Open Access
Issue
A&A
Volume 705, January 2026
Article Number L3
Number of page(s) 6
Section Letters to the Editor
DOI https://doi.org/10.1051/0004-6361/202558072
Published online 19 December 2025

© The Authors 2025

Licence Creative CommonsOpen Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

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1. Introduction

Cometary jets – localized, collimated outflows of gas and dust – are key tracers of nucleus activity and surface inhomogeneity (Sekanina & Larson 1986; Sekanina et al. 2004; Samarasinha & Larson 2014). Their detection provides constraints on the spin-axis orientation, rotation state, and nongravitational forces that drive cometary evolution (Schleicher & Farnham 2004; Kramer et al. 2019). Image-enhancement techniques such as Laplace (Serra-Ricart & Licandro 2015) or Larson–Sekanina filtering (Larson & Sekanina 1984) and azimuthal average subtraction are commonly used to isolate faint, anisotropic structures from the bright coma background (Boehnhardt & Birkle 1994). Measuring the position angle (PA) of individual jets and tracking their evolution enables modeling of the nucleus geometry and identification of discrete active regions. The recently discovered interstellar comet 3I/ATLAS (C/2025 N1 hereafter 3I, Tonry et al. 2025) presents a unique opportunity to extend jet studies beyond the Solar System.

As only the third confirmed interstellar object – after 1I/‘Oumuamua and 2I/Borisov – 3I likely retains pristine volatile and dust from the origin of a exoplanetary system that has likely undergone long-term irradiation by galactic cosmic rays in the interstellar space and some additional irradiation in other stellar systems. Such processing can significantly modify the physical and chemical properties of surface materials and should be distinguished from solar-driven alteration processes (Maggiolo et al. 2025; Ye et al. 2025). Detecting a jet in 3I would provide the first evidence of localized outgassing in an interstellar nucleus, allowing for a direct comparison with activity mechanisms observed in Solar System comets. Such a detection would constrain the orientation and rotation state of the nucleus, quantify possible nongravitational accelerations caused by anisotropic mass loss, and reveal the onset of activity as a function of heliocentric distance, thereby identifying the dominant volatile species (e.g., CO, CO2, and H2O) responsible for outflow initiation. Characterizing jets in 3I thus represents a rare opportunity to investigate the physical behavior of a pristine body formed in another planetary system.

2. Observations

3I was extensively monitored on 37 nights between 2025, July 2 and September 5 (see Table A.1), using the imaging capabilities of the Two-meter Twin Telescope (TTT1). TTT is located at the Teide Observatory on the island of Tenerife (Canary Islands, Spain). Currently, it includes two 0.80-m telescopes (TTT1 and TTT2) and a 2.0-m telescope (TTT3). All images presented in the paper were observed with TTT3. TTT3 is a 2.0-m f/6 Ritchey-Chrétien telescope that is currently in its commissioning phase. 3I images were obtained with COLORS, a 2k × 2k camera mounted at the Nasmyth 2 focus, equipped with a back-illuminated 13.5 μm pixel−1 BEX2-DD CCD sensor, resulting in a field of view of 7.85′ × 7.85′ and a plate scale of 0.23″ pixel−1. Jet images were taken using the Sloan-g′ filter. All the images were bias, dark, and flat-field corrected in the standard way. A WCS (world coordinate system) solution was obtained using Astrometry.net (Lang et al. 2010) against Gaia DR2 and all comet images are aligned from the comet’s optocenter.

3. Methods

To enhance the visibility of potential fine-scale structures in the inner coma of 3I, a Laplacian-filtering technique was applied to the reduced and combined images. The Laplacian operator highlights spatial curvature, and therefore efficiently suppresses the smooth, steep radial gradient of the coma, while enhancing localized features such as narrow jets or filaments. Unlike azimuthal-average subtraction or the Sekanina–Larson residual technique, the Laplacian filter does not rely on any assumed symmetry of the coma, nor does it require iterative rotational subtraction. This makes the method more robust in the presence of multiple or curved jets and less sensitive to small cometary optocenter errors. The resulting Laplacian-filtered frames provide clean, high-contrast representations of any detected jet morphology, from which accurate position-angle profiles can be extracted for quantitative analysis following the procedure described by Serra-Ricart & Licandro (2015). The detection and analysis of jet features were often hampered by low signal-to-noise ratios, imperfect tracking, confusion with background stars, or poor seeing conditions. After careful inspection and processing of all datasets (see Table A.1), only seven observing nights (August 3, 5, 18, 19, 21, 24, and 29) revealed evidence of a faint yet clearly defined jet structure. The corresponding Laplace-filtered frames are displayed in Fig. 1 (for clarity the August 5 frame is not included). In each panel, the PA of the jet – measured at a projected optocenter distance of 6000 km – is indicated by purple lines (median value when multiple measurements are available). Isophotal contours from the original, unfiltered images are superimposed for reference.

