the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
HiMIC-Daily: A high-resolution (daily and 1 km) multi-indicator atmospheric moisture collection over China, 2003–2020
Abstract. Near-surface atmospheric moisture is a fundamental component of the hydrological cycle and plays a key role in regulating land-atmosphere exchanges and surface energy partitioning. Reliable daily high-resolution moisture data are essential for regional climate analysis and fine-scale applications, particularly for capturing short-term variability and extreme moisture dynamics. With complex terrain and a dense population, China is highly vulnerable to extreme hydro-meteorological extremes, yet existing moisture products over China are largely constrained by coarse temporal resolution, insufficient spatial detail, and limited indicators. Here, we present HiMIC-Daily, a seamless daily 1-km-resolution near-surface atmospheric moisture dataset for China, 2003–2020. HiMIC-Daily provides a comprehensive suite of six widely used indicators that characterize atmospheric moisture from different perspectives: actual vapor pressure (AVP), dew point temperature (DPT), mixing ratio (MR), relative humidity (RH), specific humidity (SH), and vapor pressure deficit (VPD). This dataset is generated using the Light Gradient Boosting Machine (LightGBM) framework, which integrates in-situ observations from 2419 meteorological stations with multiple environmental and temporal covariates, including ERA5-Land derived near-surface temperature and DPT, AVP, land surface temperature, topography, and day of year. Validation against observations shows that HiMIC-Daily achieves robust performance across all six indicators, with R2 values ranging from 0.877 to 0.989. The strongest performance is obtained for AVP, DPT, MR, and SH, with R2 values exceeding 0.985, and error metrics remain within acceptable ranges for all indicators (e.g., mean absolute error of 0.677 hPa and a root mean square error of 0.933 hPa for AVP). Compared with two existing coarse resolution products, HiMIC-Daily provides finer spatial detail, higher accuracy, and more realistic temporal variability across different climatic regions. These capabilities support spatially explicit studies of climate variability and environmental processes. The HiMIC-Daily dataset is publicly available at https://doi.org/10.11888/Atmos.tpdc.303449.
- Preprint
(8833 KB) - Metadata XML
- BibTeX
- EndNote
Status: final response (author comments only)
- RC1: 'Comment on essd-2026-367', Anonymous Referee #1, 24 Jul 2026
-
RC2: 'Comment on essd-2026-367', Anonymous Referee #2, 06 Aug 2026
The authors of the manuscript titled “HiMIC-Daily: A high-resolution (daily and 1 km) multi-indicator atmospheric moisture collection over China, 2003–2020” present a machine learning approach which utilises the LightGBM model to develop a 1 km daily moisture dataset for China for the years spanning 2003-2020, using meteorological stations, reanalysis data, remote sensing and population density. Additionally, the dataset presented here is useful for the community and fits well with the journal’s scope. I have however a few concerns/comments before publishing the paper:
- The “Data and Methods” section needs to be expanded to include all the methodological details of the data pipeline. The authors state that “all gridded datasets are unified at a 1 km spatial resolution and consistent coordinate reference system” and later that “They are then harmonized to a consistent spatial extend, coordinate reference system (WGS84), and spatial resolution (1 km) using mosaicking, reprojection, resampling, clipping, and aggregation”. More details for each of the presented datasets is needed in the methods section and which method was applied to each. In addition to this, in lines 292-293, which hyperparameters of the LightGBM model were tuned in the grid search procedure and was the grid search exhaustive or random sampling?
- The split into training and validation sets was implemented by following a random 80/20 split of the pooled data from all the stations. While this is also informative, it’s not adequate in this context as there is significant validation leakage risk that can artificially inflate the performance metrics. Nearby days from the same station or data from nearby stations for the same day can likely appear in both sets. A temporal (split by months or even years) and spatial (leave a set of stations out) cross-validation should be added to the evaluation procedures.
- The authors made the choice to train a separate model for each year to account for possible year-to-year variations in the relationships between atmosphere moisture and its predictors. This has the potential to introduce artificial year-to-year discontinuities and complicate trend analysis. Have the authors made any comparison with a single model for all the years and this approach to validate this? The possibility of month-to-month variation in this relationship to be larger than year-to-year also exists (due to seasonal variations), so another option would be to train 12 individual models for each month or 4 seasonal ones (pool the data from all the years for all Januaries for example).
- Line 303: The Mean Error should also be include in the evaluation metrics to assess for systematic bias.
