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The following is an excerpt of a story originally published by the U.S. Department of Energy’s (DOE) Atmospheric Radiation Measurement (ARM) User Facility. Michael P. Jensen, a meteorologist at DOE’s Brookhaven National Laboratory, is the lead scientist for the study. For more information about Brookhaven’s role or to speak with a Brookhaven Lab scientist, contact Karen McNulty Walsh, (631) 344-8350, firstname.lastname@example.org.
New Campaign Will Track Deep Convective Clouds Over Houston
Scientists will gather detailed data on aerosol-cloud interactions within deep convective systems
January 23, 2019
Deep convective clouds will be the focus of an upcoming ARM field campaign in Texas. Credit: Courtesy of the National Weather Service
Deep convective clouds—the kind that often pack lightning and pour rain—occur nearly everywhere in the world. They are an important feature of the atmosphere, especially in storm systems that dominate the tropics and midlatitudes.
To poets, these harbingers of storms are a durable inspiration. German writer Johann Wolfgang von Goethe saw them as “the mad thunder-cloud, (where) fierce legions clash.”
Outside the realm of verse, scientists are still struggling to know what goes on inside convective clouds—exactly how their “fierce legions” of energy and mass combine and interact.
In 2011, Michael P. Jensen of Brookhaven Lab, second from left, was principal investigator for MC3E, one of the ARM field campaigns that informed the TRACER science plan. With Jensen, from left, are Scott Giangrande (Brookhaven) and Pavlos Kollias (then at McGill, but now a joint appointee of Stony Brook University and Brookhaven Lab), who are now TRACER co-investigators, and Nitin Bharadwaj (Pacific Northwest National Laboratory), principal engineer for ARM's radar group. Credit: Courtesy of the U.S. Department of Energy Atmospheric Radiation Measurement (ARM) user facility.
Says Michael P. Jensen, a meteorologist at Brookhaven National Laboratory in Upton, New York: “We still don’t understand important details about how atmospheric convection works”—at least not well enough to represent convective clouds in models with acceptable accuracy.
In particular, many researchers are vexed by how aerosols influence the physics of such clouds, including the precipitation processes and vertical velocities that affect rates of cloud growth, ice formation, and lightning occurrence.
Aerosols are solid or liquid particles dispersed into the atmosphere by natural sources (such as tree cover) and artificial ones (such as cars and coal plants). Under the right conditions, aerosols help clouds form, and in this way play an important part in weather and climate patterns.
Finding out what happens inside deep convective clouds is the aim of a new field campaign for which Jensen is principal investigator.
The Tracking Aerosol Convection Interactions Experiment (TRACER) got the go-ahead in mid-October 2018 from the U.S. Department of Energy’s Atmospheric Radiation Measurement (ARM) user facility.
With ARM mobile instruments in place, TRACER is scheduled to run from April 2021 to April 2022 in and around Houston, Texas.
“We want to focus on the convective core,” says Jensen. “We need very detailed measurements of the convective updraft—including the vertical winds and cloud microphysics—and how they evolve over the cloud life cycle, and under varying atmospheric conditions.”
To date, he adds, the microphysical processes within convective clouds are represented only in a limited way in the parameterizations used in models of both weather and global climate.
A map from the TRACER science plan shows the proposed approximate deployment areas for the first ARM Mobile Facility (AMF1) near the La Porte, Texas, airport; the CSAPR2 near Manvel-Croix, Texas, with 25-kilometer and 75-kilometer range rings; and an ancillary ARM site.
One related controversy is prominent today among scientists, says Jensen. Do aerosols invigorate deep convective storms? Some scientists say yes: Such particles affect the growth of cloud droplets, accelerate updrafts, cause more rain, and enhance turbulence and mixing.
Jiwen Fan, an atmospheric scientist at Pacific Northwest National Laboratory (PNNL) in Richland, Washington, argued for the rain-making power of fine aerosols as lead author of a 2018 paper in the journal Science. Other scientists doubt a connection.
Meanwhile, present climate and weather models overestimate how strong these updrafts are within convective clouds. It’s one of the model biases—offsets from observations—that TRACER is designed to correct.
“In the end,” says Jensen, “that’s what we’re trying to do. We’re trying to improve the representation of these clouds in climate models.”
ARM is a DOE Office of Science user facility operated by nine DOE national laboratories.
Brookhaven National Laboratory is supported by the Office of Science of the U.S. Department of Energy. The Office of Science is the single largest supporter of basic research in the physical sciences in the United States, and is working to address some of the most pressing challenges of our time. For more information, please visit science.energy.gov.
2019-14346 | INT/EXT | Newsroom