Thumbnail: Fig. 1. Refer to the following caption and surrounding text. Fig. 1.

Laplacian-filtered images of the inner coma of the interstellar comet 3I/ATLAS (C/2025 N1). Thin purple lines indicate the PA of the detected jet (median value when multiple measurements are available), calculated at a projected distance of 6000 km from the comet’s optocenter (dotted red circle). For each frame, the observation date (YYYY–MM–DD) and the start and end times in UTC are shown above the panels, together with the total number of sidereal-tracking exposures and the cumulative integration time. The projected velocity vector (red arrow) and the antisolar direction (yellow arrow) are marked, as well as the image scale and orientation. Degraded orange lines denote the projected spin-axis direction (PA = 280.7 ± 0.2°), derived from mean value of the measured jet PAs, while yellow lines trace the tail direction. Red crosshairs mark the comet’s optocenter. Isophotal contours of the original (unfiltered) images are overplotted using ten logarithmically spaced levels between the 20th and 95th percentiles of pixel intensity in each frame. The jet refers to the narrow, linear, black feature extending roughly northwest in the filtered images. It originates on the sunward side of the nucleus, in contrast to the dust tail, which points in the antisolar direction.

In these Laplace-enhanced images, black regions correspond to sharp structural gradients such as jets, tail streamers, shells, or point-like sources, whereas white regions represent flat areas of the coma. The “jet” refers to the narrow, linear, black feature extending roughly northwest in the filtered images (see figures 1 and A.1). It should be noted that the Laplacian filter does not preserve absolute flux; only morphological information and the spatial distribution of features can be reliably inferred from the processed data.

To determine the jet PAs, we applied the methodology described by Serra-Ricart & Licandro (2015). Each original image was first processed with a Laplacian filter, and then transformed into polar coordinates (PA versus radius, see Figure A.2). If the jet represents the two-dimensional projection of an Archimedean spiral, the PA-radius relation becomes approximately linear near the nucleus, transforming the jet into a straight feature in the polar frame. From the filtered polar images, PA profiles were extracted at different radial distances (within ±250 km around 6000 km from the optocenter). For each radius, the jet PA was measured by fitting a parabola to the local intensity minimum within the jet region. A linear regression of the resulting PA measurements yielded the final PA of the jet (at r = 6000 km) and its uncertainty for each epoch (see Fig. A.2). This procedure was applied to all nights in which the jet was clearly detected (see Fig. 1). To improve temporal sampling, several random subsets of 1200 s exposures were independently analyzed for each night when sufficient data were available.

4. Results and discussion

4.1. Coma of 3I

As noted by several observers (Bolin et al. 2025; de la Fuente Marcos et al. 2025; Chandler et al. 2025; Cordiner et al. 2025; Seligman et al. 2025) and shown in Fig. 1, the morphology of the near-nucleus coma (within a projected radius of ∼10 000 km) remained remarkably stable over several weeks, displaying a persistent, nearly sunward dust plume visible since the comet’s discovery (Alarcon et al. 2025; Jewitt et al. 2025). The observed fan-like structure, in the same direction of the jet we detected, can be interpreted as the projection onto the plane of the sky of an emission cone originating from a high-latitude active region on the sunlit hemisphere of the rotating nucleus. A numerical model of the inner coma proposed by Oldani et al. (2025) successfully reproduces the observed morphology by invoking a discrete active source located at a latitude of approximately +75°, with micron-sized dust grains ejected at velocities consistent with gas drag driven by CO2 sublimation.

