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Saturday, October 16, 2010

Russian Firestorm: Finding a Fire Cloud from Space

Russian Firestorm: Finding a Fire Cloud from Space

by Holli Riebeek, EO, August 31, 2010

Thick, choking smoke hung over Russia on August 1, 2010, adding to the misery of a stifling summer heat wave. Thousands of people were fleeing nearly 700 fires burning in the drought-dried forests and peat bogs of western Russia, while those not directly threatened were struggling to see through and breathe the smoky air.
Photograph of smokey air filling Red Square, Summer 2010.
Thick smoke filled Moscow’s Red Square during the summer of 2010. (Photograph © 2010 Evgeniya Zubchenko.)
It was perhaps not too surprising, then, when the Ozone Monitoring Instrument (OMI) on NASA’s Aura satellite recorded high concentrations of aerosols over far northern Russia on August 1. Smoke from forest fires contains tiny particles (aerosols) produced when a fire incompletely burns through trees and other carbon-based fuel. These aerosols usually linger in the lower part of the atmosphere before falling out. On this day, OMI measured aerosols above the top of high clouds.
The Ozone Monitoring Instrument detected particles (aerosols) high in the atmosphere over northern Russia on August 1, 2010. (NASA image by Jesse Allen using OMI data.)
A decade ago, a scientist trying to trace the source of those aerosols would have looked for an erupting volcano. A volcanic eruption, it was thought, was the only force powerful enough to loft aerosols twelve kilometers or more into the atmosphere.
But in 2010, meteorologist Michael Fromm saw another suspect far closer to northern Russia. Working at the Naval Research Laboratory in Washington, D.C., Fromm had spent the last decade studying how fires inject smoke into the upper atmosphere. His experience told him that at least one of the hundreds of fires burning in western Russia had probably generated a powerful, dangerous firestorm.
Satellite image of fires and smoke in western Russia, July 30, 2010.
The high-altitude particles in OMI data could have been smoke from fires in Western Russia. The fires are outlined in red in this photo-like satellite image from July 30, 2010. Clouds indicate that air was rising and conditions were right for a firestorm to form. (NASA image by Jesse Allen using MODIS data.)
Large fires can create their own weather by rapidly heating the air above them. The heated air rises with smoke until water vapor in the air condenses into a puffy cloud. An odd-looking puff of white capping a dark column of smoke is the sign of a fire-formed, or pyrocumulus cloud.
Occasionally, if the superheated air rises fast and high enough, it forms a towering thundercloud. Like the thunderstorms that form on a hot summer’s day, the tops of these cauliflower-shaped clouds reach high enough into the atmosphere that ice crystals form. Those ice crystals electrify the cloud, creating lightning. Called pyrocumulonimbus clouds,the clouds are capable of dangerous lightning, hail, and strong winds. One such firestorm in 2003 pelted Canberra, Australia, with large, soot-darkened hail, produced a damaging tornado, and generated strong winds that caused the fire to explode into neighborhoods in the capital city.
Pyrocumulonimbus cloud above Canberra, Australia.
A pyrocumulonimbus cloud towers over thick smoke from fires burning near Canberra, Australia on January 18, 2003. The umbrella-shaped cloud brought strong winds that helped the fires explode into the city. (Photograph copyright New South Wales Rural Fire Service.)
As dangerous and destructive as pyrocumulonimbus-driven storms can be, the giant clouds also act like a chimney, sucking smoke high into the atmosphere. After the Canberra fires, the Total Ozone Mapping Spectrometer (OMI’s predecessor) detected extremely high levels of aerosols in the atmosphere. NASA’s Stratospheric Aerosol and Gas Experiment (SAGE III ) satellite confirmed that the smoke from Canberra’s firestorm had reached the stratosphere.
Was OMI’s observation this summer an indicator that a similar firestorm had erupted in Russia? Fromm suspected that it was, and he set out to find proof of a pyrocumulonimbus cloud in other satellite data.

