Articles | Volume 17, issue 2
https://doi.org/10.5194/gmd-17-607-2024
© Author(s) 2024. This work is distributed under the Creative Commons Attribution 4.0 License.
A simple and realistic aerosol emission approach for use in the Thompson–Eidhammer microphysics scheme in the NOAA UFS Weather Model (version GSL global-24Feb2022)
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- Final revised paper (published on 25 Jan 2024)
- Preprint (discussion started on 17 Aug 2023)
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 egusphere-2023-1271', Anonymous Referee #1, 04 Oct 2023
- AC1: 'Reply on RC1', Haiqin Li, 05 Dec 2023
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RC2: 'Comment on egusphere-2023-1271', Anonymous Referee #2, 15 Nov 2023
- AC2: 'Reply on RC2', Haiqin Li, 05 Dec 2023
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Haiqin Li on behalf of the Authors (10 Dec 2023)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (20 Dec 2023) by David Topping
AR by Haiqin Li on behalf of the Authors (21 Dec 2023)
This paper introduces a change to allow the microphysics and radiation in the
UFS Weather Model to interact with cloud and ice nuclei from real-time emission
sources rather than the climatology currently used with the Thompson scheme.
The work represents a step forwards in allowing basic aerosol-physics interactions
without the use of a full chemistry model for medium-range global applications.
A series of cases are tested and compared with the climatology option and
verifying data from various sources. The results show that this is a promising
direction in reducing some biases and adding more realism to aerosol effects
globally.
The paper is well presented and worth publication. I only have some minor
comments to address.
Minor Points
1. line 105. State the units of WFA and IFA. Equations are hard to interpret
without units.
2. L114-116. 1^-9 is a typo.
3. L123. "is a scale-aware"
4. L127. "boulder"
5. L127. Does MYNN PBL mix WFA and IFA?
6. L131. "surface climatological(?) number concentration"
7. Figure 1. Vertically integrated?
8. L169. Is AOD interactive with radiation in the model?
9. L186-189. "aeras" typo.
10. L233. Not sure how to relate 10^9 profiles with 10^13 integrated values?
11. L246. Invigoration related to freezing level in cloud?
12. L251. Do non-hygroscopic aerosols include black carbon which interacts with
radiation but is not an ice nucleus?