the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
High-resolution spatiotemporal fields of Southern Ocean interior carbonate system parameters integrated from float- and ship-based observations
Abstract. The Southern Ocean plays a crucial role in regulating atmospheric carbon dioxide (CO2) concentrations and modulating the global oceanic carbon cycle, thereby substantially mitigating the effects of anthropogenic climate change. However, due to the region’s challenging environment and sparse observational coverage, large uncertainties remain regarding the magnitude and mechanisms of carbon uptake in the Southern Ocean. In recent decades, the deployment of Argo float arrays has facilitated autonomous and continuous profiling of hydrographic and biogeochemical properties from the surface to depths of up to 6,000 m, complementing traditional ship-based observations. Nevertheless, high-resolution, integrated datasets that combine ship-based and Argo-derived observations remain rare, partly due to the challenges of data harmonization, quality control, and uncertainty estimation, as well as the indirect nature of carbonate system parameter retrievals from Argo measurements. Here, we present a comprehensive, quality-controlled reconstruction of key carbonate system parameters in the Southern Ocean interior—including total alkalinity (TA), dissolved inorganic carbon (DIC), pH (total scale), nitrate (NO3), phosphate (PO4), silicate (SiO4), anthropogenic carbon (Cant), and aragonite saturation (Ωar)—by leveraging machine learning techniques and integrating all available Argo float profiles with ship-based survey data. The resulting datasets are gridded at 1°×1° horizontal resolution and 84 vertical pressure levels (0–5,600 dbar), and are provided as distinct climatological products: the Float Grid (using all Argo float profiles) and the All-Data Grid (integrating all available Argo and ship-based observations). The Float Grid is further separated into the Non-O2-Float Grid (limited to Core Argo floats) and O2-Float Grid (limited to oxygen-measured Biogeochemical Argo floats). Each gridded product is accompanied by uncertainty estimates. The climatological products covers nearly the whole Sothern Ocean based on direct measurements instead of applying interpolating mapping methods, thereby providing a more robust result. Model performance is assessed through cross-comparison of Argo and shipboard measurements. The gridded products, collectively termed SOCOML (Southern Ocean CO2 Machine Learning products), are freely available for downloaded (doi: 10.17632/xzr59ngmpz.1) and are expected to support future studies of Southern Ocean carbon cycle.
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Status: final response (author comments only)
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RC1: 'Comment on essd-2025-473', Anonymous Referee #1, 21 Sep 2025
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AC1: 'Reply on RC1', Wanqin Zhong, 27 Oct 2025
The comment was uploaded in the form of a supplement: https://essd.copernicus.org/preprints/essd-2025-473/essd-2025-473-AC1-supplement.zip
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AC1: 'Reply on RC1', Wanqin Zhong, 27 Oct 2025
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RC2: 'Comment on essd-2025-473', Anonymous Referee #2, 29 Sep 2025
Zhong et al. developed a new ocean carbonate data product for the Southern Ocean by integrating float- and ship-based observations. Hydrographic data from Argo floats were used to approximate carbonate variables using established algorithms, which were then merged with ship-based measurements. As the Southern Ocean remains one of the least sampled regions for carbonate system variables, this product represents an important step toward filling that gap. It is a valuable contribution, and the paper is well written.
1. Title and Abstract
The title and abstract are misleading in their current form. The float data include temperature, salinity, and in some cases oxygen, which are then used to reconstruct ocean carbon variables. As written, readers could be misled to believe that the float data directly provide ocean carbonate variables, which is not accurate. Please revise the wording to more clearly reflect the indirect nature of the reconstruction.2. Gridding method
The authors mentioned that "Profile data for each parameter are sorted into spatial bins of 1° latitude × 1° longitude bins and 84 vertical pressure levels to generate homogenized three-dimensional gridded products." As we all know, there aren't enough data at each of the grid points for the global ocean. Did the authors use some kind of gridding method? More details are needed.3. Spatial Grid Convention
It is more standard to use the grid ordering of longitude, latitude, and depth, rather than the current latitude, longitude, and depth. Adopting the conventional structure will facilitate easier integration with other datasets.4. Vertical Resolution
(a) Use depth in meters rather than pressure in dbars, in line with most other ocean carbon data products.
(b) Adopt standardized depth levels consistent with the World Ocean Atlas (WOA). For reference, the current recommended levels can be either 33 (not presented here) or 102 (as below):
0, 5, 10, 15, 20, 25, 30, 35, 40, 45, 50, 55, 60, 65, 70, 75, 80, 85, 90, 95, 100, 125, 150, 175, 200, 225, 250, 275, 300, 325, 350, 375, 400, 425, 450, 475, 500, 550, 600, 650, 700, 750, 800, 850, 900, 950, 1000, 1050, 1100, 1150, 1200, 1250, 1300, 1350, 1400, 1450, 1500, 1550, 1600, 1650, 1700, 1750, 1800, 1850, 1900, 1950, 2000, 2100, 2200, 2300, 2400, 2500, 2600, 2700, 2800, 2900, 3000, 3100, 3200, 3300, 3400, 3500, 3600, 3700, 3800, 3900, 4000, 4100, 4200, 4300, 4400, 4500, 4600, 4700, 4800, 4900, 5000, 5100, 5200, 5300, 5400, 5500 m.5. Product Variants
Presenting multiple output variants may confuse end-users. I recommend presenting the final merged grid product as the primary output, supplemented by quality flags that indicate the provenance of each grid point (e.g., derived from non-O2 floats, O2 floats, shipboard observations, etc.). This approach maintains transparency while simplifying use.6. Uncertainty Estimates
The reported uncertainties appear unrealistically low. This is concerning, as the ESPER algorithm alone typically introduces uncertainties on the order of ~20 µmol/kg for DIC and TA, not including additional uncertainties from spatial gridding. Please revisit your uncertainty estimation procedure.7. Data Publication and Metadata
The product is currently published on Mendeley, but with very limited metadata. For long-term archiving, discoverability, and broader community uptake, I strongly encourage the authors to submit the dataset to NOAA’s Ocean Carbon and Acidification Data System (OCADS) at NCEI. This would ensure proper long-term archiving, rich metadata documentation, and alignment with established practices in the ocean carbon community. Most importantly, it will make this data product available along with similar ocean carbonate data products.8. Output Variables
At present, the output only includes TA, DIC, pH, anthropogenic carbon, and aragonite saturation state. I recommend also reporting additional ocean carbonate system variables, such as the fugacity of carbon dioxide, carbonate ion concentration, calcite saturation state, and the Revelle Factor. These are commonly provided in comparable products and would broaden the product’s utility.Minor Comments
Throughout the manuscript, please use the term “variables” instead of “parameters”, to describe an observed property.
Citation: https://doi.org/10.5194/essd-2025-473-RC2 -
AC2: 'Reply on RC2', Wanqin Zhong, 27 Oct 2025
The comment was uploaded in the form of a supplement: https://essd.copernicus.org/preprints/essd-2025-473/essd-2025-473-AC2-supplement.zip
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AC2: 'Reply on RC2', Wanqin Zhong, 27 Oct 2025
Data sets
Southern Ocean CO2 Machine Learning products (SOCOML) Wanqin Zhong, Xin Ma, Yingxu Wu, Chenglong Li, Tianqi Shi, Wei Gong, and Di Qi https://doi.org/10.17632/xzr59ngmpz.1
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Review of the Manuscript Number: essd-2025-473: Title: High-resolution spatiotemporal fields of Southern Ocean interior carbonate system parameters integrated from float- and ship-based observations by Wanqin Zhong et al.
See attached document.