2026· IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing· Vol 19, pp. 23246-23263· 0 citations· 71 references
TL;DR
It is suggested that the proposed hybrid dynamic-statistical reconstruction framework named interior+surface quasi-geostrophic (isQG)-empowered ResNet is a feasible and stable framework for subsurface reconstruction and is, thus, helpful for analyzing the three-dimensional structures of mesoscale phenomena.
Abstract
High-precision reconstruction of subsurface ocean temperatures is of great significance for the identification and monitoring of mesoscale phenomena and the prediction of climate change trends. Although advanced artificial intelligent (AI) algorithms have been widely applied to reconstruct subsurface thermohaline fields from surface inputs, most of them cannot be trained on in situ data because of the sparsity and discontinuity of Argo profiles. Considering Argo profiles as labels, only one-dimensional AI algorithms are applicable thus far, and they cannot fully capture the spatiotemporal evolutionary characteristics of the ocean. As a basic property of mesoscale to larger-scale oceans, quasi-geostrophic (QG) dynamics can help estimate the interior parameters of the ocean. Combining QG with AI algorithms is promising for improving the performance of subsurface reconstruction, which has not been fully exploited by current studies. In this study, a hybrid dynamic-statistical reconstruction framework named interior+surface quasi-geostrophic (isQG)-empowered ResNet is proposed, which is based on the one-dimensional residual network (1D-ResNet) and incorporates the density anomalies reconstructed by the isQG method. The results demonstrate the following. First, the model performance is better than that of the conventional 1D-ResNet model, with the layer-averaged root mean square error being reduced by approximately 0.18 $^{\circ }$C. Shapley additive explanations analysis verifies the important contribution of isQG factors. Second, the predicted temperature profiles are in good agreement with the Argo in situ profiles, reasonably reflecting the vertical temperature variations in actual marine conditions. Third, the reconstructed 3-D temperature field can reasonably represent mesoscale phenomena (e.g., mesoscale eddies) and is in line with the GLORYS12V1 reanalysis data. It is suggested that the proposed method is a feasible and stable framework for subsurface reconstruction and is, thus, helpful for analyzing the three-dimensional structures of mesoscale phenomena.
Despite significant advances in observational systems such as the global Argo array of autonomous profiling floats, the spatiotemporal coverage of subsurface ocean observations remains limited compared to the dense data provided by satellite platforms. This study develops a data‐driven framework to reconstruct synthetic profiles of upper ocean temperature and salinity by training a self‐attention‐based neural network with satellite‐derived sea surface height (SSH) and sea surface temperature anomalies, using 17 years of collocated Argo float measurements. Daily synthetic profiles for the upper 650 m of the Philippine Sea were generated for the entirety of 2010 and assimilated into a regional ocean model via 4D‐Var data assimilation. Results show overall improved effectiveness of state estimation when synthetic profiles are utilized. Diagnostic variables like temperature, salinity, SSH, horizontal velocity all show improvement. Synthetic profiles of subsurface temperature had an overall positive impact on SSH analysis and forecast, especially in regions east of the Luzon Strait and the southern domain influenced by the North Equatorial Current. In the vertical range of 150–600 m, the impact of synthetic profiles on various observations was promising, leading to substantial reductions in the analysis and forecast error.
Guangpeng Liu, B. Powell· Journal of Advances in Model...· 0 citations
The first oceanic 4D sparse observation reconstruction dataset, named OceanVerse, is presented, providing a novel large-scale dataset that meets the MNAR (Missing Not at Random) condition, supporting more effective model comparison, generalization evaluation and potential advancement of scientific reconstruction architectures.
Bin Lu, Jingjing Shen, Ze Zhao et al.· Proceedings of the 32nd ACM...· 0 citations
Abstract. Land surface temperature (LST) obtained from satellite observations is a key parameter for understanding Earth surface-atmosphere energy exchange and urban thermal environments. However, the use of existing satellite-derived LST datasets for urban applications is limited by the coarse spatial resolution and the mixed-pixel problem. By integrating both two-dimensional (2D) surface properties and three-dimensional (3D) urban morphological characteristics, this study proposes a machine learning-based framework for high-resolution downscaling of satellite-based urban land surface temperature (SULST). A Random Forest model was developed to generate a 1-m downscaled SULST (DSULST) map. The model demonstrates strong performance, with a Pearson correlation coefficient of 0.89, RMSE of 1.15 K, NRMSE of 0.095, MAE of 0.56 K, and an index of agreement of 0.95. The 1-m DSULST maps reveal substantial sub-pixel thermal heterogeneity that is not captured by conventional 30-m LST data. Fine-scale spatial patterns associated with vegetation, building structures, and roads are clearly resolved in the downscaled 1-m temperature maps. These results highlight a critical limitation of satellite-derived LST in representing intra-urban thermal variability. The findings demonstrate that enhancing the spatial resolution of urban LST is essential for urban applications, including modeling surface energy fluxes, pedestrian-level heat exposure, and energy consumption, all of which benefit from higher spatial resolution.
N. Mijani, J. Voogt, Mohammad Karimi Firozjaei et al.· The International Archives o...· 0 citations
OceanDepths is introduced, the first open, global, regridded AI-ready dataset that pairs satellite-derived sea surface temperature, sea surface salinity, and sea surface height products with co-located EN4 subsurface temperature and salinity profiles, complemented by matched GLORYS12 ocean reanalysis data to support comparisons or multi-stage learning.
Simon Donike, Ruben Cartuyvels, A. I. Ferola et al.· 0 citations
Despite millions of ship soundings, bathymetry from satellite derived gravity is still necessary to fill in approximately three quarters of the global oceans. The methods used to carry out this inference have not changed significantly since the 1990s; however new methodology involving Machine Learning (ML) improves the bathymetric predictions considerably. Here we utilize five independent ML models from a workshop at the Technical University of Denmark (DTU). We highlight the benefits achieved by either (a) inclusion of a new highly‐accurate gravity field from the Surface Water and Ocean Topography (SWOT) satellite (∼22% improvement in spatial resolution), or (b) highly flexible ML methods capable of inferring bathymetric regimes not previously possible. By taking advantage of these five independent models we can determine regions of high confidence in our bathymetric inversion as well as regions with challenging conditions. Building on model prediction confidence and features revealed from the dense gravity field obtained by SWOT, we present a global features‐of‐interest map that, if mapped by ship soundings, would yield the largest improvement of the global bathymetry. These features are primarily located in regions with sparse multibeam coverage and associated with large gravity anomalies in the marine gravity field, indicating a potential presence of complex seafloor topography.
B. Nilsson, B. Phrampus, F. Salajegheh et al.· Journal of Geophysical Resea...· 1 citation
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