Articles | Volume 14, issue 1
https://doi.org/10.5194/essd-14-33-2022
© Author(s) 2022. This work is distributed under the Creative Commons Attribution 4.0 License.
EUREC4A's Maria S. Merian ship-based cloud and micro rain radar observations of clouds and precipitation
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- Final revised paper (published on 10 Jan 2022)
- Preprint (discussion started on 10 Aug 2021)
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
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RC1: 'Comment on essd-2021-265', Martin Hagen, 07 Sep 2021
- AC1: 'Reply on RC1', Claudia Acquistapace, 19 Nov 2021
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RC2: 'Comment on essd-2021-265', Anonymous Referee #2, 08 Oct 2021
- AC3: 'Reply on RC2', Claudia Acquistapace, 19 Nov 2021
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RC3: 'Comment on essd-2021-265', Anonymous Referee #3, 10 Oct 2021
- AC4: 'Reply on RC3', Claudia Acquistapace, 19 Nov 2021
- AC2: 'Comment on essd-2021-265', Claudia Acquistapace, 19 Nov 2021
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Claudia Acquistapace on behalf of the Authors (19 Nov 2021)
Author's response
Author's tracked changes
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ED: Publish as is (22 Nov 2021) by Silke Gross
AR by Claudia Acquistapace on behalf of the Authors (26 Nov 2021)
The manuscript describes the set-up, attitude control, and exemplary measurements of two vertical pointing radars onboard RV MS Merian during Eurec4a. Main focus of this data paper is the compensation of the ship motion in situations where the active stabilization platform was properly working and different treatment of data in situations where the platform got stuck in arbitrary orientations.
The manuscript is consistent and well written and certainly deserves publication as data paper. There are only minor modifications required. I like the lessons learned section, I hope that this will be considered in future campaigns.
Some general comments:
Obviously, the authors did develop the methods behind the ship motion correction by themselves, without borrowing from the airborne radar community (e.g. Bange, J. et al., 2013: Measurement of aircraft state and thermodynamic and yynamic variable, in: Airborne Measurements for Environmental Research: Methods and Instruments, edited by: Wendisch, M. and Brenguier, J-L., https://doi.org/10.1002/9783527653218.ch2). The methods are the same and there is an agreement between the two worlds (air - sea).
For the W-band radar you do not mention anything about attenuation (gaseous, liquid) which certainly has to be considered, you call it just reflectivity (factor). Whereas for the MRR you talk about attenuated equivalent reflectivity (factor). This should be consistent. Otherwise one might assume that data from W-band radar are corrected for gaseous and liquid attenuation as well as for Mie effects. Reflectivity factor z implies Rayleigh approximation. However, since both systems are mm-wave systems you better write about effective reflectivity factor. This implies that Mie scattering effects have to be considered in the interpretation of reflectivity factor.
I think the labels/numbers in the figures are too small, but I leave this to the technical editor.
Minor specific comments and hints in the order of appearance in the text:
Line 14: I think DOI's have to be given in the abstract, but this is a task for the technical editor
Line 22: What does OA stand for?
Line 69: Section instead of Session
Line 78: can you give here some numbers about the temporal drift
Line 127: Why longitude and latitude with the same temporal resolution as the radar data are not copied to the radar dataset?
Lines 170 - 175: can you also give the temporal resolution of the MRU?
Lines 179 - 184: this should go to section 2.3
Figure 5 is hardly readable, the sketch of MS Merian is 2D, whereas the vectors are 3D; this figure should be improved considerable
Lines 206 + 207: “whereas w_heave … gates” is repeated from above
Lines 224 - 230: confusing, ex,ey,ez is first ship relative and later horizon relative, maybe you could use different notations for the two reference systems
Line 226: appendix C or equation C4
Figure 6: faint lines are hard to read, you could also use dashed lines instead
Line 239: horizontal or ship relative coordination system? These are different reference systems
Line 262: v_trans would be more memorable for the translation velocity than v_trasl
Line 264? - rotation vector: what is about bending and twisting of the ship body (I remember a video you showed once at a workshop)
Figure 7: maybe panels a), b), c), e), f), g) could be larger, and d) and h) could be smaller (or omitted)
Line 296: Figure 7 e)-g)
Line 298: the high fall velocities in the second half of the plot and persistent through all heights seem unrealistic, can you comment on this?
Line 311: signal to noise "ratio"
Line 313: Table 2 gives 7.5 to 34 m resolution. For the horizontal resolution also beamwidth has to be considered
Line 321: numbering Fig. A1 is confusing. The figure does not belong to Appendix A
Figure 9 caption: interpretation “and made a hook rain structure … wind mixing” should not go to caption
Figure 12: I think, images from both radars should have the identical height axis range and identical color bar range and color map. This makes comparisons between W- and K-band much easier, even though it is not the objective of the paper.
Line 399: It might be worth to discuss shortly the observed differences between both radars and how the complement each another. Different attenuation due to different wavelengths, different sensitivity, …
Line 434: just a comment: some airborne systems (unfortunately not HALO/HAMP) have an IRS/IMU as close as possible to the radar antenna
Line 507: … by alpha clockwise from North
Line 507: for non-meteorologists you could add "(the direction where the wind is coming from)” this makes it easier to understand the minus signs in Eq. B1
Line 514: If “yaw” psi is indeed …
Line 523: heave is not discussed here
Line 531 till end of page: check order of description of r_rot and v_rot, looks like repeating of definitions
Line 544, Eq. D1: should be e_p0 = … (?)
Line 547, Eq. D2: why not t_final for theta_tbl,S