Estimation of vertical profiles of raindrop size distribution and cloud microphysical processes in stratiform rainfall using vertical-pointing X- and VHF-band radars

Goto, Yusuke; Shinoda, Taro; Minda, Haruya; Kyushima, Moeto; Hashiguchi, Hiroyuki; Toda, Nozomu; Shige, Shoichi

doi:10.5194/egusphere-2025-5944

Preprints

https://doi.org/10.5194/egusphere-2025-5944

Preprints

16 Dec 2025

| 16 Dec 2025

Estimation of vertical profiles of raindrop size distribution and cloud microphysical processes in stratiform rainfall using vertical-pointing X- and VHF-band radars

Yusuke Goto, Taro Shinoda, Haruya Minda, Moeto Kyushima, Hiroyuki Hashiguchi, Nozomu Toda, and Shoichi Shige

Abstract. Simultaneous vertical pointing observations by X- and VHF-band radars were conducted in Japan, and these data were used to estimate vertical profiles of drop size distribution (DSD) parameters of raindrops, assuming a gamma distribution, for a stratiform rainfall event. We used X-band reflectivity, vertical Doppler velocity, and spectral width, combined with VHF-band vertical air motion data. The estimation considers non-Rayleigh scattering and the influence of vertical air motion, and accounts for the contamination of spectral broadening using a forward convolution technique. We demonstrated that for stratiform rainfall, broadening by wind shear may be neglected, even with a relatively coarse radar range resolution of 150 metres. Cloud physical quantities (median volume diameter, liquid water content, normalised intercept parameter) retrieved from the estimated DSD parameters were compared with operational X-band polarimetric radar data and found to be highly accurate. We also point out the potential applicability of this method to satellite-borne radars. Among the estimated parameters, the shape and slope parameters generally increased with decreasing altitude. These changes are attributed to collision-coalescence and breakup based on variations in the cloud physical quantities, likely due to the humid environment. This study suggests that retrieving cloud physical quantities from DSD parameters estimated from vertical observations enables robust discussions on cloud physical processes.

Received: 05 Dec 2025 – Discussion started: 16 Dec 2025

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.

Download & links

Yusuke Goto, Taro Shinoda, Haruya Minda, Moeto Kyushima, Hiroyuki Hashiguchi, Nozomu Toda, and Shoichi Shige

Status: final response (author comments only)

RC1:
'Comment on egusphere-2025-5944', Anonymous Referee #1, 05 Jan 2026
General comments:
The authors proposed a method for estimating the vertical distributions of DSD parameters and cloud microphysics-related parameters for layered rainfall events using vertically pointing observations from X-band and VHF-band radars. Although the validation was limited to specific regions and cases, their analysis was conducted with great care and is considered highly valuable. However, whilst the technical steps undertaken are listed in the main text, the reasons for undertaking them and their advantages are generally absent, and the relationships between them remain unclear, rendering the text very difficult to read. Consequently, the novelty of this research is hard to discern. There must be pros and cons associated with each radar used; these should be explicitly stated whilst reviewing relevant prior research.

Furthermore, the advantages gained from combining these radars and how they differ from previous research should be clearly stated in the introduction. Relatedly, within the methodology section, it would be preferable to include a brief explanatory sentence at the beginning of each subsection to clarify the context within the text.

Specific comments:
L34-63: This section should outline what is known from ground-based drop-size distribution observations and their limitations, and subsequent sections should highlight the importance of the vertical distribution of cloud microphysical properties.

L66-67: Please briefly state why the Rayleigh approximation allows the average vertical flow to be negligible.

L-103: Having read this far, I could not discern why synchronised observations of X- and VHF-band radars are practical. As noted in the general comments, the introduction requires restructuring to state the pros/cons of X-band and VHF-band explicitly, and to clarify the advantages of combining them. Furthermore, mention should be made of why a stratiform rain event is the focus.

Section 4.1: Could you show the horizontal distribution of horizontally polarised reflectivity at the peak time for the case study? With only the vertical distribution, readers, including me, cannot fully grasp what kind of case study is being targeted.

L587-589: It is the distribution shape that approaches equilibrium, not the state. Therefore, it would be preferable to describe 'equilibrium shape'.

Figure 15: Why was the delta cut-off set between 2500 and 2750 m? Looking at Figs 11, 13 and 14, there appears to be no apparent kink in the vertical distributions. If there is some intention behind this, it should be explicitly stated.

Figure 16: Why was ERA5 data used instead of Japanese reanalysis data? Furthermore, has the accuracy been verified regardless of the reanalysis data used? For instance, near Shigaraki, I found an upper-air sounding site called Shionomisaki. I strongly recommend checking the scatter plot of relative humidity for the neighbouring grid of the reanalysis data at this site, which would enhance the reliability of this figure and strengthen the authors' arguments.

Technical Corrections:
L27, 371, 374, 376, 378, 385, 390, 394, 555, 578, Table 3, Figure 11, Figure 14: L_WC [gm^-3] should be LWC [g m^-3].

L29, 148: mm⁶m^-3 should be mm⁶ m^-3 (space required between units).

L34: N(D) should be defined; e.g., ... a gamma distribution to show DSD (N(D)), whichi is ...

