Tiny particles in Arctic ponds may play role in cloud formation, climate change

Tiny particles bubbling up from the tops of melting sea ice into the Arctic sky may be a key, understudied element of cloud formation in that climate-sensitive region.

Researchers from Colorado State University have published findings in Geophysical Research Letters that highlight how these airborne “ice-nucleating particles” from biological sources, such as bacteria, provide a platform for the creation of clouds. Because cloud cover plays an important role in the balance between incoming solar energy and outgoing heat, as well as precipitation, these particles may be key to developing a better understanding of climate change in the Arctic.

Ice-nucleating particles can come in the form of things like mineral dust, microbes or sea spray. As they make their way into the atmosphere, they act as templates for water vapor to freeze on to support cloud formation. The new paper highlights ponds of melted water that sit on top of sea ice as a key source of these particles.

The ponds are made of melted snow but can also include a mix of seawater that has seeped in as well as released soil sediment or melted ice from the pack of ice below that hosts small organisms. By taking sea-ice core samples and measuring aerosol emissions around these pools, the team was able to show that ice-nucleating particle concentrations were higher there than in seawater. That likely means there are specific biological processes at play in these pools, contributing to their formation.

Researchers in the Department of Atmospheric Science led the work with samples collected during the MOSAiC expedition – the Multidisciplinary Drifting Observatory for the Study of Arctic Climate. The expedition is a $150 million international effort to develop a better understanding of declines in Arctic sea ice and how they are linked to climate change. Germany’s Alfred Wegener Institute led the expedition, with key support from the Cooperative Institute for Research in Environmental Sciences – a partnership of the University of Colorado Boulder and the National Oceanic and Atmospheric Administration. In total, scientists and funding agencies from 20 nations were involved, including support from the National Science Foundation, Department of Energy, NOAA and NASA.

The 2019-2020 MOSAiC project offered an opportunity to gather data on these particles in a region that is already feeling the effects of climate change in the form of glacial melt, permafrost thaw and sea-ice decline. So far, only a few specific particles are known to be a part of this cloud formation process. And their path into the atmosphere has rarely been studied in the northernmost, extreme high Arctic, partially because it is difficult to gather samples in that challenging environment.

Camille Mavis, a CSU doctoral student, served as lead author on the paper. She said the Arctic environment lent itself to studying these particles because it is a somewhat simpler system with fewer animals and variables than others around the globe.

She said the Arctic is warming four times faster than the rest of the globe. That could mean more ponds may form in the future, or small changes in their composition could significantly alter the entire system.

“Clouds are complex, and there is still a lot of uncertainty associated with how aerosol interactions affect cloud radiative effects overall. Developing an understanding of the role these particles play will help with weather modeling and a host of other benefits in the future,” Mavis said. “Our current models don’t do a good job of mimicking these clouds right now, especially in polar regions.”