pith. sign in

arxiv: 2605.21509 · v1 · pith:RYIIOQMGnew · submitted 2026-05-12 · ⚛️ physics.flu-dyn · physics.ao-ph· physics.chem-ph

Tracking water vapor homogeneous nucleation and droplet growth with spectroscopy and holography in a free expansion cloud chamber

Pith reviewed 2026-05-22 01:46 UTC · model grok-4.3

classification ⚛️ physics.flu-dyn physics.ao-phphysics.chem-ph
keywords homogeneous nucleationwater vaporsaturation ratioexpansion chamberTDLASholographydroplet growthmixing effects
0
0 comments X

The pith

Homogeneous nucleation of water vapor occurs at saturation ratio near 5.

A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.

The paper sets up a rapid expansion chamber to observe water vapor turning into liquid droplets under controlled conditions. Tunable diode laser absorption spectroscopy measures the remaining vapor while in-line holography records the number and size of new droplets as the expansion proceeds. From these combined readings the authors extract the peak saturation ratio reached in each run and identify the point where nucleation reliably begins. This threshold matches earlier reports and the predictions of classical nucleation theory. The measurements also expose how mixing and turbulence inside the chamber alter droplet growth after the initial nucleation event.

Core claim

In the rapid expansion aerosol chamber, TDLAS tracks vapor concentration while holography tracks droplet size and number throughout the expansion. Peak saturation ratios are retrieved from the TDLAS data together with adjusted thermocouple temperatures. Nucleation begins once the saturation ratio reaches a threshold near S=5, in agreement with prior literature and classical nucleation theory. Average droplet diameter and concentration trends indicate warm air pockets near the walls mix inhomogeneously with colder central air. Forced mixing with fans improves spatial temperature uniformity yet broadens the droplet size distribution.

What carries the argument

Combined TDLAS vapor-concentration measurements and in-line holography droplet tracking inside a free-expansion cloud chamber.

If this is right

  • Nucleation onset is observed near S=5 and aligns with classical nucleation theory.
  • Droplet number and growth rates vary with the degree of post-expansion mixing.
  • Forced mixing improves temperature uniformity across the chamber volume.
  • The dual optical techniques can follow both vapor and liquid phases at the high supersaturations required for homogeneous nucleation.

Where Pith is reading between the lines

These are editorial extensions of the paper, not claims the author makes directly.

  • The same chamber and diagnostics could test nucleation thresholds for other condensable vapors under varying expansion rates.
  • Accounting for wall-driven mixing may refine models that predict droplet spectra in turbulent clouds.
  • Coupling these measurements to fluid simulations could quantify how small-scale temperature fluctuations control nucleation timing.

Load-bearing premise

The saturation ratio derived from TDLAS vapor readings and adjusted thermocouple temperatures accurately reflects the conditions at the chamber center that trigger nucleation.

What would settle it

Direct local measurements at the chamber center that yield saturation ratios markedly different from the TDLAS-derived values at the moment nucleation is first detected would falsify the reported threshold.

Figures

Figures reproduced from arXiv: 2605.21509 by Cole R. Sagan, Gwenore F. Pokrifka, Ilian Ahmed, Luc Deike, Marissa L. Weichman, Martin A. Erinin, Nadir Jeevanjee, Samuel M. Koblensky.

Figure 1
Figure 1. Figure 1: FIG. 1 [PITH_FULL_IMAGE:figures/full_fig_p004_1.png] view at source ↗
Figure 2
Figure 2. Figure 2: FIG. 2 [PITH_FULL_IMAGE:figures/full_fig_p008_2.png] view at source ↗
Figure 4
Figure 4. Figure 4: FIG. 4. Evolution of water vapor and droplet statistics over [PITH_FULL_IMAGE:figures/full_fig_p010_4.png] view at source ↗
Figure 7
Figure 7. Figure 7: FIG. 7. Evolution of droplet size distributions for the same [PITH_FULL_IMAGE:figures/full_fig_p012_7.png] view at source ↗
read the original abstract

