the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
JUICE-MAJIS Earth observations during the 2024 gravity assist: first analysis and comparison with PRISMA data
Abstract. The JUpiter ICy moons Explorer spacecraft (JUICE) performed a Lunar-Earth gravity assist maneuver on 20th August 2024, during which the scientific instruments were turned on to test their functionality. At the Earth, the Moon and Jupiter Imaging Spectrometer (MAJIS) acquired a sequence of multispectral images over the Western Pacific Ocean at tropical latitudes. In parallel, an observing campaign was also conducted by the Earth-orbiting PRISMA imaging spectrometer, with the purpose of validating MAJIS spectral observations with independent measurements of the same kind.
These two datasets are here exploited to investigate and compare several atmospheric and cloud properties, including composition, temperatures, and atmospheric gravity waves. In the MAJIS spectral range, covering the 500–5560 nm wavelengths, we identified major and minor atmospheric gases, including O2, H2O, CO2, O3, CH4, N2O. Since MAJIS observations mostly covered diffuse cloudiness over the ocean, our analysis mainly focused on the discrimination of clouds’ properties and altitudes. We verified that ice particles are widespread in the data, allowing for an investigation of their properties (e.g. crystallinity) through different spectral signatures. The only land features identified in MAJIS data are not observed in daylight, hence only a thermal emission analysis is presented. Finally, the coverage of the 4300 nm CO2 band enables the identification of high altitude structures, revealing the presence of several atmospheric wave packets, likely induced by convective events, or lightning strikes known to have occurred at the time of the flyby. The present analysis demonstrates how MAJIS data can contribute to the scientific investigation of an atmospheric environment, and provide the first benchmark in the analysis of water ice, whose characterization in the Jovian system will be of primary importance for the JUICE mission.
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Status: open (until 14 Mar 2026)
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RC1: 'Comment on egusphere-2025-6455', Vincent Kofman, 03 Feb 2026
reply
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AC1: 'Reply on RC1', Fabrizio Oliva, 27 Feb 2026
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Units used on the figures. Figure 2E for instances are in values of radiance (W m-2 sr-1 um-1). Following SI definitions, these should be spectral radiance I think. I know can often be a point of discussion, so if in your experience radiance is correct, then that's fine by me, but please ensure consistency. For instance, in Figure 6B reflectance is used, which is incorrect for the range above 2800 nm. Same for 11E.
- We thank the reviewer for noticing this. We have now updated “spectral radiance” in all figures in which “radiance” was displayed. Also, we now specify at the end of Section 2.3 that, for readability, in the manuscript the term “radiance” is used to refer to “spectral radiance” instead. Moreover, I/F is now used if the quantity is being discussed in the thermal range.
The color scheme used it somewhat unfortunate. Light blue and pink are not easy to see. If the figures are remade, it would be beneficial to make sure they are in a vector based format. Please ensure the titles of the figures are also better labeled.
- All color/title/subtitle updates suggested by the reviewer have been applied. High-resolution figures are going to be uploaded upon the re-submission of the manuscript.
title: 'perhaps reconsider the use of 'first-ever' in the title. Yes, this is the first fly-by of JUICE, but it's certainly not the 'first-ever' flyby by any other spacecraft.
- ‘First-ever’ is not appearing in our manuscript title. However, the special issue is named this way because this is indeed the first-ever flyby taking advantage of both the Earth and the Moon gravity to perform the maneuver.
Line 23 and 51. What is the time difference between the two observations?
- No spatial/temporal coincidence could be achieved and the closest observations are acquired more than 500 km and 2 hours apart. This is expanded in Section 2.1, where Tables 1 and 2 provide details on the observing parameters related to the two datasets.
F2 F... not so helpful?
- We also put panel F in the Figure to show more quantitatively how much different wavelengths are affected by the degradation, which is not readily evident from panel E, being in log scale.
Section 2.3 - 140 and on. Please briefly explain how the spectra in F3 are obtained from spectral radiance. In principle these can just be divided by the spectral radiance of the sun, but what is the spectrum of the Sun used here? MODTRAN is paid-for software, and SPIE is not a journal that is typically available.
- As suggested by the reviewer, reflectances are obtained by dividing the observed spectral radiances by the solar spectrum by Kurucz. This is now specified in the text at the end of Section 2.3. The “newkur” spectrum is available from the website https://earth.gsfc.nasa.gov/climate/projects/solar-irradiance/data (website now cited in the text).
191 cox-munk https://opg.optica.org/josa/abstract.cfm?uri=josa-44-11-838
- We thank the reviewer for the reference. It has now been added in the text.
