the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Small Uncrewed Aircraft Based Microphysical Measurements of Polar Stratus Cloud During The Pallas Cloud Experiment 2022
Abstract. A dataset of in-situ observations of stratus cloud microphysics was created from measurements performed at the Pallas atmosphere-ecosystem super site. The data were collected using a small uncrewed aircraft (SUA) and the low-cost, lightweight Universal Cloud and Aerosol Sounding System (UCASS, Smith et al., 2019). Data from the instrument – platform combination was previously validated in Girdwood et al. (2022b) during a similar field campaign at the same site. The dataset contains cloud droplet size distribution, number concentration, and mass concentration, in addition to geolocation data, and meteorological variables. The flight pattern of the SUA was planned to provide a quasi-vertical profile. A total of 84 of these profiles across 39 flights were performed during the campaign period. The data from the SUA flights are available from 10.5281/zenodo.14756233 (Girdwood et al. 2022a).
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Status: final response (author comments only)
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RC1: 'Comment on essd-2025-257', Anonymous Referee #1, 05 Sep 2025
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AC1: 'Reply on RC1', Jessica Girdwood, 24 Dec 2025
## Response to RC1
---# General Comments
- The UAV profiles were all up to a set altitude of 2 km above ground level
which was the legal limit. The cloud tops were beneath this limit for all but
two of these profiles. The flight information section did contain this.
Overall, instead of a separate section, the discussion of the cloudy conditions
has been expanded upon in this section.
- the flight information and constraints section was renamed to "flight
information and conditions"
- information, however it has been made more plain
- The "Data analysis and qa" section was amended to explain all the derived cloud
properties in the dataset.# Specific Comments
- added "during the Pallas Cloud Experiment - 2022" on Line 2
- "These measurements are intended to expand on the previous campaign since
they form an extended dataset with the uncertainties already evaluated by
previous experimental work" added to this line.
- I have added a paragraph in the introduction to explain the difference
between this and my previous work. It's worth stating that I am actually the
same author as Girdwood et al 2022, I have just changed my name since then.
- climate models changed to earth system models on L10.
- Specific references to polar clouds added.
- I added a clarification of the intended use case of the dataset at the end of
the introduction since it made more sense to put it here after I introduce
the SUA, instrument, location, etc.
- rephrased L11 to clarify
- UCASS explanation moved to L22 and more citations of previous use given. The
UCASS is described in detail later in the paper, this is now cross
referenced.
- Altered the section headings to remove method section and move its
subsections up a level, since there is already a more
specific flight information section.
- The abbreviation was actually a corrupted reference which is now fixed.
- The flight in Fig. 3 was very characteristic, and the caption has been
updated to reflect this. Any attempt at plotting multiple profiles resulted
in an unreadable plot, though I am colourblind so this probably does not help.
- The spatial resolution of the data depends on the ground speed and ascent speed
of the aircraft. This changed throughout the campaign as a result of changes
in wind speed. The dataset is in the time domain in order to comply with the
data standards for the rest of the campaign outlined in Brus et al 2025. The
manuscript has been amended to reflect this.
- "one of a number of algorithms" is now expanded upon in the data analysis
section, which now has a relevant cross reference.
- data analysis and quality assurance sections split apart.
- the constraining conditions for the UCASS being referred to here are the AoA
and airspeed limits, which are discussed in the flight information section.
This has now been cross referenced and expanded upon.
- The reason for the choice of these limits was engineering constraints with
the UCASS, which was previously stated in the flight information and
apparatus sections.
- Expanded the apparatus section to include information on UCASS uncertainty.
- Line 101 was rephrased
- Added paragraph discussing co-location error at the end of data QA.
- The altitude is above sea level, this was clarified in the text. There is no
minimum altitude, just the take off altitude.
- Figures 5 and 6 have been altered to include the error for other reviewers
comments.
- I added references to the exact equations used to calculate corrected airspeed.
- The take off site was the same each time, and the profiles were very similar
and only changed in orientation with different wind directions. This was
added to the text already in response to a different comment.
- A paragraph was added to the summary with the intended uses of the data.# Technical
- date now added to citation on L74.
- L94 QA now spelled out.
- L109 the manuscript is reformatted following publication anyway and the
spacing of section titles is changed when the two column format is
implemented.
- SHT and BME are just the names of the sensors, and AG is a broken reference
which is now fixed.Citation: https://doi.org/10.5194/essd-2025-257-AC1
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AC1: 'Reply on RC1', Jessica Girdwood, 24 Dec 2025
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RC2: 'Comment on essd-2025-257', Anonymous Referee #2, 19 Sep 2025
The manuscript presents a dataset of in situ data of polar stratus clouds collected from a fixed-wing small uncrewed aircraft (SUA) during the Pallas Cloud Experiment (PaCE) 2022 at the Pallas atmosphere-ecosystem super site. The dataset over 39 flights with 84 quasi-vertical profiles includes data on cloud droplet size distributions including derived products (number concentration, liquid water content, effective radius), meteorological variables, and SUA flight data. A quality check was performed on the data and different processing depths (“a1” and “c1”) were applied.
