the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
A model framework on atmosphere-snow water vapor exchange and the associated isotope effects at Dome Argus, Antarctica: part I the diurnal changes
Tianming Ma
Zhuang Jiang
Minghu Ding
Yuansheng Li
Wenqian Zhang
Abstract. Ice-core water isotopes contain valuable information on past climate changes. However, such information can be altered by post-depositional processing after snow deposition. Atmosphere-snow water vapor exchange is one of such processes, but its influence remains poorly constrained. Here we constructed a box model to quantify the atmosphere-snow water vapor exchange fluxes and the associated isotope effects at sites with low snow accumulation rate where the effects of atmosphere-snow water vapor exchange are suspected to be large. The model reproduced the observed diurnal variations of δ18O, δD, and d-excess in water vapor at Dome C, East Antarctica. According to the same model framework, we found that under summer clear-sky conditions atmosphere-snow water vapor exchange at Dome A can cause diurnal variations in atmospheric water vapor δ18O and δD by 8.2±0.3 ‰ and 54.4±1.2 ‰, with corresponding diurnal variations in surface snow δ18O and δD by 0.11±0.01 ‰ and 0.62±0.01 ‰, respectively. The modeled results under summer cloudy conditions display similar patterns to those under clear-sky conditions but with smaller magnitudes of diurnal variations. After 24-hour simulation, snow water isotopes were enriched under both cloudy and clear-sky conditions. Under winter conditions at Dome A, the model indicates there are no diurnal cycles in atmospheric and surface snow water isotopes can be caused by atmosphere-snow vapor exchange, but the model predicts more or less depletions in snow δ18O and δD in the period of 24-hour simulation, opposite to the results under summer conditions. If the modeled snow isotope enrichments in summer and depletions in winter represent general situations at Dome C, this likely suggests the air-snow vapor exchange tends to enlarge snow water isotope seasonality, but the annual net effect would be small due to the offsetting of effects in summer and winter. This remains to be explored in the future.
- Preprint
(1852 KB) - Metadata XML
-
Supplement
(487 KB) - BibTeX
- EndNote
Tianming Ma et al.
Status: final response (author comments only)
-
RC1: 'Comment on tc-2023-76', Mathieu Casado, 07 Sep 2023
Review of « A model framework on atmosphere-snow water vapor exchange and the associated isotope effects at Dome Argus, Antarctica：part I the diurnal changes» by Ma and others.
This manuscript considers the exchange between water molecules between the firn and the atmosphere, and the impact it can induce on the change of isotopic composition in extremely low accumulation regions of Antarctica. Using the results from Dome C as an analogue for Dome A is a clever strategy that can yield promising results to how to explain the impact of surface processes on the future Dome A ice core. The study takes into account the variations of stability of the atmosphere with systematic calculations of the Richardson number and developed three case studies associated with two sets of summer conditions (clear sky and cloud), and one set of winter conditions.
While the authors used a rather classical set of equations to evaluate the isotopic exchanges during sublimation and condensation, it seems not pertinent here, as it ignores major contributors to the boundary layer processes and only consider the system as a closed box without exchange with the free atmosphere. As a result, the results do not match the observations that were made for the surface snow isotopic composition at Dome C, even though, it is supposed to be the case study used to parametrise the model.
I suggest profound modifications to the model, which take into account exchanges between the atmospheric boundary layer and the free atmosphere on top of the surface processes, and which would match the surface snow changes, at least in order of magnitude, before considering the manuscript for publication.
Major Comments:
- The box model developed by the authors was parametrised against vapour measurements obtained at Dome C, in order to compensate for lack of measurements at Dome A. The outputs of the model predict changes of vapour isotopic composition that seem realistic, but it is not the case for the changes of snow isotopic composition for which the variations are extremely small (less than 0.02‰) while the observed changes are around 2‰ during a typical night (Casado et al., 2018). The relative changes of snow and vapour isotopic compositions during a typical clear sky night were modelled in this manuscript, and suggested that a closed box model (which is de facto what the authors have implemented since no exchanges between the free atmosphere and the boundary layer are taken into account) is not realistic for this type of event.
- Another aspect that suggests that exchanges between the boundary layer and the free atmosphere must happen is the Richardson number. Indeed, for negative Richardson numbers, the atmosphere must be quite convective, which suggest that the boundary layer exchanges with both the surface snow and the free atmosphere.
- The atmosphere is qualified as stable for any positive Richardson number, yet, it seems that some studies suggest that some amount of mixing remains quite strong for 0 < Ri < 0.1 (Zilitinkevich et al., 2008) . This could be discussed.
- Some limited vapour data exist at Dome A (Liu et al., 2022). While these data might be difficult to compare to your results, in particular consider how high the d-excess is, which could be associated with calibration issues, it should be discussed.
Considering how fundamental these changes are, an updated version of the manuscript could have completely different conclusions.
Bibliography
Casado, M., Landais, A., Picard, G., Münch, T., Laepple, T., Stenni, B., Dreossi, G., Ekaykin, A., Arnaud, L., Genthon, C., Touzeau, A., Masson-Delmotte, V., & Jouzel, J. (2018). Archival processes of the water stable isotope signal in East Antarctic ice cores. The Cryosphere, 12(5), 1745–1766. https://doi.org/10.5194/tc-12-1745-2018
Liu, J., Du, Z., Zhang, D., & Wang, S. (2022). Diagnoses of Antarctic Inland Water Cycle Regime: Perspectives From Atmospheric Water Vapor Isotope Observations Along the Transect From Zhongshan Station to Dome A . In Frontiers in Earth Science (Vol. 10). https://www.frontiersin.org/articles/10.3389/feart.2022.823515
Zilitinkevich, S. S., Elperin, T., Kleeorin, N., Rogachevskii, I., Esau, I., Mauritsen, T., & Miles, M. W. (2008). Turbulence energetics in stably stratified geophysical flows: Strong and weak mixing regimes. Quarterly Journal of the Royal Meteorological Society, 134(633), 793–799. https://doi.org/10.1002/qj.264
Citation: https://doi.org/10.5194/tc-2023-76-RC1 -
RC2: 'Comment on tc-2023-76', Anonymous Referee #2, 08 Sep 2023
The comment was uploaded in the form of a supplement: https://tc.copernicus.org/preprints/tc-2023-76/tc-2023-76-RC2-supplement.pdf
Tianming Ma et al.
Tianming Ma et al.
Viewed
| HTML | XML | Total | Supplement | BibTeX | EndNote | |
|---|---|---|---|---|---|---|
| 168 | 69 | 14 | 251 | 27 | 8 | 8 |
- HTML: 168
- PDF: 69
- XML: 14
- Total: 251
- Supplement: 27
- BibTeX: 8
- EndNote: 8
Viewed (geographical distribution)
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1