Impact of the coagulation of dust particles on Mars during the 2018 global dust storm

TL;DR

This study uses a 3D climate model to analyze how dust particle coagulation during the 2018 Martian global dust storm affects particle sizes and climate, revealing significant impacts on atmospheric temperature and storm decay.

Contribution

It introduces a new parameterization for dust coagulation in a 3D climate model, accounting for Brownian motion, diffusion, and gravitational effects during a Martian dust storm.

Findings

Coagulation rates increase tenfold during the storm.

Particle sizes can double due to coagulation, cooling the atmosphere.

Improved storm decay simulation aligns better with observations.

Abstract

Coagulation of particles occurs when two particles collide and stick together. In the Martian atmosphere, dust coagulation would increase the effective particle size, as small particles accrete to larger particles. Murphy et al. (1990) showed that Brownian coagulation of dust in the Martian atmosphere was not significant, due to the low dust particle mixing ratios, while Montmessin et al. (2002) and Fedorova et al. (2014) showed that it mostly involves particle radii smaller than 0.1 um. However, the effects of coagulation have never been explored in 3D, during a global dust storm, i.e. in presence of larger numbers of small particles. Here we revisit this issue by using the NASA Ames Mars Global Climate Model (MGCM) to investigate the temporal and spatial changes in dust particle sizes during the 2018 global storm due to coagulation and the overall impact of these processes on Mars' climate. Our parameterization for coagulation includes the effect of Brownian motion, Brownian diffusion enhancement, and gravitational collection. We show that Brownian motion and Brownian diffusion enhancement dominate gravitational collection. The impact of coagulation is significant during the storm, with coagulation rates increased by a factor of 10 compared to non-storm conditions. The effective particle radius can be increased by a factor of 2 due to coagulation, leading to a 20K colder atmosphere above 30 km altitude. Overall, our parameterization improves the representation of the decay phase of the storm relative to observations. The process remains significant outside the storm period if large numbers of submicron-sized particles are involved. It may be possible, in GCMs, to lift larger amounts of submicron-sized particles from the surface without excess dust buildup in the atmosphere, thus improving the agreement with some of the observations without diverging from the observed column opacities.