The Role of Variability in Transport for Large-Scale Flow Dynamics

TL;DR

This paper introduces a framework to analyze how variability influences transport in large-scale flow dynamics, highlighting the importance of characteristic scales and resonance effects in flux variability and pseudo-lobe formation.

Contribution

It presents a novel combined graphical and analytical framework for understanding variability-driven transport in large-scale flows, emphasizing the role of characteristic scales and resonance.

Findings

Flux variability is governed by the interaction of flow and variability scales.

Pseudo-lobe sequences describe spatial and temporal transport coherence.

Resonance occurs when the ratio of characteristic scales equals one.

Abstract

We develop a framework to study the role of variability in transport across a streamline of a reference flow. Two complementary schemes are presented: a graphical approach for individual cases, and an analytical approach for general properties. The spatially nonlinear interaction of dynamic variability and the reference flow results in flux variability. The characteristic time-scale of the dynamic variability and the length-scale of the flux variability in a unit of flight-time govern the spatio-temporal interaction that leads to transport. The non-dimensional ratio of the two characteristic scales is shown to be a a critical parameter. The pseudo-lobe sequence along the reference streamline describes spatial coherency and temporal evolution of transport. For finite-time transport from an initial time up to the present, the characteristic length-scale of the flux variability regulates the width of the pseudo-lobes. The phase speed of pseudo-lobe propagation averages the reference flow and the flux variability. In contrast, for definite transport over a fixed time interval and spatial segment, the characteristic time-scale of the dynamic variability regulates the width of the pseudo-lobes. Generation of the pseudo-lobe sequence appears to be synchronous with the dynamic variability, although it propagates with the reference flow. In either case, the critical characteristic ratio is found to be one, corresponding to a resonance of the flux variability with the reference flow. Using a kinematic model, we demonstrate the framework for two types of transport in a blocked flow of the mid-latitude atmosphere: across the meandering jet axis and between the jet and recirculating cell.