General comments:
- I’m not sure if the dataset now only includes measurements of “arctic warm stratus” (line: 32), or also arctic cold stratus / mixed-phase clouds (line 104: “ice while flying”, line: 136 mixed-phase clouds).
- If you were also measuring mixed-phase clouds and aerosols (line: 53) how did you handle the discrimination between cloud droplets, ice crystals, and aerosols? Also, due to their very different refractive indices that could affect the measurement. This could strongly influence the measure cloud droplet size distribution and derive variables.
If you measure cold cloud or mixed-phase conditions a flag in the data set would be helpful, and some short sentences on how you define these temperature regimes, i.e., using the BME temperature or other instruments. - You could also include a “QA masking impact”, i.e., how much of the respective flight/profile (e.g., the fraction) was masked.
- What is largely missing in the manuscript is a compact uncertainty budget for (a) sizing (e.g., due to refractive-index / model dependence), (b) counting / concentration (e.g., sample volume), (c) LWC (e.g., density assumption, mixed-phase conditions), and (d) airspeed substitutions when the pitot tube froze (e.g., ground-station wind - based correction). Particularly the latter considering the wind speeds were presumably measured on ground level.
- Please extend the analysis part of the data on how the variables are derived from the particle size distribution measurements. Which processes “proc” were actually used.
- Summary/Conclusion: This part is very short and missing an outlook on what the dataset could be used for or how it could support other datasets if used in synergy. Mainly what is the fundamental value for future studies.
Specific comments:
- Line 117-119: This should go into the data analysis part, where you introduce the masks.
- Figure 5: Number concentration of cloud droplets, aerosols or both?
Do you always show the same x-range?
Are the concentration values saturated (e.g., profile 6) or just not displayed due to the x-axis range? - Figure 6: The x-axis label is confusing looks like “510”, please at least include the ticks for every profile. Also here particularly evident is that you need to give some error estimates. Comparing profile 002 with 011 already indicates that due to counting statistics the uncertainty for 002 is higher compared to profile 011.
- Line 120: Level “c1” means that the flight controller data was available and “a1” where it was not available? Please clarify.
- Line 117: What do you mean by “The data level is also included here.” This needs more explanation, what is a data level?
Minor comments:
- Line 44: what is (noa,a) after pitot tube?
- Line 56, 116: what is (noa,b)?
- Line 68: include space between 15° and angle
- Lines 69,70, 99, 100: include small space between unit m\,s
- Line 74: check reference year number
- Line 75: Period missing
- Line 101: remove first “time”
- Table 1: kg\,m^-3
- 115: I thin the company is called Sensirion not Senserion
- 116: Change “Bosh” to “Bosch”
- 119: altitude not attitude :)
- Table 2: define n/a in description (not available vs not applicable)
- Throughout: change in-situ to in situ
Citation: https://doi.org/10.5194/essd-2025-257-RC2 -
AC3: 'Reply on RC2', Jessica Girdwood, 24 Dec 2025
## Response to RC2
---# General Comments
- Warm cloud changed to liquid cloud. There were no ice crystals in this cloud
but there were supercooled droplets which froze on impact with the airframe.
The manuscript has been changed to reflect this.
- Droplets and ice crystals are discriminated against by size fraction
separation. The scattering geometry of the UCASS means any ice encountered
during the flights will have a scattering cross section beyond the range of
detection. In addition, the probability of encountering an ice crystal during
measurements at this time of year is negligible. The manuscript was changed
to state this with the relevant references in the flight information section.
- A section on data analysis was added for reviewer #1 and I think this also
covers your comment here :)
- A paragraph at the end of the summary was added to explain the intended uses
of the dataset.
- The data levels are consistent with the rest of the papers in this ESSD
special edition for the PACE22 campaign. An explanation of this and the
relevant reference was added to the manuscript.
- I have added standard error to the effective radius plot in addition to a
discussion in the manuscript.# Specific Comments (response in order)
- broken reference which is now fixed
- broken reference which is now fixed
- L68 spacing now fixed
- half space now added
- Year number added
- full stop added to end of sentence
- This sentence was reworded for a different reviewer :)
- spacing corrected
- Senserion changed to Sensirion
- bosh changed to bosch
- attitude is an aviation term which refers to the angular position of an airframe in
space, which is what i meant in this instance.
- n/a defined in caption of Table 2.
- changed in-situ to in situCitation: https://doi.org/10.5194/essd-2025-257-AC3
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RC3: 'Comment on essd-2025-257', Anonymous Referee #3, 01 Oct 2025
The manuscript describes a dataset collected in 2022 to understand cloud microphysics using a small UAS. The article contains useful information regarding the UCASS sensor and the available data. The platform would be beneficial for addressing the data gap in in-situ cloud observations. However, the manuscript lacks some key information about data processing.