We use a newly commissioned rapid expansion aerosol chamber (REACh) facility to study the homogeneous nucleation of water vapor to form liquid droplets. We perform high-speed measurements to track the partitioning of water into vapor and droplets throughout the expansion process, including tunable diode laser absorption spectroscopy (TDLAS) to access the vapor concentration and in-line holography to track the size and concentration of nucleating droplets. We retrieve the peak saturation ratio achieved in each expansion from the TDLAS measurements in combination with adjusted thermocouple temperature readout. We monitor the number of nucleated droplets and their subsequent growth as a function of saturation ratio, and observe the onset of homogeneous nucleation of water vapor occurring at a threshold saturation ratio near $S=5$, in agreement with prior literature and classical nucleation theory. The trends we observe in average diameter and droplet concentration suggest that warm air pockets near the chamber walls inhomogeneously mix with cold air at the center of the chamber following expansion. Active forced mixing with fans yields more spatially uniform temperature readings across the chamber, but also significantly broadens the droplet size distribution. Our results demonstrate the capability of TDLAS and holography techniques to track both water vapor and liquid water in the high saturation ratio environments necessary for the homogeneous nucleation of droplets. Our findings also reveal that droplet nucleation and growth dynamics are highly sensitive to turbulence.

Editorial analysis

A structured set of objections, weighed in public.

Desk editor's note, referee report, simulated authors' rebuttal, and a circularity audit. Tearing a paper down is the easy half of reading it; the pith above is the substance, this is the friction.

Referee Report

1 major / 2 minor

Summary. The manuscript reports experiments in a newly commissioned rapid expansion aerosol chamber (REACh) using tunable diode laser absorption spectroscopy (TDLAS) to measure vapor concentration and in-line holography to track droplet size and number density during free expansions of water vapor. The central claim is that homogeneous nucleation onsets at a threshold saturation ratio near S=5, consistent with classical nucleation theory and prior literature; the authors also report that post-expansion inhomogeneous mixing of warm wall pockets with cold center air affects droplet growth, while forced mixing broadens the size distribution.

Significance. If the local saturation ratio at the nucleation site is accurately determined, the work provides useful high-speed, in-situ diagnostics for tracking both vapor and liquid partitioning in high-supersaturation expansions. The demonstration of combined TDLAS and holography techniques, together with the explicit discussion of mixing-induced spatial nonuniformity, could inform the design of future cloud-chamber studies in fluid dynamics and aerosol science.

major comments (1)
  1. [Abstract and Results] Abstract and Results: The peak saturation ratio is obtained from path-averaged TDLAS vapor concentration combined with an 'adjusted' thermocouple temperature. The manuscript itself notes inhomogeneous mixing of warm wall pockets with cold center air after expansion. Because TDLAS is line-of-sight and the thermocouple is a point measurement, spatial gradients will cause the derived S to differ from the local value at the chamber center where nucleation occurs. The adjustment procedure is unspecified; this directly affects the validity of the reported threshold S≈5 and must be detailed with validation (e.g., comparison to local probes or CFD) before the onset claim can be accepted.
minor comments (2)
  1. [Results] The abstract states that forced mixing 'significantly broadens the droplet size distribution'; include quantitative metrics (e.g., standard deviation or polydispersity index) and corresponding holography images or histograms to support this observation.
  2. [Methods] Clarify the temporal resolution and spatial averaging inherent to the TDLAS and holography measurements when reporting the 'onset' timing relative to the expansion.

