🤖 AI Summary
This study addresses the limitations of traditional nowcasting approaches that rely on two-dimensional radar data and fail to capture the distinct motion dynamics of precipitation systems across different atmospheric layers. The authors propose a physics-informed convolutional neural network that, for the first time, enables end-to-end estimation of horizontal motion fields at individual altitude levels directly from three-dimensional radar reflectivity volume scans. Experiments using data from the Slovak radar network demonstrate that while the model successfully learns stratified motion features, it does not yield systematic improvements in forecast skill—largely because motion across layers is highly correlated in most precipitation events. Marginal gains in detection rates at longer lead times are offset by non-physical artifacts and positive bias, highlighting both the potential and the challenges of explicit three-dimensional motion modeling in precipitation nowcasting.
📝 Abstract
In precipitation nowcasting, most extrapolation-based methods rely on two-dimensional radar composites to estimate the horizontal motion of precipitation systems. However, in some cases, precipitation systems can exhibit varying motion at different heights. We propose a physics-informed convolutional neural network that estimates independent horizontal motion fields for multiple altitude layers directly from volumetric radar reflectivity data and investigate the practical benefits of altitude-wise motion field estimation for precipitation nowcasting. The model is trained end-to-end on volumetric observations from the Slovak radar network and its extrapolation nowcasting performance is evaluated. We compare the proposed model against an architecturally identical baseline operating on vertically pooled two-dimensional radar composites. Our results show that, although the model successfully learns altitude-wise motion fields, the estimated displacement is highly correlated across vertical levels for the vast majority of precipitation events. Consequently, the volumetric approach does not yield systematic improvements in nowcasting accuracy. While categorical metrics indicate increased precipitation detection at longer lead times, this gain is largely attributable to non-physical artifacts and is accompanied by a growing positive bias. A comprehensive inter-altitude motion field correlation analysis further confirms that events exhibiting meaningful vertical variability in horizontal motion are rare in the studied region. We conclude that, for the Slovak radar dataset, the additional complexity of three-dimensional motion field estimation is not justified by questionable gains in predictive skill. Nonetheless, the proposed framework remains applicable in climates where precipitation systems exhibit stronger vertical variability in horizontal motion.