The coma composition derived from near- and mid-infrared spectroscopy reveals a CO2-dominated volatile budget with a CO2/H2O ratio significantly higher than in typical Solar System comets (Cordiner et al. 2025). Such a composition promotes efficient dust entrainment and contributes to the diffuse, isotropic appearance of the coma. Time-series imaging further indicates that the coma morphology remained globally stable between July and September 2025, although subtle variations in the brightness of the sunward fan were observed, possibly modulated by the nucleus rotation (Santana-Ros et al. 2025).

Polarimetric measurements reveal an unusually strong negative polarization branch and a low inversion angle, indicating that the coma dust of 3I is dominated by large, compact particles. Such a dust population naturally explains the relatively weak effects of solar radiation pressure and the smooth transition between the sunward fan and the antisolar tail. As has been argued by Gray et al. (2025), the deep negative polarization branch can be reproduced by large grains composed of mixed icy and dark materials. Consistently, the pre-perihelion visible spectrum of 3I displays a moderately red slope, likely caused by scattering from large dust grains (Alvarez-Candal et al. 2025).

4.2. Dust tail of 3I

In addition to its nearly symmetric inner coma and prominent sunward fan, 3I exhibits a dust tail that developed progressively as the comet approached the Sun. By mid-August, a tail became clearly apparent in the antisolar direction (Tonry et al. 2025). In our sample (see Table A.1), this tail is detected in images from August 14, 18, 19, 21, 24, and 29, with measured PAs – from isophotal contours – of 100.9°, 102.6°, 101.3°, 100.4°, 102.6°, and 103.3° (yellow lines in Fig. 1, errors of ±0.5°), respectively, in agreement with the antisolar direction (yellow arrows in Fig. 1) of 101.4°, 101.7°, 101.8°, 102.3°, and 102.7° for the same dates.

The feature remained short and diffuse, consistent with weak radiation-pressure effects acting on relatively large dust particles. This morphology suggests that the dust-size distribution is dominated by grains of several tens to hundreds of microns, which experience limited acceleration by solar photons (Santana-Ros et al. 2025). The faint appearance and slow temporal evolution of the tail can therefore be explained by a combination of (i) low ejection velocities, (ii) large average grain size, and (iii) projection effects due to the observing geometry.

4.3. Rotation period of 3I

Assuming that the comet’s aspect angle – defined as the angle between the sky-projected spin axis and the observer’s line of sight – remained approximately constant during the observing timespan, we can also constrain the rotation period from the temporal variability of the jet morphology. For practical purposes, this aspect angle is approximated by the angle of the target’s heliocentric velocity vector (“PsAMV” in the JPL ephemerides) as projected onto the observer’s plane of the sky. Under this approximation, the measured PAs of the two-dimensional jet projection are corrected using the corresponding PsAMV values provided by the orbit ephemerids. Over the August observing interval, the PsAMV varied by only ∼4°, indicating that the viewing geometry was relatively stable. We further assume that the nucleus rotated uniformly throughout the campaign, with no measurable precession or nutation.

We note that the jet is not located exactly at the rotational pole. A perfectly polar jet would produce a strictly constant PA under the nearly fixed viewing geometry of our campaign. Instead, the observed PA exhibits a small but significant modulation (∼12° peak-to-peak; Fig. 2), indicating that the active source lies at high, but not polar, latitude compatible with the model of Oldani et al. (2025). This geometry naturally yields a nearly constant PA with low-amplitude oscillations, consistent with the measured values and enabling the use of PA modulation to infer the rotation period.

Thumbnail: Fig. 2. Refer to the following caption and surrounding text. Fig. 2.

Phase angle of the PA of jet in the inner coma of 3I, measured at 6000 km from the cometary optocenter and phased with the calculated 7.74 ± 0.35 h period. The horizontal red line is the mean value of PA angles representing the sky-projected orientation of the spin axis.