Simulated Author's Rebuttal

1 responses · 0 unresolved

We thank the referee for their careful and constructive review of our manuscript. We address the major comment on the saturation ratio determination below and have revised the manuscript to improve transparency on this point.

read point-by-point responses
  1. Referee: The peak saturation ratio is obtained from path-averaged TDLAS vapor concentration combined with an 'adjusted' thermocouple temperature. The manuscript itself notes inhomogeneous mixing of warm wall pockets with cold center air after expansion. Because TDLAS is line-of-sight and the thermocouple is a point measurement, spatial gradients will cause the derived S to differ from the local value at the chamber center where nucleation occurs. The adjustment procedure is unspecified; this directly affects the validity of the reported threshold S≈5 and must be detailed with validation (e.g., comparison to local probes or CFD) before the onset claim can be accepted.

    Authors: We agree that the adjustment procedure for the thermocouple temperature was insufficiently detailed and that spatial inhomogeneities warrant explicit discussion. In the revised manuscript we have added a dedicated paragraph in the Methods section describing the adjustment: it is derived from pre-expansion calibration runs comparing thermocouple readings to independent pressure-based temperature estimates under uniform conditions, with a small empirical correction applied to account for wall heat transfer observed in the post-expansion phase. We also clarify that the TDLAS beam traverses the central volume where holography confirms nucleation first appears, and that the reported onset occurs at the end of the rapid expansion before significant wall-pocket mixing develops (as evidenced by the timing of droplet appearance in the holography data). While we acknowledge that full CFD validation or additional local probes would further strengthen the local S estimate, the consistency of our threshold with classical nucleation theory and prior literature, together with the direct observation of nucleation timing, supports the reported value. We have expanded the discussion of uncertainties arising from path averaging. revision: yes

Circularity Check

0 steps flagged

No significant circularity; experimental observations compared to external literature

full rationale

The paper is an experimental study that measures vapor concentration via TDLAS, temperature via thermocouple, and droplet properties via holography during chamber expansions. The central claim reports an observed nucleation onset threshold near S=5 and notes agreement with prior literature and classical nucleation theory. Saturation ratio is retrieved from direct measurements rather than derived or fitted from the nucleation data itself. No equations or steps reduce the reported threshold to a self-definition, a fitted input renamed as prediction, or a self-citation chain. The work remains self-contained against external benchmarks, with any mixing inhomogeneity concerns falling under measurement accuracy rather than circularity.

Axiom & Free-Parameter Ledger

0 free parameters · 1 axioms · 0 invented entities

The central claim rests on standard assumptions in thermodynamics and fluid dynamics for interpreting saturation ratios and droplet growth; no free parameters or invented entities are evident from the abstract.

axioms (1)
  • domain assumption Classical nucleation theory provides the expected threshold for homogeneous nucleation of water vapor.
    The paper compares observations to this theory for validation.

pith-pipeline@v0.9.0 · 5821 in / 1210 out tokens · 63600 ms · 2026-05-22T01:46:45.430372+00:00 · methodology

discussion (0)

Sign in with ORCID, Apple, or X to comment. Anyone can read and Pith papers without signing in.

Lean theorems connected to this paper

Citations machine-checked in the Pith Canon. Every link opens the source theorem in the public Lean library.

  • IndisputableMonolith/Cost/FunctionalEquation.lean washburn_uniqueness_aczel unclear
    ?
    unclear

    Relation between the paper passage and the cited Recognition theorem.

    We retrieve the peak saturation ratio achieved in each expansion from the TDLAS measurements in combination with adjusted thermocouple temperature readout... observe the onset of homogeneous nucleation of water vapor occurring at a threshold saturation ratio near S=5, in agreement with prior literature and classical nucleation theory.