Evidence of a Firestorm

Fromm started with true-color images from the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Terra and Aqua satellites. At about 7:00 UTC, a few hours before OMI made its observation, an odd circular cloud complex was visible above a field of smoke in the Terra MODIS image. The cloud was faintly tinted brown, and its circular shape was different from the long lines of clouds beneath it. Temperature measurements from MODIS also revealed that the cloud was much cooler than the surrounding clouds, indicating that it was a high-altitude ice cloud.
Satellite image of pyrocumulonimbus clouds over Arctic Russia.
A circular cloud structure is the remnant of a pyrocumulonimbus cloud or firestorm that had drifted over northern Russia from fires in western Russia. MODIS on NASA’s Aqua satellite acquired this image on August 1, 2010. (NASA images by Jesse Allen and Robert Simmon based on MODIS data.)
To confirm the cloud’s height, Fromm got a tip from David Nelson, a scientist from the Jet Propulsion Laboratory working with the Multi-angle Imaging Spectroradiometer (MISR), which also flies on Terra. MISR carries nine cameras that simultaneously acquire images of the Earth from nine different angles. By merging images from each angle, scientists like Nelson can get a multidimensional view of clouds and Earth’s surface. On August 1, Nelson’s multidimensional view revealed that the cloud over the Russian fires was shaped like an umbrella with a bulging top and lower edges. The top of the cloud reached 12 kilometers.
Map of cloud heights of pyrocumulonimbus cloud over Arctic Russia.
The Multi-angle Imaging Spectroradiometer confirms that the umbrella-shaped cloud reached 12 kilometers above the Earth’s surface into the lower stratosphere on August 1, 2010. (NASA image by Jesse Allen and Robert Simmon based on MISR data.)
The final piece of evidence connecting the cloud to the unusual aerosols came from NASA’s Cloud-Aerosol Lidar and Infrared Pathfinder Satellite(CALIPSO). By sending a pulse of light into the atmosphere and measuring the light that comes back, CALIPSO provides a profile of what types of particles are in the atmosphere and at what altitude. Clouds return a different type of signal than aerosols because cloud particles have a different shape and size. Particles that are high up also return a signal more quickly than those closer to the ground, information that CALIPSO turns into particle altitude.
Fortunately, CALIPSO passed over part of the suspicious cloud on August 1. The sensor recorded the high, dome-shaped cloud at 12 kilometers. It also confirmed that the cloud contained more than water and ice. Smoke aerosols formed a cap over the cloud, and the air around the cloud was contaminated with smoke. The cloud, CALIPSO confirmed, was a pyrocumulonimbus.
Transect of pyrocumulonimbus cloud showing profile and entrained aerosols.
A profile of the atmosphere from the CALIPSO satellite reveals smoke above and around the top of the suspected pyrocumulonimbus cloud. (NASA image by Jesse Allen using CALIPSO andMODIS data.)
Four satellite sensors together confirmed that a pyrocumulonimbus cloud had formed and drifted over northern Russia, but where had the dangerous storm originated? By tracing the air back in time in a weather model, Fromm discovered that the air over northern Russia had traveled from western Russia. The cloud and smoke that the satellites observed had been situated over the fires in western Russia on July 30, when the fires had grown explosively. The satellites provided evidence that a firestorm helped fuel the fires’ growth.
Map of aerosol backtraces.
A model containing weather data helped confirm that the pyrocumulonimbus cloud and smoke had been over fires in western Russia on July 30. The model connects the satellite observations of smoke in northern Russia to the fires in western Russia. (NASA map by Robert Simmon using NOAA’s HYSPLIT and Natural Earth.)
While pyrocumulonimbus clouds are probably not unusual, only about ten have been identified in scientific literature. As this series of images documents, pyrocumulonimbus clouds pump soot from fires high into the atmosphere. Once in the stratosphere, above the part of the atmosphere where weather occurs, aerosols can travel long distances. In this recent case, the smoke from Russian fires reached the Eastern United States. The smoke stays in the stratosphere for a long time because it is above the part of the atmosphere where weather occurs, so it doesn’t rain or fall out as easily.
The smoke aerosols are also important because of their potential influence on climate. Dark aerosols in the stratosphere absorb and reflect energy from the Sun, warming the stratosphere (which may impact our weather), while cooling the lower atmosphere. This means fires might have a slight cooling influence on the climate, similar to volcanoes. But unlike volcanoes, pyrocumulonimbus pollution of the stratosphere is not yet accounted for in climate models. Just how frequently pyrocumulonimbus clouds form and how much they contribute to aerosols in the stratosphere are questions that will require more observations to answer.
“Satellites are the key to unlocking those mysteries,” says Fromm, “and there is a multi-decade treasure of data yet to explore.”

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