193. Please clarify whether this is instrumental stray light
- Yes, the effect is instrumental. Straylight assessment is fully described in the companion paper by Langevin et al., submitted to this same issue. We added a reference to this paper in the text.
F3 it looks like there's consistently less flux in the MAJIS spectra below 700 nm. Particularly the decrease in the reflectance is unexpected (F3B top two panels).
- The decrease of flux in MAJIS clouds’ spectra can be explained by different grain size and opacity of the sampled clouds, e.g. F3 in https://doi.org/10.5194/amt-9-4615-2016. This reference has now been added in the text to help understand how sensitive the spectral shape in this range is with respect to aerosols.
Panel F3B with the ocean spectra is slightly cut off. The reflectance of the Earth below 600 nm is pretty high, so it would be good to fully show this range. As this work is partly to assess the performance of the MAJIS instrument, it seems important to highlight the difference between the two instruments.
- The panel is cut off to better show the agreement between the two spectra over the continuum. The information on the difference at lower wavelengths is fully covered in panel A at log scale. The full-range linear-scale figure (that will be provided in the response to the reviewer) makes the comparison longwards of 1000 nm unreadable.
233-234. Not entirely sure that the values below 700 nm are contaminated by scattering See for instance (https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1002/2014RG000449 F13). These are disk integrated spectra, but particularly over relatively dark ocean the Rayleigh tail will be particularly strong.
- We agree with the reviewer that Rayleigh scattering could be playing a role in this range, even if it is not possible to isolate the effects responsible for the differences in Figure 3 (as also different aerosols properties and the presence of straylight could produce similar discrepancies). This explanation has now been added to the text.
F4, the color light blue is hard to see. Is it possible to add the O3 trace in this one too? It's discussed in line 260, so would be relevant to show. I recognize that the figure may be more busy that way, but perhaps an offsets from 1 can be added.
- O3 trace added, light blue color changed to grey.
273. English language detail... Exploit is almost exclusively used in a negative manner. Id suggest using use, study or modeled.
- Done.
F5 caption. These are not reflectances. Furthermore, I think the absolute values here would be super valuable for the community. Is it possible to obtain the spectral radiances here?
- Caption updated and spectral radiances are now displayed.
6A/B. The light blue color is hard to see (I'm not color impaired).
- Color changed.
6B. Similarly to F5, the photons here are not from reflectance, those are emission values.
- Both panels have now been renamed as I/F, which is a radiance ratio without necessarily implying anything about the photon sources.
362. See comment on line 273 regarding the use of exploited. Also used on line 390, 527, 534
- The term has now been changed at all lines.
390.I am not familiar with the K-means classification or the ENVI software package. Please briefly explain what is done here.
- We have updated the description of what the algorithm is doing and referenced further technical details to Tou and Gonzalez, 1974. In brief, the algorithm is capable of grouping the observations into an ensemble of "K" non-overlapping clusters driven by spectral similarity, whose average spectra are representative of the main signatures in the dataset.
393. Not entirely clear what is meant with the term cluster
- Changed to “average spectra”. See also response to previous comment.
Section lines 389-417 would benefit from some some restructuring. There a lot of information here, but it is hard to follow.
- On the basis of the reviewer’s suggestion, the paragraph has been reworked.
F8. Light green and light blue are both colors that are tricky to see on a white background. Please consider modifying.
- Colors changed to green and grey respectively.
Not clear what the different traces are. Are these identified by the K-means classification? The statement 'colors are ordered with increasing reflectance of the 1700 nm from (cyan to green)' is confusing. Please clarify the use of colors, and label the sub figures with titles that are slightly more helpful.
- Color legend added to each panel and Figure caption updated accordingly.
Consider relabeling the radiance to spectral radiance here.
- Done.
479 'Only the last three can be appreciated in the MAJIS spectra'. Consider replacing appreciated with 'are visible' or 'can be distinguished'. The mean is the same, the statement 'can be appreciated' suggest a value of beauty, which is inappropriate here. (Although I do recognize that the observations are of exquisite quality and definitely appreciate the work and analysis performed here!)
- Replaced with “detected”.
F11. Change the title to the ones corresponding to Tables 1 and 2 and add a clear time stamp (i.e. add spaces to the number string), 20240920024630_20240820024634_0001 is not a helpful title for a sub-figure.
- Done
F11 E&F. Please consider relabeling, the photons about 2700nm are not from reflected light. Refrain from using light blue as a color.
- Y axis relabeled to I/F for both panels, color updated.
F11 E&F These figure panels could probably be combined, this may help visualizing the slopes of the spectral radiance between the two different instruments.
