Some features of this site are not compatible with your browser. Install Opera Mini to
better experience this site.
At the Intersection of Clouds and Smoke
This page contains archived content and is no longer being updated. At the time of publication, it represented the best available science. However, more recent observations and studies may have rendered some content obsolete.
In late July 2013, numerous wildfires burned through boreal forests in northern Canada. On July 29 and 30, 2013, the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Aqua and Terra satellites acquired these images of a large smoke plume spreading south over Hudson Bay. The Canadian Interagency Forest Fire Center reported 21 uncontrolled fires burning in Manitoba and six burning in Nunavut on July 30.
The satellite images from MODIS and other sensors got the attention of a community of wildfire and remote sensing experts who monitor fires for signs of pyrcocumulus clouds, towering clouds that can send smoke as high as the stratosphere.
When Raymond Hoff saw the images, he saw no evidence of pyrocumulus clouds. But the atmospheric scientist from the University of Maryland at Baltimore County saw something peculiar: it looked like the smoke had cut a strip of fair weather through the otherwise cloudy scene. Images from MODIS, which only show the top of the smoke and clouds, are not enough to definitively confirm his suspicion, but the physics of the phenomenon are understood well enough to think it was a possibility.
For more than a decade, atmospheric scientists have noticed and reported examples of smoke and other pollution particles suppressing clouds. Andrew Ackerman, a scientist at NASA’s Goddard Institute for Space Studies, was among the scientists to describe the “cloud burning” effect of dark soot particles within haze over the northern Indian Ocean. In a study published in 2000, Ackerman and colleagues explained how particles known as black carbon, readily absorb sunlight, warming the layer of smoky air and reducing the relative humidity of smoke plumes. This causes existing clouds to break down more rapidly than they would otherwise. The particles also can interfere with the normal rising and cooling of moist air, one of the key processes that fuels cloud formation.
But is that what was happening over Hudson Bay in July 2013? After reviewing the MODIS imagery, as well as data collected by CALIPSO, Ackerman was not convinced. The CALIPSO data revealed that smoke was mingling with clouds to the south of the plume, but the layer of clouds to the north was significantly higher, suggesting the clear area may simply be a gap between the two cloud layers.
“Bottom line: It is possible that we’re simply looking at a coincidence,” explained Ackerman.