We searched for periodicities in the temporal evolution of the measured PAs using the phase dispersion minimization (PDM) method (Stellingwerf 1978). The best-fit solution corresponds to a period of 7.74 ± 0.35 h (Fig. 2), with the zero phase defined at MJD 60891.1035. If the jet originates from a single active area located near one of the rotational poles, the true nucleus rotation period would be twice this value, i.e., Prot = 15.48 ± 0.70 h. This period, derived from images acquired in August, is slightly shorter than those obtained from independent photometric analyses of data taken about a month earlier, Prot = 16.79 ± 0.23 h (de la Fuente Marcos et al. 2025) and Prot = 16.16 ± 0.01 h (Santana-Ros et al. 2025). The discrepancy may reflect the intrinsic uncertainties of the indirect methods used, or it may indicate an actual change in the rotation period caused by outgassing torques acting on the jet.

From the mean value of the measured jet PAs, the sky-projected orientation of the spin axis was derived (see the horizontal red line in Fig. 2), yielding PA = 280.7 ± 0.2°. Considering the full range of observed PAs, the jet defines a fan or plume extending from PA = 274.7 ± 0.6° to PA = 288.8 ± 0.8°. These values are consistent with the fan orientations reported by other observers. Early imaging obtained on July 2 with the Two-meter Twin Telescope (TTT) revealed a plume at PA = 279.5 ± 1.4° (de la Fuente Marcos et al. 2025), while subsequent Hubble Space Telescope (HST) observations confirmed a similar morphology, showing a well-resolved fan-like feature at PA = 280 ± 10° (Jewitt et al. 2025).

5. Conclusions

In this Letter, we have presented an extensive monitoring campaign of 3I conducted over 37 nights between 2025, July 2 and September 5 with the imaging capabilities of the Two-meter Twin Telescope (TTT), aimed at characterizing the morphology of its coma. Our main conclusions are as follows:

  1. The morphology of the coma evolves from a sunward dust fan in pre-August observations to a more pronounced antisolar tail at later dates (Fig. 1). This delayed development of the tail likely results from the weak influence of solar radiation pressure on the slow-moving coma dust.

  2. A Laplacian-filtering technique (Serra-Ricart & Licandro 2015) applied to the combined images revealed fine-scale structures in the inner coma. A faint but well-defined jet was detected on seven nights (2025, August 3, 5, 18, 19, 21, 24, and 29). Position angle measurements at a projected distance of 6000 km from the cometary optocenter exhibit a periodic modulation centered at ∼280° (Fig. 2), consistent with a high-latitude jet undergoing precessional motion around the sky-projected spin axis. This is the first periodic jet-angle modulation detected in an interstellar comet. These jet-angle oscillations therefore offer a purely morphological route to constraining the spin axis. From the mean value of jet PAs, the sky-projected orientation of the spin axis was determined to be PA = 280.7 ± 0.2°.

  3. The derived periodicity of the jet PA of 7.74 ± 0.35 h may imply a nucleus rotation period of Prot = 15.48 ± 0.70 h, slightly shorter than the value of 16.79 ± 0.23 h reported by de la Fuente Marcos et al. (2025) from the inner-coma photometry.


Acknowledgments

This article is based on observations made in the Two-meter Twin Telescope (TTT (http://ttt.iac.es)) sited at the Teide Observatory of the Instituto de Astrofísica de Canarias (IAC), that Light Bridges operates in Tenerife, Canary Islands (Spain). The observation time rights (DTO) used for this research were consumed in the PEI “PLANETIX25”. This research used storage and computing capacity in ASTRO POC’s EDGE computing center at Tenerife under the form of Indefeasible Computer Rights (ICR). The ICR were consumed in the PEI “PLANETIX25” with the collaboration of Betchle AG. Dr. Antonio Maudes’s insights in economics and law were instrumental in shaping the development of this work. JL acknowledge support from the Agencia Estatal de Investigación del Ministerio de Ciencia e Innovación (AEI-MCINN) under grant “Hydrated Minerals and Organic Compounds in Primitive Asteroids” with reference PID2020-120464GB-100.