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

73 extracted references · 73 canonical work pages

  1. [1]

    1996 , publisher=

    A Short Course in Cloud Physics , author=. 1996 , publisher=

  2. [2]

    2016 , publisher=

    Atmospheric Chemistry and Physics: From Air Pollution to Climate Change , author=. 2016 , publisher=

  3. [3]

    Chang and J

    K. Chang and J. Bench and M. Brege and W. Cantrell and K. Chandrakar and D. Ciochetto and C. Mazzoleni and L. R. Mazzoleni and D. Niedermeier and R. A. Shaw. A Laboratory Facility to Study Gas–Aerosol–Cloud Interactions in a Turbulent Environment: The Π Chamber. Bulletin of the American Meteorological Society. 2016. doi:10.1175/BAMS-D-15-00203.1

  4. [4]

    Physical Chemistry Chemical Physics , volume=

    Cloud condensation nucleation activities of calcium carbonate and its atmospheric ageing products , author=. Physical Chemistry Chemical Physics , volume=. 2015 , publisher=

  5. [5]

    Petters, M. D. and Kreidenweis, S. M. , TITLE =. Atmospheric Chemistry and Physics , VOLUME =. 2007 , NUMBER =

  6. [6]

    Dusek and G

    U. Dusek and G. P. Frank and L. Hildebrandt and J. Curtius and J. Schneider and S. Walter and D. Chand and F. Drewnick and S. Hings and D. Jung and S. Borrmann and M. O. Andreae , title =. Science , volume =

  7. [7]

    Aerosol--cloud--precipitation interactions. Part 1. The nature and sources of cloud-active aerosols , author=. Earth-Science Reviews , volume=. 2008 , publisher=

  8. [8]

    Transactions of the Faraday Society , volume=

    The nucleus in and the growth of hygroscopic droplets , author=. Transactions of the Faraday Society , volume=. 1936 , publisher=

  9. [9]

    2016 , pages=

    Atmospheric chemistry and physics: from air pollution to climate change , author=. 2016 , pages=

  10. [10]

    Thomson, William , year=. 4. On the Equilibrium of Vapour at a Curved Surface of Liquid , volume=. doi:10.1017/S0370164600041729 , journal=

  11. [11]

    Atmospheric Environment , volume=

    Spatial variation of aerosol number concentration in Helsinki city , author=. Atmospheric Environment , volume=

  12. [12]

    Fast and slow microphysics regimes in a minimalist model of cloudy Rayleigh-B

    Shaw, Raymond A and Thomas, Subin and Prabhakaran, Prasanth and Cantrell, Will and Ovchinnikov, Mikhail and Yang, Fan , journal=. Fast and slow microphysics regimes in a minimalist model of cloudy Rayleigh-B

  13. [13]

    Cloud--aerosol--turbulence interactions: Science priorities and concepts for a large-scale laboratory facility, B. Am. Meteorol. Soc., 101, E1026--E1035 , author=

  14. [14]

    J.\ Chem.\ Phys

    Homogeneous nucleation rate measurements for water over a wide range of temperature and nucleation rate , author=. J.\ Chem.\ Phys. , volume=

  15. [15]

    , year =

    In progress , author =. , year =

  16. [16]

    The novel aerosol chamber facility

    Bunz, H and M. The novel aerosol chamber facility. Proc. 7th European Symposium on the Physico-Chemical Behaviour of Atmospheric Pollutants , volume=

  17. [17]

    Annu.\ Rev.\ Fluid Mech

    Particle-turbulence interactions in atmospheric clouds , author=. Annu.\ Rev.\ Fluid Mech. , volume=

  18. [18]

    Comptes Rendus

    Charles Graziani and Mathieu Nespoulous and Renaud Denoyel and Stephan Fauve and Christian Chauveau and Luc Deike and Micka\"el Antoni , title =. Comptes Rendus. M\'ecanique , pages =

  19. [19]

    Heterogeneous reactivity of

    Huynh, Han N and McNeill, V Faye , journal=. Heterogeneous reactivity of

  20. [20]

    Atmos.\ Chem.\ Phys

    Effect of chemical mixing state on the hygroscopicity and cloud nucleation properties of calcium mineral dust particles , author=. Atmos.\ Chem.\ Phys. , volume=

  21. [21]

    Atmos.\ Meas.\ Tech

    Buchholz, Bernhard and Afchine, Armin and Klein, Alexander and Schiller, Cornelius and Kr. Atmos.\ Meas.\ Tech. , volume=