- Figure 5: The colormap used makes comparisons very difficult. Consider changing (e.g. viridis or magma).
- The ERA5-Land dataset in coastal areas has a lot of missing data over land (when interpolating to a 1x1 km grid). How did the authors treat this? Please clarify whether any coastal stations were excluded or interpolated and if prediction accuracy was checked separately for coastal vs inland stations.
- ERA5-Land-derived indicators dominate feature importance for all six target variables. This raises the question of whether HiMIC-Daily performs genuine sub-grid downscaling or is primarily a bias-corrected sharpening of the ERA5-Land field, with other covariates adding only secondary local adjustments. I suggest for a sample of ERA5-Land grid cells across contrasting terrain, compute the variance of the corresponding 1 km HiMIC-Daily predictions within each cell. Low within-cell variance relative to between-cell variance would indicate the product largely reproduces the coarse ERA5-Land field.
Additionally, while the manuscript is well written and has a good structure and flow there are some minor mistakes that need to be fixed:
- Line 21: Extreme is repeated
- Line 481: fine-scale informations (should be information)
- Table 4 could not be located in the manuscript as provided (mentioned twice in text).
Citation: https://doi.org/10.5194/essd-2026-367-RC2
Data sets
HiMIC-Daily: A high-resolution (daily and 1 km) multi-indicator atmospheric moisture collection over China, 2003–2020 Z. Su et al. https://doi.org/10.11888/Atmos.tpdc.303449
Viewed
| HTML | XML | Total | BibTeX | EndNote | |
|---|---|---|---|---|---|
| 143 | 47 | 12 | 202 | 7 | 12 |
- HTML: 143
- PDF: 47
- XML: 12
- Total: 202
- BibTeX: 7
- EndNote: 12
Viewed (geographical distribution)
| Country | # | Views | % |
|---|
| Total: | 0 |
| HTML: | 0 |
| PDF: | 0 |
| XML: | 0 |
- 1
This manuscript presents a daily 1km dataset of six near-surface atmospheric moisture indicators over China for 2003-2020 by integrating a variety of data sources, such as meteorological stations, remote sensing, climate reanalysis, and population data. The topic is highly relevant to the journal, and the data itself will benefit broad research applications. The manuscript is clearly organized and well written. I have some comments/suggestions for improving the quality of this work.
Major comments.
Model validation data. The authors split daily samples randomly into 80% training and 20% validation subsets. Because daily observations from the same station, nearby stations, and adjacent dates are strongly autocorrelated, a sample-level random split is likely to place observations from the same stations and closely related dates in both subsets. Consequently, the reported R2, MAE, and RMSE values may characterize interpolation among familiar stations and dates rather than performance at other unseen locations. Have the authors tried adding station-held-out or spatially blocked validation, in which all dates from a few selected stations are excluded from training? Additionally, the authors should explain how errors and systematic biases in LST, ERA5 and other inputs may influence the model.
Baseline comparison. I suggest the authors do some baseline comparison against the input datasets. For example, compare native ERA5-Land values with ground stations; native ERA5 with resampled ERA5 values; resampled ERA5 with ground stations. These will help examine whether the main feature-importance results that show ERA-derived moisture variables are the dominant predictors are partly biased by the close mathematical and statistical relationships between these highly correlated variables.
More details are needed regarding harmonization of heterogeneous input datasets for reproducibility. For example, what are the exact spatial resampling methods for each variable; how hourly data were converted to daily values; how missing MODIS observations were handled; how station and grid-cell elevation differences were treated.
Minor comments.
The authors should report quantitative comparisons in the text. The authors state in several places that “closest agreement”, “larger deviations”, etc. The exact values (especially for MAE and RMSE) and significance tests are needed when comparing different products.
The manuscript should describe HiMIC-Daily more explicitly as a machine learning downscaling/bias-correction product, to avoid claiming that 1-km information is independently observed.
The full dataset is not shared on Zenodo. Now it only includes some sample data.
L21: remove “extreme”. It is repetitive with “extremes”
L39-40: claims of higher accuracy and more realistic temporal variability should be supported by quantitative comparisons.
L64: “has” to “have”
L111: “of assessing” to “for assessing”
L180: “daily estimates” to “estimates”
Table 2 and L232: version of MODIS doesn’t seem consistent.
Table 4: is cited several times in the text but absent.
Figure 5 caption: “Deeper red indicates larger values, reflecting better model performance” is true only for R2. Larger MAE and RMSE indicate worse performance.