References

  1. Alarcon, M. R., Serra-Ricart, M., Licandro, J., et al. 2025, ATel, 17264, 1 [Google Scholar]
  2. Alvarez-Candal, A., Rizos, J. L., Lara, L. M., et al. 2025, A&A, 700, L10 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
  3. Boehnhardt, H., & Birkle, K. 1994, A&AS, 107, 101 [NASA ADS] [Google Scholar]
  4. Bolin, B. T., Belyakov, M., Fremling, C., et al. 2025, MNRAS, 542, L139 [Google Scholar]
  5. Chandler, C. O., Bernardinelli, P. H., Jurić, M., et al. 2025, arXiv e-prints [arXiv:2507.13409] [Google Scholar]
  6. Cordiner, M. A., Roth, N. X., Kelley, M. S. P., et al. 2025, ApJ, 991, L43 [Google Scholar]
  7. de la Fuente Marcos, R., Alarcon, M. R., Licandro, J., et al. 2025, A&A, 700, L9 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
  8. Gray, Z., Bagnulo, S., Borisov, G., et al. 2025, ApJ, 992, L29 [Google Scholar]
  9. Jewitt, D., Hui, M.-T., Mutchler, M., Kim, Y., & Agarwal, J. 2025, ApJ, 990, L2 [Google Scholar]
  10. Kramer, T., Läuter, M., Hviid, S., et al. 2019, A&A, 630, A3 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
  11. Lang, D., Hogg, D. W., Mierle, K., Blanton, M., & Roweis, S. 2010, AJ, 139, 1782 [Google Scholar]
  12. Larson, S. M., & Sekanina, Z. 1984, AJ, 89, 571 [NASA ADS] [CrossRef] [Google Scholar]
  13. Maggiolo, R., Dhooghe, F., Gronoff, G., de Keyser, J., & Cessateur, G. 2025, arXiv e-prints [arXiv:2510.26308] [Google Scholar]
  14. Oldani, V., Manzini, F., Reguitti, A., et al. 2025, ATel, 17350, 1 [Google Scholar]
  15. Samarasinha, N. H., & Larson, S. M. 2014, Icarus, 239, 168 [NASA ADS] [CrossRef] [Google Scholar]
  16. Santana-Ros, T., Ivanova, O., Mykhailova, S., et al. 2025, A&A, 702, L3 [NASA ADS] [CrossRef] [EDP Sciences] [Google Scholar]
  17. Schleicher, D. G., & Farnham, T. L. 2004, in Comets II, eds. M. C. Festou, H. U. Keller, & H. A. Weaver (University of Arizona Press), 449 [Google Scholar]
  18. Sekanina, Z., & Larson, S. M. 1986, Nature, 321, 357 [Google Scholar]
  19. Sekanina, Z., Brownlee, D. E., Economou, T. E., et al. 2004, Science, 304, 1769 [CrossRef] [Google Scholar]
  20. Seligman, D. Z., Micheli, M., Farnocchia, D., et al. 2025, ApJ, 989, L36 [Google Scholar]
  21. Serra-Ricart, M., & Licandro, J. 2015, ApJ, 814, 49 [Google Scholar]
  22. Stellingwerf, R. F. 1978, ApJ, 224, 953 [Google Scholar]
  23. Tonry, J., Denneau, L., Alarcon, M., et al. 2025, ApJ, 995, L15 [Google Scholar]
  24. Ye, Q., Kelley, M. S. P., Hsieh, H. H., et al. 2025, ApJ, 993, L31 [Google Scholar]

Appendix A: Observations and Laplacian-filtering process

3I was extensively monitoring on 37 nights between 2025 July 2 and 2025 September 9 using the imaging capabilities of TTT3 facility (see section 2 for details). Observational circumstances are summarized in Table A.1. Figures A.1 and A.2 show the Laplacian-filtering technique and the method to calculate the PA of the jet, respectively.

Table A.1.

Observing log for 3I/ATLAS

Thumbnail: Fig. A.1. Refer to the following caption and surrounding text. Fig. A.1.

Unprocessed image (left) and Laplacian-filtered image (right) of the inner coma of the interstellar comet 3I/ATLAS (C/2025 N1). The observation date (YYYY–MM–DD), start and end times (UTC), number of sidereal-tracking exposures, and total integration time are indicated above the panels. The projected velocity vector (red arrow) and antisolar direction (yellow arrow) are shown, together with the image scale and orientation. Red crosshairs mark the comet’s optocenter. Isophotal contours of the original (unfiltered) frame are overplotted on the filtered image (right) using ten logarithmically spaced levels between the 20th and 95th percentiles of the pixel-intensity distribution. The jet refers to the narrow, linear, black feature extending roughly northwest in the filtered image. It originates on the sunward side of the nucleus, in contrast to the dust tail, which points in the antisolar direction. The red dotted circle marks a projected radial distance of 6000 km from the optocenter, at which the jet PA is measured.