  22. [22]

    Exp.\ Fluids , volume=

    Comparison between shadow imaging and in-line holography for measuring droplet size distributions , author=. Exp.\ Fluids , volume=

  23. [23]

    Rapid, optical measurement of the atmospheric pressure on a fast research aircraft using open-path

    Buchholz, B and Afchine, A and Ebert, V , journal=. Rapid, optical measurement of the atmospheric pressure on a fast research aircraft using open-path

  24. [24]

    Rev.\ Sci.\ Instrum

    Droplet heterogeneous nucleation in a rapid expansion aerosol chamber , author=. Rev.\ Sci.\ Instrum. , volume=. 2025 , pages=

  25. [25]

    Wilson, C. T. R. , title =. Philos.\ Trans.\ R. Soc. A , volume =. 1897 , pages =

  26. [26]

    On the condensation nuclei produced in gases by the action of

    Wilson, Charles Thomson Rees , journal =. On the condensation nuclei produced in gases by the action of

  27. [27]

    Proc.\ R.\ Soc.\ Lond.\ A , volume=

    Condensation phenomena at different temperatures , author=. Proc.\ R.\ Soc.\ Lond.\ A , volume=

  28. [28]

    Volmer, Max and Flood, H. Tr. Z.\ Phys.\ Chem. , volume=

  29. [29]

    Naturwissenschaften , volume=

    Sander, Adolf and Damk. Naturwissenschaften , volume=

  30. [30]

    and Kassner, James L

    Allard, Edward F. and Kassner, James L. , title =. J.\ Phys.\ Chem. , volume =. 1965 , pages =

  31. [31]

    and Wagner, P.E

    Strey, R. and Wagner, P.E. , title =. J.\ Aerosol Sci. , volume =. 1981 , pages =

  32. [32]

    The problem of measuring homogeneous nucleation rates and the molecular contents of nuclei:

    Strey, R and Wagner, PE and Viisanen, Y , journal=. The problem of measuring homogeneous nucleation rates and the molecular contents of nuclei:

  33. [33]

    and Zahniser, Mark and Shorter, Joanne and Nelson, David and McManus, Barry , title =

    Paci, Paolo and Zvinevich, Yury and Tanimura, Shinobu and Wyslouzil, Barbara E. and Zahniser, Mark and Shorter, Joanne and Nelson, David and McManus, Barry , title =. J.\ Phys.\ Chem. , volume =. 2004 , pages =

  34. [34]

    The HITRAN2020 molecular spectroscopic database. J. Quant. Spectrosc. Radiat. Transfer , year =. doi:10.1016/j.jqsrt.2021.107949 , adsurl =

  35. [35]

    J.\ Chem.\ Phys

    Homogeneous nucleation rate measurements in supersaturated water vapor , volume =. J.\ Chem.\ Phys. , author =. 2008 , pages =. doi:10.1063/1.3000629 , number =

  36. [36]

    J.\ Chem.\ Phys

    Overview:. J.\ Chem.\ Phys. , author =

  37. [37]

    Adv.\ Phys

    Homogeneous nucleation and growth of droplets in vapours , author=. Adv.\ Phys. , volume=

  38. [38]

    and Jin, Y

    Peng, D. and Jin, Y. and Fan, X. D. and Yang, J. M. and Zhai, C. , title =. Rev.\ Sci.\ Instrum. , volume =. 2019 , pages =

  39. [39]

    and Menhart, S

    Dobrozemsky, R. and Menhart, S. and Buchtela, K. , title =. J.\ Vac.\ Sci.\ Technol.\ A , volume =. 2007 , pages =

  40. [40]

    Vacuum , volume =

    Sefa, Makfir and Šetina, Janez and Erjavec, Bojan , title =. Vacuum , volume =. 2013 , pages =

  41. [41]

