452A Estimating Mean Supersaturation in a Laboratory Convection Cloud Chamber

Tuesday, 14 January 2025
Hall C (New Orleans Ernest N. Morial Convention Center)
Steven K. Krueger, Univ. of Utah, SALT LAKE CITY, UT; and G. Daniels, J. C. Anderson, K. K. Chandrakar, PhD, M. Rajagopal, D. H. Richter, R. A. Shaw, and K. J. Swartz-Schult

Laboratory convection cloud chambers (such as the Pi Chamber at Michigan Technological University) produce supersaturation by turbulent mixing of saturated air parcels that have different temperatures. The parcels originate from the warm saturated lower surface and the cool saturated upper surface. A steady state is easy to in such a chamber when CCN are continuously injected and a balance is achieved between CCN injection and droplet growth and droplet fallout. In the simple case of uniform supersaturation and injection of small water droplets (instead of CCN), the droplet radius PDF depends solely on the supersaturation. In the chamber however, the PDF depends also depends on the supersaturation fluctuations and the CCN properties.

Measurements of water vapor in the Pi Chamber have been made by using an infrared hygrometer. Anderson et al. (2021, 2024) combined these with temperature measured by a sonic temperature sensor to calculate supersaturation. This approach provides estimates of both mean and fluctuating supersaturation. However, Anderson et al. (2024) noted limitations in their ability to measure the absolute magnitude of the supersaturation, which has motivated us to investigate methods of inferring the chamber mean supersaturation using additional or alternative measurements.

One such approach relies on the measured particle size distribution (PSD). PSDs are measured in the Pi Chamber using the WELAS2000 Digital Optical Particle Counter. We derived an equation to estimate the mean supersaturation from the measured PSD and the injected CCN properties. The equation is valid if the chamber is well-mixed. We are in the process of testing this method using particle-resolving simulations of the Pi Chamber. We are using the One-Dimensional Turbulence (ODT) model, and two direct numerical simulation (DNS) models (from NSF NCAR and University of Notre Dame). The results are accurate when the mean supersaturation is positive (as shown in the graphic), but not so when the mean supersaturation is negative. We suspect that the inaccurate results occur when the well-mixed assumption is violated.

We are currently investigating a version of the PSD method that is more general, as well as another method that relies on comparisons of measured and theoretical ratios of moments of the PDF in conjunction with the measured supersaturation variance (which should be more reliable than the measured mean supersaturation).

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