Scripps researcher Kerri Pratt with "Shirley," an aerosol
time-of-flight mass spectrometer (ATOFMS) mounted into a C-130
aircraft operated by the National Center for Atmospheric Research.
Photo courtesy of Andrew J. Heymsfield, NCAR
Wild is the Wind
Aircraft-mounted instrument makes first-ever direct measurements of biological particles in ice clouds
A UC San Diego-led science team and a particle analyzer named
"Shirley" are behind the first detection ever of biological
particles -- pieces of bacteria, fungi, and plants --— in cold
ice clouds.
Atmospheric chemistry Professor Kim Prather, who holds a joint
appointment at Scripps Institution of Oceanography and the
Department of Chemistry and Biochemistry at UCSD, described the find
as a key step forward toward explaining how airborne particles, or
aerosols, affect cloud formation. That dynamic has been considered one of the top challenges of scientists who try to simulate future climate
through the use of computer models, she said.
"Understanding which particles form ice nuclei, which occur at
extremely low concentrations and are inherently difficult to
measure, means you can further understand processes that result in
precipitation," said Prather. "Any new piece of information you can
get is critical."
Prather and her graduate student Kerri Pratt installed Shirley, an
aircraft aerosol time-of-flight mass spectrometer (A-ATOFMS), onto a
C-130 operated by the National Center for Atmospheric Research.
(Shirley's partner "Laverne" was back at the UCSD campus with other
ATOFMS units "Jake" and "Elwood" and newer units.) The aircraft flew
through ice and liquid clouds over Wyoming during a series of
flights in fall 2007, channeling the residues of ice crystals and
cloud droplets to Shirley's intake valves. The mass spectrometer
collected second-by-second data about the chemical composition of
these cloud residues, providing information about cloud condensation
nuclei and ice nuclei, the aerosols around which moisture condenses.
This was the first aircraft deployment of the A-ATOFMS co-designed
by Prather.
Analysis of the ice crystal cores revealed that they were made up
almost entirely of either dust or biological particles such as
bacteria, fungal spores and plant material. While it has long been
known that microorganisms or parts of them get airborne and travel
great distances, this study is the first to yield in-situ data on
their participation in cloud ice processes.
Unclear from this experiment is whether any of the biological matter
included living organisms, a matter of key interest to scientists
trying to understand how bacteria can propagate around the world.
Also to be seen is how much the microbial particles and dust affect
rainfall, sometimes in places thousands of miles away from where the
aerosols originated.
Prather said initial evidence is increasingly suggesting that dust
transported from Asia could be influencing precipitation in North
America, for example. Researchers hope to use the ICE-L data to
design future studies timed to events when such particles may be
playing a bigger role in triggering rain or snowfall.
—Robert Monroe
June 2009
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