- Instead of making a radiometric/spectral comparison here (already discussed in Figure 3), the purpose of panels E and F is to show that spectra related to the pixel masks in panels C and D do indeed show the spectral signatures typical of ocean, liquid water clouds and ice clouds, as discussed at the beginning of Section 4.1. Moreover, a combined image (that will be provided in the response to the reviewer) would look a bit too crowded.
637. Probably helpful here to remind the reader of the time difference between these two observations.
- We are not sure if the reviewer is referring to the observations in Figure 11. If this is the case, now the UTC times of both observations are displayed in panels from A to D.
F12 consider subfigure titles
- Done.
F13 consider using 'spectral radiance'. Please relabel the sub-figures.
- Done.
F16A It is hard to see what the cloud top height is here for the untrained eye. The text mentioned 10KM, consider making this clearer in the figure by making the 10 KM bold for instance.
- The figure is now updated with larger fonts.
763 The use of 'of course' here seems what colloquial
- Removed.
765 'quick and robust way for estimating'. I don't want to change the meaning of the sentence, but 'quick and robust way of estimating' seems a bit of a contradiction in terms, and actually quite labor intensive. Perhaps 'independent method of estimating the ... ' describes it better?
- Rephrased to “quick and independent”.
F19 caption. I don't think I understand the 'samples and number of lines' description. Is the point here that these are maps where the pixels aren't directly assigned to a location? In principle this is not an issue, but the meaning of 'lines' and 'samples' isn't clear. I'd suggest to just remove the number on the axis as the message seems more descriptive than absolute here?
- As the reviewer says, these maps do not directly refer to specific longitude-latitude coordinates. The ‘samples’ indicate the spatial pixels in the spectrometer’s slit, while ‘lines’ refer to adjacent acquisitions of the slit in the cube. This explanation was already given in F16 caption and we now also added it in F19 for consistency.
917-918 and 920. I would avoid the use of 'of course' here. It doesn't help clarify what is described and could be perceived as condescending.
- Removed.
932: summary of atmospheric wave parameters ... add the 'atmospheric wave'. Unspecified use of 'parameters' can be confusing. We're at figure 20 and table 5 now, good to help readers keep track of material! The table might also move around in the editorial process, being not directly under the subheading.
- ‘Atmospheric wave’ is now added in the caption, along with the list of the provided parameters.
F23. Suggest to make the spectra larger, text is hard to read unless reader can zoom in on the figures. I would also think the paper would benefit from vector-based images, this makes them much more clear, particularly if one wants to zoom in on the details. What is going on at 2300 nm btw? Is this an artifact from switching detector types perhaps? If so, mention this in the caption perhaps.
- Figure panels have been rearranged to be larger. Regarding the 2300 nm noisy region, it is due to the boundary between MAJIS VISNIR and IR channels and it has been now removed from the plot since not useful for the discussion
Citation: https://doi.org/10.5194/egusphere-2025-6455-AC1
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AC1: 'Reply on RC1', Fabrizio Oliva, 27 Feb 2026
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- 1
This work describes and expansive analysis of the observations of the Earth from space by the Moon and Jupiter Imaging Spectrometer (MAJIS) on board the JUICE mission during a gravity assist passage by the Earth. The analysis spans the full wavelength range of the instrument, starting at reflected light from 500 to about 2800 nm, and including emitted light from the Earth surface and atmosphere from 3-5.5 um. The work spans a wide range of different strategies over spectroscopic windows. The analysis are very detailed and where possible results are verified between them.
The paper is well written and the results are clearly presented. I have no doubt that the work presented here is an excellent preparation for the analysis of the observations in the Jupiter system. The results presented may also prove to be of direct relevance to the Earth science community.
I have no reservations about recommending this manuscript for publication, but I would strongly recommend addressing the following issues though. The other points are minor or textual things.
1. Units used on the figures. Figure 2E for instances are in values of radiance (W m-2 sr-1 um-1). Following SI definitions, these should be spectral radiance I think. I know can often be a point of discussion, so if in your experience radiance is correct, then that's fine by me, but please ensure consistency. For instance, in Figure 6B reflectance is used, which is incorrect for the range above 2800 nm. Same for 11E.
2. The color scheme used it somewhat unfortunate. Light blue and pink are not easy to see. If the figures are remade, it would be beneficial to make sure they are in a vector based format. Please ensure the titles of the figures are also better labeled.
Please see the list of minor comments below.
title: 'perhaps reconsider the use of 'first-ever' in the title. Yes, this is the first fly-by of JUICE, but it's certainly not the 'first-ever' flyby by any other spacecraft.
Line 23 and 51. What is the time difference between the two observations?
F2 F... not so helpful?
