Dune initiation in a bimodal wind regime

TL;DR

This study validates linear stability theory as a quantitative tool for predicting the initiation and development of dunes under bimodal wind regimes through field measurements and modeling at Great Sand Dunes.

Contribution

It extends linear stability theory application to bimodal wind conditions and provides empirical validation with detailed field data.

Findings

Theoretical predictions match well with observed dune attributes.

Linear stability theory effectively predicts dune orientation, wavelength, and growth rate.

Bimodal wind regimes can be modeled to understand dune initiation and evolution.

Abstract

Early-stage bedforms develop into mature dunes through complex interactions between wind, sand transport and surface topography. Depending on varying environmental and wind conditions, the mechanism driving dune formation and, ultimately, the shape of nascent dunes may differ markedly. In cases where sand availability is plentiful one mechanism suggested for triggering dune growth is linear stability theory. Until now, this theory has only been tested using field evidence in unidirectional winds. However, in many areas of the world and on other planets where aeolian processes act, wind regimes are often bimodal or multimodal. Here, we investigate field evidence of protodune formation under bimodal winds by applying linear stability analysis to a developing protodune field. Employing recent theoretical and experimental research, combined with in-situ wind, sediment transport, and topographic measurements during a month long field campaign at Great Sand Dunes National Park, Colorado, USA, we use a development of the linear stability theory to predict the spatial characteristics (orientation and wavelength) and temporal evolution (growth rate and migration velocity) of a protodune field. We find that the theoretical predictions compare well with measured dunefield attributes as characterized by high-resolution Digital Elevation Models measured using repeat terres trial laser scanning. Our findings suggest that linear stability theory is a quantitative predictor of protodune development on sandy surfaces with a bimodal wind regime. Our findings are significant as they offer critical validation of the linear stability theory for explaining the initiation and development of dunes towards maturity in a complex natural environment.