distance for one Carrington rotation. Panel 3: The left side is identical to Panel 2.5 and the right side shows with the same color…
Figure 3. Spacecraft orbits and resulting reconstruction uncertainties and contributions. Yellow: SolO; Red: PSP; Black: STEREO-A; Blue: OMNI. Panel (a): Heliographic latitudinal separations to Earth; (b): Longitudinal separations to Earth; (c): Speed uncertainty; (d): Density uncertainty; (e): Relative contribu￾tions of each spacecraft to the reconstruction. 2.3. Resulting Products Figures 4 and 5 and their respective animations show the resulting models after performing all the above mentioned steps. On the left side of each figure, there are two-dimensional maps, showing speed and density,…
Figure 4. Final two-dimensional speed map and time series extracted from the map at Earth location on March 6, 2023, 12:00 UT. Left: 2D map, color-coded with the reconstructed solar wind bulk speed. Upper right: Time series of the solar wind bulk speed at Earth from the OMNI database in blue and P2D reconstruction in magenta with a light magenta uncertainty area. Lower right: Relative contribution from each spacecraft or database to the reconstruction at the shown time. A movie of the entire reconstructed time range between January 2008 and December 2025 is available in the online version of…
Figure 5. Final two-dimensional density map and time series extracted from the map at Earth location on March 6, 2023, 12:00 UT. Left: 2D map, color-coded with the reconstructed solar wind proton density. Upper right: Time series of the solar wind proton density at Earth from the OMNI database in blue and P2D reconstruction in magenta with a light magenta uncertainty area. Lower right: Relative contribution from each spacecraft or database to the reconstruction at the shown time. A movie of the entire reconstructed time range between January 2008 and December 2025 is available in the online…
Figure 6. Running MAE of the speed over the entire time range (2008-2026). Black profile: Running MAE of the 27-day persistence model. Magenta profile: MAE of P2D. Blue profile: Sunspot number. Black vertical line: Loss of contact with STEREO-B. Red vertical line: Launch of PSP. Yellow vertical line: Launch of SolO. The grey shaded areas mark the time periods where either STEREO-B or STEREO-A are located between Earth and L5. in-situ profiles and evaluating the MAE for each window. The blue line on the bottom shows the monthly averaged sunspot number (Source: WDC-SILSO, Royal Observatory of…
Figure 7. Speed peak error distributions. Left: Histogram of timing errors. Center: Histogram of speed errors. Right: Scatterplot of speed errors against timing errors. Blue: Misses. Red: Hits Metric P2D 27-day persistence ME −0.67 −0.08 MSE 30.89 37.30 MAE 3.51 3.89 RMSE 5.56 6.11 CC 0.21 0.18 Cadence 1h 1h
Figure 8. Running MAE of the proton density over the entire time range (2008-2026). Black profile: Running MAE of the 27-day persistence model, Magenta profile: MAE of P2D, Blue profile: Sunspot number. Black vertical line: Loss of contact with STEREO-B, Red vertical line: Launch of PSP, Yellow vertical line: Launch of SolO. The grey shaded areas mark the time periods where either STEREO-A or STEREO-B are located between Earth and L5. Metric P2D 27-day persistence ME - timing 0.03 d 0.01 d RMSE - timing 0.74 d 0.83 d ME - density −6.53 cm−3 −5.38 cm−3 RMSE - density 13.84 cm−3 14.48 cm−3 Hit…
Figure 9. Density peak error distributions. Left: Histogram of timing errors. Center: Histogram of density errors. Right: Scatterplot of density errors against timing errors. Blue: Misses. Red: Hits meaning underestimated peak amplitudes. This is also clearly visible in the right panel, where many blue dots, i.e. misses, are below the −10 cm−3 line, which we chose as a threshold. 4. Discussion 4.1. Lead time As our model is based on persisting solar wind, which is assumed to circulate the Sun infinitely, we can choose the lead time on the model arbitrarily. Throughout this work, we present a…

Figures reproduced from arXiv:2609.34685 by the authors.

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