Section 2.3 - 140 and on. Please briefly explain how the spectra in F3 are obtained from spectral radiance. In principle these can just be divided by the spectral radiance of the sun, but what is the spectrum of the Sun used here? MODTRAN is paid-for software, and SPIE is not a journal that is typically available.
191 cox-munk https://opg.optica.org/josa/abstract.cfm?uri=josa-44-11-838
193. Please clarify whether this is instrumental stray light
F3 it looks like there's consistently less flux in the MAJIS spectra below 700 nm. Particularly the decrease in the reflectance is unexpected (F3B top two panels). Panel F3B with the ocean spectra is slightly cut off. The reflectance of the Earth below 600 nm is pretty high, so it would be good to fully show this range. As this work is partly to assess the performance of the MAJIS instrument, it seems important to highlight the difference between the two instruments.
233-234. Not entirely sure that the values below 700 nm are contaminated by scattering See for instance (https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1002/2014RG000449 F13). These are disk integrated spectra, but particularly over relatively dark ocean the Rayleigh tail will be particularly strong.
F4, the color light blue is hard to see. Is it possible to add the O3 trace in this one too? It's discussed in line 260, so would be relevant to show. I recognize that the figure may be more busy that way, but perhaps an offsets from 1 can be added.
273. English language detail... Exploit is almost exclusively used in a negative manner. Id suggest using use, study or modeled.
F5 caption. These are not reflectances. Furthermore, I think the absolute values here would be super valuable for the community. Is it possible to obtain the spectral radiances here?
6A/B. The light blue color is hard to see (I'm not color impaired).
6B. Similarly to F5, the photons here are not from reflectance, those are emission values.
362. See comment on line 273 regarding the use of exploited. Also used on line 390, 527, 534
390. I am not familiar with the K-means classification or the ENVI software package. Please briefly explain what is done here.
395. Not entirely clear what is meant with the term cluster
Section lines 389-417 would benefit from some some restructuring. There a lot of information here, but it is hard to follow.
F8. Light green and light blue are both colors that are tricky to see on a white background. Please consider modifying.
Not clear what the different traces are. Are these identified by the K-means classification? The statement 'colors are ordered with increasing reflectance of the 1700 nm from (cyan to green)' is confusing. Please clarify the use of colors, and label the sub figures with titles that are slightly more helpful.
Consider relabeling the radiance to spectral radiance here.
479 'Only the last three can be appreciated in the MAJIS spectra'. Consider replacing appreciated with 'are visible' or 'can be distinguished'. The mean is the same, the statement 'can be appreciated' suggest a value of beauty, which is inappropriate here. (Although I do recognize that the observations are of exquisite quality and definitely appreciate the work and analysis performed here!)
F11. Change the title to the ones corresponding to Tables 1 and 2 and add a clear time stamp (i.e. add spaces to the number string)
20240920024630_20240820024634_0001 is not a helpful title for a sub-figure.
F11 E&F. Please consider relabeling, the photons about 2700nm are not from reflected light. Refrain from using light blue as a color.
F11 E&F These figure panels could probably be combined, this may help visualizing the slopes of the spectral radiance between the two different instruments.
637. Probably helpful here to remind the reader of the time difference between these two observations.
F12 consider subfigure titles
F13 consider using 'spectral radiance'.
Please relabel the sub-figures.
F16A It is hard to see what the cloud top height is here for the untrained eye. The text mentioned 10KM, consider making this clearer in the figure by making the 10 KM bold for instance.
763 The use of 'of course' here seems what colloquial
765 'quick and robust way for estimating'. I don't want to change the meaning of the sentence, but 'quick and robust way of estimating' seems a bit of a contradiction in terms, and actually quite labor intensive. Perhaps 'independent method of estimating the ... ' describes it better?
F19 caption. I don't think I understand the 'samples and number of lines' description. Is the point here that these are maps where the pixels aren't directly assigned to a location? In principle this is not an issue, but the meaning of 'lines' and 'samples' isn't clear. I'd suggest to just remove the number on the axis as the message seems more descriptive than absolute here?
917-918 and 920. I would avoid the use of 'of course' here. It doesn't help clarify what is described and could be perceived as condescending.
932: summary of atmospheric wave parameters ... add the 'atmospheric wave'. Unspecified use of 'parameters' can be confusing. We're at figure 20 and table 5 now, good to help readers keep track of material! The table might also move around in the editorial process, being not directly under the subheading.
F23. Suggest to make the spectra larger, text is hard to read unless reader can zoom in on the figures. I would also think the paper would benefit from vector-based images, this makes them much more clear, particularly if one wants to zoom in on the details. What is going on at 2300 nm btw? Is this an artifact from switching detector types perhaps? If so, mention this in the caption perhaps.