A Topological Framework for Atmospheric River Interaction Using Framed Braids
Ioannis Diamantis
TL;DR
ARs are analyzed with a topological framework that treats multiple filaments as interacting strands whose time-ordered crossings are captured by oriented braids and whose internal moisture evolution is encoded by integer framings. By extracting braid words from ERA5 AR track data in sliding windows and attaching framing via a moisture integral around cross-sections, the authors generate framed braid representations that couple geometry and transport strength. Case studies in the North Pacific demonstrate that braid-based indicators reveal structural reorganizations and moisture intensification not evident from centroid geometry or IVT alone, offering a potential topological early-warning perspective. The work discusses limitations and outlines future directions including braidoids for birth/dissipation, pseudo crossings for uncertainty, and integration with forecasting workflows.
Abstract
Atmospheric Rivers (ARs) are filamentary moisture pathways responsible for a large fraction of extreme precipitation and often occur as interacting filament bundles within the same synoptic regime. Existing diagnostics typically analyze ARs in isolation, despite the frequent coexistence and interaction of multiple filaments. We introduce a topological framework for AR analysis based on framed braids and framed braidoids, which encodes both the geometric interaction of AR centroids and the internal evolution of moisture transport. In this approach, AR filaments are represented as strands whose time-ordered crossings form braid words, while moisture-based framing captures internal intensification or weakening along each filament. Applying this framework to reanalysis-derived Atmospheric River track data, we construct braid and framed braid representations over sliding time windows and analyze a strongly interacting multi-filament AR episode in the North Pacific. The results show that braid-based indicators capture structural reorganizations and moisture intensification episodes that are not apparent from centroid geometry or IVT magnitude alone, offering a complementary structural perspective on atmospheric moisture transport.