Thumbnail: Fig. A.2. Refer to the following caption and surrounding text. Fig. A.2.

Left: Polar Laplacian-filtered image of 3I from the August 19 observations (the inset shows the corresponding sky-plane filtered image). From the polar-filtered frames, PA profiles were extracted at several radial distances within ±250 km (dotted red lines) around 6000 km from the optocenter (solid red line). At each radius, the PA of the jet was measured by fitting a parabola to the local intensity minimum in the jet region. Right: Linear regression of the measured PAs as a function of radius yields the final PA jet value (yellow line) with errors (dotted yellow lines) at r = 6000 km.

All Tables

Table A.1.

Observing log for 3I/ATLAS

All Figures

Thumbnail: Fig. 1. Refer to the following caption and surrounding text. Fig. 1.

Laplacian-filtered images of the inner coma of the interstellar comet 3I/ATLAS (C/2025 N1). Thin purple lines indicate the PA of the detected jet (median value when multiple measurements are available), calculated at a projected distance of 6000 km from the comet’s optocenter (dotted red circle). For each frame, the observation date (YYYY–MM–DD) and the start and end times in UTC are shown above the panels, together with the total number of sidereal-tracking exposures and the cumulative integration time. The projected velocity vector (red arrow) and the antisolar direction (yellow arrow) are marked, as well as the image scale and orientation. Degraded orange lines denote the projected spin-axis direction (PA = 280.7 ± 0.2°), derived from mean value of the measured jet PAs, while yellow lines trace the tail direction. Red crosshairs mark the comet’s optocenter. Isophotal contours of the original (unfiltered) images are overplotted using ten logarithmically spaced levels between the 20th and 95th percentiles of pixel intensity in each frame. The jet refers to the narrow, linear, black feature extending roughly northwest in the filtered images. It originates on the sunward side of the nucleus, in contrast to the dust tail, which points in the antisolar direction.

In the text
Thumbnail: Fig. 2. Refer to the following caption and surrounding text. Fig. 2.

Phase angle of the PA of jet in the inner coma of 3I, measured at 6000 km from the cometary optocenter and phased with the calculated 7.74 ± 0.35 h period. The horizontal red line is the mean value of PA angles representing the sky-projected orientation of the spin axis.

In the text
Thumbnail: Fig. A.1. Refer to the following caption and surrounding text. Fig. A.1.

Unprocessed image (left) and Laplacian-filtered image (right) of the inner coma of the interstellar comet 3I/ATLAS (C/2025 N1). The observation date (YYYY–MM–DD), start and end times (UTC), number of sidereal-tracking exposures, and total integration time are indicated above the panels. The projected velocity vector (red arrow) and antisolar direction (yellow arrow) are shown, together with the image scale and orientation. Red crosshairs mark the comet’s optocenter. Isophotal contours of the original (unfiltered) frame are overplotted on the filtered image (right) using ten logarithmically spaced levels between the 20th and 95th percentiles of the pixel-intensity distribution. The jet refers to the narrow, linear, black feature extending roughly northwest in the filtered image. It originates on the sunward side of the nucleus, in contrast to the dust tail, which points in the antisolar direction. The red dotted circle marks a projected radial distance of 6000 km from the optocenter, at which the jet PA is measured.

In the text
Thumbnail: Fig. A.2. Refer to the following caption and surrounding text. Fig. A.2.

Left: Polar Laplacian-filtered image of 3I from the August 19 observations (the inset shows the corresponding sky-plane filtered image). From the polar-filtered frames, PA profiles were extracted at several radial distances within ±250 km (dotted red lines) around 6000 km from the optocenter (solid red line). At each radius, the PA of the jet was measured by fitting a parabola to the local intensity minimum in the jet region. Right: Linear regression of the measured PAs as a function of radius yields the final PA jet value (yellow line) with errors (dotted yellow lines) at r = 6000 km.

In the text

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