Cloud-top infrared observations reveal the four-dimensional precipitation structure
Authors: Tianchi Xu, Ziqiang Ma, Andrea Marinoni, Yuanpeng He, Xiaoqing Li, Chuanfeng Zhao, Kang He, Jintao Xu, +6 more
Organizations: Institute of Remote Sensing and Geographical Information Systems, School of Earth and Space Sciences, Peking University, Beijing, 100871, China · Department of Computer Science and Technology, University of Cambridge, Cambridge, United Kingdom · Key Laboratory of High Confidence Software Technologies (Peking University), Ministry of Education; School of Computer Science, Peking University, Beijing, 100871, China · Innovation Center for Fengyun Meteorological Satellite, National Meteorological Centre, China Meteorological Administration, Beijing, 100081, China · Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, 100871, China · Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu, 610213, China · School of Civil Engineering and Environmental Science, University of Oklahoma, Norman, OK, United States
Accurate four-dimensional (4D) precipitation information is essential for understanding the Earth's energy and water cycles, yet remains observationally unresolved at global scales. Conventional theory holds that geostationary infrared observations primarily sense cloud-top properties, with limited sensitivity to sub-cloud precipitation. Here we show that cloud-top infrared measurements nevertheless encode sufficient information to recover the four-dimensional structure of precipitation, revealing a previously unexploited observability of sub-cloud processes. We introduce a physically constrained deep learning framework, 4DPrecipNet, in which a moisture-first constraint requires the latent representation to recover precipitable water vapour, anchoring the model in thermodynamic consistency. By integrating multi-channel infrared radiances with these constraints and radar-derived precipitation profiles, we reconstruct the vertical and temporal evolution of precipitation systems from geostationary orbit. The framework captures deep convective structures and their evolution, with robust performance across large samples and independent radar comparisons. These results demonstrate that sub-cloud precipitation is physically encoded in cloud-top infrared observations, establishing a new pathway for continuous global monitoring of precipitation structure.