L35: mm^-1-µm^-3 should be mm^-1-µ m^-3 (space required between units).

L42, 580, Table 3, Figure 11: mm^-1m^-3 should be mm^-1 m^-3 (space required between units)

L67, 132, 134, 149, 556, Table 2: m/s needs to be m s^-1.

L88: How large is it?

L92: ... of raindrops?

L175: Here, N(D) should explicitly state which function is assumed.

L185: kg/m³ should be kg m^-3.

L271: m²/s² needs to be m² s^-2.

L370, 371: °/km should be degree km^-1.

L411: UTC+9 should be UTC + 9 hours. which may apply the other place in the main text.

L519: dB/km should be dB km^-1.

Figure 9: 1/mm should be mm^-1

Figure 12: deg./km should be degree km^-1
Citation: https://doi.org/10.5194/egusphere-2025-5944-RC1
- AC1: 'Reply on RC1', Yusuke Goto, 20 Jan 2026
  
  We greatly appreciate the referee’s thorough and constructive comments. Please find our detailed responses and revision plan in the attached file.
  
  Citation: https://doi.org/10.5194/egusphere-2025-5944-AC1
RC2:
'Comment on egusphere-2025-5944', Anonymous Referee #2, 09 Jan 2026

This manuscript describes a method to estimate the gamma raindrop size distribution parameters using moments from a vertically pointing X-band radar and the air motion retrieved from a VHF wind profiler. Since the X-band radar did not record the Doppler velocity spectra, the DSD parameters were retrieved from measured moments of reflectivity, mean Doppler velocity, and spectrum width. The manuscript does a nice job of describing the spectrum broadening terms (i.e., due to horizontal wind, turbulence, and shear) that contribute to the measured spectrum width, provides an error analysis, and estimates the DSD uncertainties when not including those correction terms. After clarifying a couple minor items, I believe this manuscript would be ready for publication.
Specific Comments:
1. Equation (4). I do not think equations (4) and (8) are correct. From Fukao and Hamazu, the spectrum width is given by equation (5.102). The second term in equations (4) and (8) appear consistent with (5.102), but the first term is not consistent with equation (5.102). Also, to me, it does not look correct to have the mean air motion V_a(overbar) included in the spectrum width estimate. The spectrum width calculation is the width of the rain portion in the spectrum (see Fukao and Hamazu, Fig. 5.10). If V_a(overbar) is replaced with V_tz^nonRay(overbar) in equation (8), then would the spectrum width be just the first term in equation (8)? For equation (4), the text would need to define a similar variable called V_tz^Ray(overbar) for equation (4). Please examine equations (4) and (8) and make changes where needed.
2. Lines 246-247. As written, I thought the phrase 'liquid phase' is referring to the Rayleigh scattering peak observed by the MU radar, but it appears to refer to the height region containing rain drops (aka, liquid phase). Please clarify that the 'liquid phase' refers to a height region containing liquid phase hydrometeors and not to the hydrometeors themselves.
3. Line 370. Is a word missing? How about, '...found that the XRAIN K_DP is sensitive..."
4. Line 518. Attenuation in TAMX is discussed, but attenuation in NUX is not discussed. At these short ranges and larger particle regimes during stratiform rain, I do not believe that attenuation will impact the N0 estimate very much. But please confirm that assumption and please provide a sentence or two near equation (20) that discusses how attenuation in the measured NUX reflectivity is ignored or included in the estimate of N0.

Citation: https://doi.org/10.5194/egusphere-2025-5944-RC2
- AC2: 'Reply on RC2', Yusuke Goto, 20 Jan 2026
  
  We greatly appreciate the referee’s thorough and constructive comments. Please find our detailed responses and revision plan in the attached file.
  
  Citation: https://doi.org/10.5194/egusphere-2025-5944-AC2

Yusuke Goto, Taro Shinoda, Haruya Minda, Moeto Kyushima, Hiroyuki Hashiguchi, Nozomu Toda, and Shoichi Shige

Viewed

Total article views: 291 (including HTML, PDF, and XML)

HTML	PDF	XML	Total	BibTeX	EndNote
190	80	21	291	62	65

HTML: 190
PDF: 80
XML: 21
Total: 291
BibTeX: 62
EndNote: 65

Views and downloads (calculated since 16 Dec 2025)

Month	HTML	PDF	XML	Total
Dec 2025	82	40	12	134
Jan 2026	108	40	9	157

Cumulative views and downloads (calculated since 16 Dec 2025)

Month	HTML	PDF	XML	Total
Dec 2025	82	40	12	134
Jan 2026	108	40	9	157

Viewed (geographical distribution)

Total article views: 267 (including HTML, PDF, and XML) Thereof 267 with geography defined and 0 with unknown origin.

Country	#	Views	%

Latest update: 28 Jan 2026

Short summary

We combined radar data from two frequencies for a case of stratiform rainfall in Japan to estimate the relationship between raindrop size and number concentration aloft. One of the radars used operates at a frequency close to that of satellite-mounted precipitation radars. However, even for stratiform rainfall expected under calm atmospheric conditions, data corrections are required, suggesting that challenges remain for the application to satellite observations.


Total:	0
HTML:	0
PDF:	0
XML:	0