C3LOUD-Ex: Raising the curtain on convection
Heever, Susan C. van den ; Grant, Leah D. ; Freeman, Sean W. ; Marinescu, Peter J. ; Barnum, Julie ; Bukowski, Jennie ; Casas, Eleanor ; Drager, Aryeh J. ; Fuchs, Brody ; Herman, Gregory R. ; Hitchcock, Stacey M. ; Kennedy, Patrick C. ; Nielsen, Erik R. ; Park, J. Minnie ; Rasmussen, Kristen ; Razin, Muhammad Naufal ; Riesenberg, Ryan ; Dellaripa, Emily Riley ; Slocum, Christopher J. ; Toms, Benjamin A. ; Heever, Adrian van den
The Colorado State University Convective CLoud Outflows and UpDrafts Experiment (C3LOUD-Ex)
The intensity of deep convective storms is driven in part by the strength of their updrafts and cold pools. In spite of the importance of these storm features, they can be poorly represented within numerical models. This has been attributed to model parameterizations, grid resolution, and the lack of appropriate observations with which to evaluate such simulations. The overarching goal of the Colorado State University Convective CLoud Outflows and UpDrafts Experiment (C3LOUD-Ex) was to enhance our understanding of deep convective storm processes and their representation within numerical models. To address this goal, a field campaign was conducted during July 2016 and May-June 2017 over northeastern Colorado, southeastern Wyoming, and southwestern Nebraska. Pivotal to the experiment was a novel "Flying Curtain" strategy designed around simultaneously employing a fleet of uncrewed aerial systems (UAS; or drones), high-frequency radiosonde launches, and surface observations to obtain detailed measurements of the spatial and temporal heterogeneities of cold pools. Updraft velocities were observed using targeted radiosondes and radars. Extensive datasets were successfully collected for 16 cold pool-focused and seven updraft-focused case studies. The updraft characteristics for all seven supercell updraft cases are compared and provide a useful database for model evaluation. An overview of the 16 cold pools' characteristics is presented, and an in-depth analysis of one of the cold pool cases suggests that spatial variations in cold pool properties occur on spatial scales from O(100) m through to O(1) km. Processes responsible for the cold pool observations are explored and support recent high-resolution modeling results.</p>
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