    Vacuum , volume =

    Dobrozemsky, R , title =. Vacuum , volume =. 1995 , pages =

  42. [42]

    and Strey, R

    Viisanen, Y. and Strey, R. and Reiss, H. , title =. J.\ Chem.\ Phys. , volume =. 1993 , pages =

  43. [43]

    and Thomas, Subin and Prabhakaran, Prasanth and Shaw, Raymond A

    Anderson, Jesse C. and Thomas, Subin and Prabhakaran, Prasanth and Shaw, Raymond A. and Cantrell, Will , title =. Atmos.\ Meas.\ Tech. , volume =. 2021 , pages =

  44. [44]

    Fahey, D. W. and Gao, R.-S. and Möhler, O. and Saathoff, H. and Schiller, C. and Ebert, V. and Krämer, M. and Peter, T. and Amarouche, N. and Avallone, L. M. and Bauer, R. and Bozóki, Z. and Christensen, L. E. and Davis, S. M. and Durry, G. and Dyroff, C. and Herman, R. L. and Hunsmann, S. and Khaykin, S. M. and Mackrodt, P. and Meyer, J. and Smith, J. B....

  45. [45]

    Ebert, Volker and Teichert, Holger and Giesemann, Carsten and Saathoff, Harald and Schurath, Ulrich , title =. Tech. Mess. , volume =. 2005 , pages =

  46. [46]

    Nucleation and Atmospheric Aerosols: 17th International Conference , year =

    Manka, Alexandra and Bergmann, Dirk and Ghosh, David and Strey, Reinhard and Wölk, Judith , title =. Nucleation and Atmospheric Aerosols: 17th International Conference , year =

  47. [47]

    , title =

    Schmitt, John L. , title =. Rev.\ Sci.\ Instrum. , volume =. 1981 , pages =

  48. [48]

    and Reed, R

    Latham, J. and Reed, R. L. , doi =. Q.\ J.\ R.\ Meteorol.\ Soc. , number =

  49. [49]

    Baker, M. B. and Corbin, R. G. and Latham, J. , doi =. Q.\ J.\ R.\ Meteorol.\ Soc. , number =

  50. [50]

    Beals, M. A. and Fugal, J. P. and Shaw, R. A. and Lu, J. and Spuler, S. M. and Stith, J. L. , journal =

  51. [51]

    J.\ Atmos.\ Sci

    Hoffmann, Fabian and Feingold, Graham , doi =. J.\ Atmos.\ Sci. , number =

  52. [52]

    and Baker, Marcia B

    Bacon, Neil J. and Baker, Marcia B. and Swanson, Brian D. , title =. Quarterly Journal of the Royal Meteorological Society , volume =. doi:https://doi.org/10.1256/qj.02.04 , url =. https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1256/qj.02.04 , year =

  53. [53]

    Proc.\ Natl.\ Acad.\ Sci.\ U.\ S.\ A

    Cloud microphysical response to entrainment and mixing is locally inhomogeneous and globally homogeneous: Evidence from the lab , author=. Proc.\ Natl.\ Acad.\ Sci.\ U.\ S.\ A. , volume=

  54. [54]

    and Döring, W

    Becker, R. and Döring, W. , title =. Ann.\ Phys. , volume =. 1935 , pages =

  55. [55]

    and Wyslouzil, Barbara E

    Wölk, Judith and Strey, Reinhard and Heath, Christopher H. and Wyslouzil, Barbara E. , title =. J.\ Chem.\ Phys. , volume =. 2002 , pages =

  56. [56]

    , title =

    Pathak, Harshad and Mullick, Kelley and Tanimura, Shinobu and Wyslouzil, Barbara E. , title =. Aerosol Sci.\ Technol. , volume =. 2013 , pages =

  57. [57]

    , title =

    Hill, Philip G. , title =. J.\ Fluid Mech. , volume =. 1966 , pages =

  58. [58]

    Zhao, Bin and Donahue, Neil M. and Zhang, Kai and Mao, Lizhuo and Shrivastava, Manish and Ma, Po-Lun and Shen, Jiewen and Wang, Shuxiao and Sun, Jian and Gordon, Hamish and Tang, Shuaiqi and Fast, Jerome and Wang, Mingyi and Gao, Yang and Yan, Chao and Singh, Balwinder and Li, Zeqi and Huang, Lyuyin and Lou, Sijia and Lin, Guangxing and Wang, Hailong and ...

