arXiv:2509.04991physics.ao-phcs.AI2025-09

提出新型神经网络,提升中高分辨率地表温度反演精度与泛化能力。

A Mechanism-Coupled Split Window Network for Medium- to High-Resolution Land Surface Temperature Retrieval

  • 将红外双窗算法重构为物理分量系数动态学习问题
  • 可自适应计算不同地表与大气条件下的系数,提升复杂场景精度
  • 适合遥感、气候建模等需要高精度地表温度的应用

地表温度(LST)是陆面-大气相互作用、地表能量收支和气候过程中的基本物理变量。基于中高分辨率热红外(TIR)观测的LST能有效揭示不同地貌单元间的热环境差异。然而,在复杂大气条件和多样的地表覆盖类型下,实现准确、鲁棒且全球通用的LST反演仍具挑战。传统双窗(SW)算法严重依赖经验参数化,其固定系数难以适应高温地表或高水汽含量等复杂场景。同时,传统数据驱动模型因缺乏显式物理结构约束,对分布外(OOD)样本泛化能力有限。为此,本文提出并行分量解耦神经网络(PCD-Net)框架,将SW反演重构为物理分量系数的动态学习问题。以双窗方程为物理基础,构建并行子网络,自适应学习常数项、一阶和二阶亮温差项对应的系数;同时引入残差分支,补充表面发射率与大气水汽联合效应引起的非线性耦合修正。通过分量级解耦建模,PCD-Net 显式刻画了地表发射率、大气水汽含量与各双窗物理分量之间的动态响应关系。

原文摘要 · Abstract (English)

Land surface temperature (LST) is a fundamental physical variable in land-atmosphere interactions, surface energy budgets, and climate processes. LST derived from medium- to high-resolution thermal infrared (TIR) observations effectively reveals thermal environmental disparities across distinct landscape units. However, achieving accurate, robust, and globally generalizable LST retrieval remains challenging under complex atmospheric conditions and diverse land cover types. Traditional split window (SW) algorithms heavily rely on empirical parameterizations, whose fixed coefficients fail to adapt to complex scenarios such as high surface temperatures and high atmospheric water vapor content. Concurrently, conventional data-driven models exhibit limited generalizability to out-of-distribution (OOD) samples due to the absence of explicit physical structure constraints. To address these issues, this study proposes a Parallel Component Decoupled Neural Network (PCD-Net) framework, which reformulates SW retrieval as a dynamic learning problem of physical component coefficients. Using the SW equation as the physical backbone, the framework constructs parallel subnetworks to adaptively learn the dynamic coefficients corresponding to the constant, first-order, and second-order brightness temperature difference terms; meanwhile, a residual branch is incorporated to supplement the nonlinear coupling corrections induced by the joint effects of surface emissivity and atmospheric water vapor. Through this component-level decoupled modeling, PCD-Net explicitly characterizes the dynamic response relationships between land surface emissivity, atmospheric water vapor content, and different SW physical components.

地表温度遥感反演神经网络物理模型

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