# Buoyancy-Driven Entrainment in Dry Thermals

## TL;DR

This paper develops a buoyancy-driven model for dry thermal entrainment that does not rely on turbulence or self-similarity assumptions, and validates it through simulations showing buoyancy's key role.

## Contribution

The authors derive a simple, buoyancy-based model for thermal entrainment that aligns with numerical simulations, challenging turbulence-centric theories.

## Key findings

- Entrainment rate scales as psilon \u2264 B/w^2
- Buoyancy is essential for entrainment, confirmed by gravity-off simulations
- Model agrees quantitatively with direct numerical simulations

## Abstract

\citet{turner1957} proposed that dry thermals entrain because of buoyancy (via a constraint which requires an increase in the radius $a$). This however, runs counter to the scaling arguments commonly used to derive the entrainment rate, which rely on either the self-similarity of \citet{scorer1957} or the turbulent entrainment hypothesis of \citet{morton1956}. The assumption of turbulence-driven entrainment was investigated by \citet{lecoanet2018}, who found that the entrainment efficiency $e$ varies by less than $20\%$ between laminar (Re = 630) and turbulent (Re = 6300) thermals. This motivated us to utilize Turner's argument of buoyancy-controlled entrainment in addition to the thermal's vertical momentum equation to build a model for thermal dynamics which does not invoke turbulence or self-similarity. We derive simple expressions for the thermals' kinematic properties and their fractional entrainment rate $\epsilon$ and find close quantitative agreement with the values in direct numerical simulations. In particular, our expression for entrainment rate is consistent with the parameterization $\epsilon \sim B/w^2$, for Archimedean buoyancy $B$ and vertical velocity $w$. We also directly validate the role of buoyancy-driven entrainment by running simulations where gravity is turned off midway through a thermal's rise. The entrainment efficiency $e$ is observed to drop to less than 1/3 of its original value in both the laminar and turbulent cases when $g=0$, affirming the central role of buoyancy in entrainment in dry thermals.