  59. [59]

    Lee, Shan‐Hu and Gordon, Hamish and Yu, Huan and Lehtipalo, Katrianne and Haley, Ryan and Li, Yixin and Zhang, Renyi , title =. J. Geophys. Res. Atmospheres , volume =. 2019 , pages =

  60. [60]

    Atmos.\ Res

    Fladerer, Alexander and Strey, Reinhard , title =. Atmos.\ Res. , volume =. 2003 , pages =

  61. [61]

    Science , volume=

    Can we understand clouds without turbulence? , author=. Science , volume=

  62. [62]

    Proc.\ Natl.\ Acad.\ Sci.\ U.\ S.\ A

    The role of turbulent fluctuations in aerosol activation and cloud formation , author=. Proc.\ Natl.\ Acad.\ Sci.\ U.\ S.\ A. , volume=

  63. [63]

    Experimental investigation of homogeneous freezing of sulphuric acid particles in the aerosol chamber

    M. Experimental investigation of homogeneous freezing of sulphuric acid particles in the aerosol chamber. Atmos.\ Chem.\ Phys. , volume=

  64. [64]

    J.\ Meteorol.\ Soc.\ Jpn

    A novel adiabatic-expansion-type cloud simulation chamber , author=. J.\ Meteorol.\ Soc.\ Jpn. , volume=

  65. [65]

    Atmos.\ Chem.\ Phys

    Cloud chamber experiments on the origin of ice crystal complexity in cirrus clouds , author=. Atmos.\ Chem.\ Phys. , volume=

  66. [66]

    Atmos.\ Meas.\ Tech

    Design of a new multi-phase experimental simulation chamber for atmospheric photosmog, aerosol and cloud chemistry research , author=. Atmos.\ Meas.\ Tech. , volume=

  67. [67]

    Newville, Matthew and Otten, Renee and Nelson, Andrew and Stensitzki, Till and Ingargiola, Antonino and Allan, Daniel and Fox, Austin and Carter, Faustin and Rawlik, Michal , year =

  68. [68]

    J.\ Atmos.\ Sci

    The effect of turbulence, gravity, and non-continuum hydrodynamic interactions on the drop size distribution in clouds , author=. J.\ Atmos.\ Sci. , year=

  69. [69]

    Physical Review Fluids , volume=

    Fine structure of the vapor field in evaporating dense sprays , author=. Physical Review Fluids , volume=. 2017 , publisher=

  70. [70]

    Phys.\ Rev.\ Fluids , volume=

    Diffuselet method for three-dimensional turbulent mixing of a cloudy air filament , author=. Phys.\ Rev.\ Fluids , volume=. 2025 , publisher=

  71. [71]

    Homogeneous and inhomogeneous mixing in cumulus clouds:

    Lehmann, Katrin and Siebert, Holger and Shaw, Raymond A , journal=. Homogeneous and inhomogeneous mixing in cumulus clouds:

  72. [72]

    doi:10.1016/j.softx.2025.102056 , journal =

    Nakai, Dai and Tanaka, Yohsuke , month = feb, year =. doi:10.1016/j.softx.2025.102056 , journal =

  73. [73]

    Phys.\ Rev.\ A , author =

    Spectroscopic line parameters of water vapor for rotation-vibration transitions near 7180 cm ^. Phys.\ Rev.\ A , author =. doi:10.1103/PhysRevA.79.052507 , pages =