General Comments:
I think it would benefit the reader if there was more description about how this article differs and expands upon the work from Girdwood et al. 2022b. As the introduction stands now, I do not see how this dataset is unique or what was learned from the previous campaign.
There should be more description on the data processing mentioned in Software. The authors mention that there is space for customization but do not describe the standard practice used on the dataset herein. Overall, the description of the QA process needs to be expanded. I do not understand the processes which went into creating the c1 level files.
The meteorological observations (T and RH) are mentioned but never described in their data quality or availability. I would imagine condensation on the sensors could pose an issue, but this is not mentioned, nor do we see any examples of meteorological data plotted in the manuscript. Were there any calibration offsets or post-processing to ensure accurate measurements?
The doi links in the Abstract and Data Availability statement do not work.
Specific Comments:
L4: It would be nice to add the year of the Girdwood 2022b campaign to distinguish the two datasets better.
L20: Have there been other UAS to gather cloud physics observations? If so, they should be mentioned in the introduction.
L41: What is (noa, a)?
L44-L47: All of the pointing to references to describe the data processing makes it hard to follow.
L54-56: Are there any differences between these two sensors? Or in their respected data quality?
Fig 3: You might consider adding a satellite image to understand the cloud types and coverage in the flight path.
L102: Are there differences in data quality between ascending profiles and descending? How is the concern for rotor-wash influence on the environment mediated?
L104: This seems like a fundamental issue given the goals of the platform. How often was the pitot tube unusable? Does that reduce the frequency of observations?
L128: Fix the citation
Citation: https://doi.org/10.5194/essd-2025-257-RC3 -
AC2: 'Reply on RC3', Jessica Girdwood, 24 Dec 2025
## Response to RC3
### Jessica Girdwood
---### General Comments
- The purpose of the previous campaign was to validate the technique used to
gather these data. During the 2020 experiment, we flew the aircraft --
instrument combination in a number of configurations with a number of flight
paths to experiment with how is best to gather these data. The introduction
was expanded as part of another reviewers comments and I think that this is now
clearer :)
- The data analysis and data QA sections were split apart, and the data
analysis was greatly expanded upon, I hope that this is now clear.
- description of temperature sensor and housing added to the end of the
apparatus section. Condensation on the sensor is an expansive issue with
in-cloud temperature measurements and sparks a lot of debate in conventional
aircraft measurement spaces. Solving this issue here is considered beyond the
scope of this paper.
- Links are now fixed.### Specific comments (in order)
- Date is now added for clarification.
- The introduction was expanded upon with links to previous campaigns.
- a broken reference which is now fixed
- I'm not 100% sure what you mean by this, though the description of the UCASS
was greatly expanded upon for another reviewer which I think might address
this comment.
- the only difference between the two UCASS variants is the size range, there
is no difference in data quality.
- unfortunately there was no satellite data. However I have added a more
detailed description of the cloudy conditions and type of cloud encountered.
- Yes. I discussed this in detail in Girdwood et al 2020, 2022. Rotor wash is not an
issue here because this is a fixed wing SUA and it does not fly through its
own wake at any point. I have altered the manuscript to state this.
- you're right, this is an issue. I have recently worked on an upgrade to the
UCASS which includes a hot wire airspeed sensor which does not have this
issue, but it was unfortunately not ready in time for these experiments. The
associated error with the corrected airspeed is now mentioned in the text, and
the affected profiles can be found in table 2.
- Fixed the citation.Citation: https://doi.org/10.5194/essd-2025-257-AC2
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AC2: 'Reply on RC3', Jessica Girdwood, 24 Dec 2025
Data sets
Data From the Universal Cloud and Aerosol Sounding System Abord an Uncrewed Aircraft During the Pallas Cloud Experiment 2022 Jessica Girdwood et al. https://doi.org/10.5281/zenodo.14756233
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The authors present cloud micro-physical measurements taken by the UCASS optical particle spectrometer aboard a small uncrewed aircraft (SUA) during the Pallas Cloud Experiment 2022. The manuscript provides a good overview on the used instrument and data products, and illustrates an example of measurements. I am lacking some information on the retrievals used and a discussion of their uncertainties and limitations. I recommend publication of the manuscript after the following comments have been addressed by the authors.
General comments
mass and number concentration and effective radius (Tab 1) calculated and what errors and limitations arise from the retrievals and assumptions therein? How is phase information taken into account when retrieving in mixed-phase or ice cloud conditions? I would suggest to add a sub-section to either Sec 2 or 3 illustrating this currently missing information on the dataset.
Specific comments
Abstract
Sec 1: Introduction
Sec 2: Methods
Sec 3: Data
Minor xtick labels should be added to all respective flights sub-panels at the bottom. Are all panels showing the same xrange? It would be nice to add ‘10’ and ‘20’ to the top x-ticks.
It seems like lines are connecting points throughout clear air patches (eg Fig 6 profiles 25-28 between 750-1200m). Replacing lines with plotted dots would further illustrate the vertical resolution of the measurements.
Summary
Technical Corrections