Articles | Volume 22, issue 10
https://doi.org/10.5194/cp-22-1927-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Interaction between the East Asian summer monsoon and Westerlies as shown by desert shrub-ring records from the Alxa Plateau, Northwest China
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- Final revised paper (published on 26 Oct 2026)
- Supplement to the final revised paper
- Preprint (discussion started on 27 Apr 2026)
- Supplement to the preprint
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-2026-2026', Anonymous Referee #1, 28 May 2026
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AC1: 'Reply on RC1', Yu Ren, 04 Jun 2026
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RC2: 'Reply on AC1', Anonymous Referee #1, 04 Jul 2026
- AC3: 'Reply on RC2', Yu Ren, 25 Aug 2026
- AC4: 'Reply on RC2', Yu Ren, 25 Aug 2026
- AC5: 'Reply on RC2', Yu Ren, 25 Aug 2026
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RC2: 'Reply on AC1', Anonymous Referee #1, 04 Jul 2026
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AC1: 'Reply on RC1', Yu Ren, 04 Jun 2026
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RC3: 'Comment on egusphere-2026-2026', Anonymous Referee #2, 02 Aug 2026
- AC2: 'Reply on RC3', Yu Ren, 06 Aug 2026
- AC6: 'Reply on RC3', Yu Ren, 25 Aug 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Submit a revised manuscript (02 Sep 2026) by Hans Linderholm
AR by Yu Ren on behalf of the Authors (02 Sep 2026)
Author's response
Author's tracked changes
Manuscript
ED: Publish subject to minor revisions (review by editor) (16 Sep 2026) by Hans Linderholm
AR by Yu Ren on behalf of the Authors (22 Sep 2026)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (24 Sep 2026) by Hans Linderholm
AR by Yu Ren on behalf of the Authors (24 Sep 2026)
This study collected shrub tree-ring samples from 26 sites in a region influenced by both the westerlies and East Asian summer monsoon (EASM). By establishing chronologies and analyzing the relationship with climatic factors, the study found that water is the primary limiting factor affecting shrub growth. It is found that shrub growth shows no clear relationship with the westerlies and EASM on an interannual scale, characterizing by a positive correlation with westerlies and a negative correlation with the EASM on a decadal scale. I recommend a revision.
Major comments:
Lines 263 and 274: Figure 5 and Table 1 show a strong correlation between the tree-ring chronology and the westerlies and EASM. However, this correlation is based on time-series data obtained from 11-year moving average. This may introduce spurious correlations, creating the illusion of strong correlation. As shown in Figure 4, the correlations are not strong at the interannual scale. And the differences in decadal trends, shown in Figure 5, are quite pronounced. These increase the likelihood of spurious correlation.
Line 402: The authors use the foehn effect to explain the negative impact of the EASM on tree growth. However, EASM has a dual role, bringing both moisture and the foehn effect. Analyzing the impact of EASM on drought in the study area would help strengthen the conclusions.
The authors aim to elucidate the interaction between the westerlies and EASM on the climate of the study area. But, shrub growth under different westerlies and the EASM (Figure 5) does not adequately answer the scientific questions. The authors have identified that shrub growth in this region is influenced by moisture conditions. So, I suggest establishing structural equation models (or other functions) comprising factors such as westerlies, EASM, climate factors and chronologies. By comparing the direct and indirect effects of the westerlies and EASM on shrub growth, you can demonstrate the direction and intensity of their effects.
Text and figures require correction. Such as the punctuation in Line 160, the font size in the figures and the order of sub-figures in Figure 7.