用卫星数据生成云层垂直结构,提升气象模型精度
CERBERUS: A Three-Headed Decoder for Vertical Cloud Profiles
- 三头解码器融合卫星、地面数据与时间信息,预测云反射率分布
- 在多个云层场景下恢复结构,对复杂云系给出可信不确定性估计
- 适合气候建模与遥感数据融合研究者参考
大气云具有复杂的三维结构和微物理特征,但全球尺度上主要依赖二维卫星观测,导致天气与气候模型中云过程的数据驱动学习与评估受限,加剧了大气物理的不确定性。本文提出CERBERUS,一种基于概率推断的框架,从地球静止卫星亮温、近地表气象变量及时间上下文出发,生成垂直雷达反射率剖面。该模型采用三头编码器-解码器架构,预测零膨胀(ZI)的垂直分辨反射率分布。在阿曼南方大平原站点的地面Ka波段雷达观测数据上训练与评估,CERBERUS能有效恢复不同云型下的相干结构,对保留测试时段具备泛化能力,并在多层及动态复杂云中提供反映物理不确定性的置信度估计。结果表明,基于分布的学习目标有助于弥合观测尺度差异,为气候模型生成具有物理意义的合成观测数据开辟新路径。
原文摘要 · Abstract (English)
Atmospheric clouds exhibit complex three-dimensional structure and microphysical details that are poorly constrained by the predominantly two-dimensional satellite observations available at global scales. This mismatch complicates data-driven learning and evaluation of cloud processes in weather and climate models, contributing to ongoing uncertainty in atmospheric physics. We introduce CERBERUS, a probabilistic inference framework for generating vertical radar reflectivity profiles from geostationary satellite brightness temperatures, near-surface meteorological variables, and temporal context. CERBERUS employs a three-headed encoder-decoder architecture to predict a zero-inflated (ZI) vertically-resolved distribution of radar reflectivity. Trained and evaluated using ground-based Ka-band radar observations at the ARM Southern Great Plains site, CERBERUS recovers coherent structures across cloud regimes, generalizes to withheld test periods, and provides uncertainty estimates that reflect physical ambiguity, particularly in multilayer and dynamically complex clouds. These results demonstrate the value of distribution-based learning targets for bridging observational scales, introducing a path toward model-relevant synthetic observations of clouds.
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