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Dependence of Deep Convective Cell Properties on Meteorological and Aerosol Conditions during TRACER

  • Dhwanit J. Mise
  • , Yongjie Huang
  • , Greg M. McFarquhar
  • , Ming Xue
  • , Alexander V. Ryzhkov
  • , Jeffrey Snyder
  • , Lulin Xue
  • , Mariko Oue
  • , Pavlos Kollias
  • , Michael P. Jensen
  • , Mateusz Taszarek
  • University of Oklahoma
  • National Oceanic and Atmospheric Administration
  • National Center for Atmospheric Research
  • Stony Brook University
  • Brookhaven National Laboratory
  • Adam Mickiewicz University in Poznań

Research output: Contribution to journalArticlepeer-review

Abstract

Deep convective cells significantly influence Earth’s energy balance and water cycle. However, their accurate representation in numerical models remains challenging due to their small spatiotemporal scales and limited observational constraints. This study examines over ~400 deep convective cells near Houston, observed by a dual-polarization C-band radar during the Tracking Aerosol Convection Interactions Experiment (TRACER) intensive observation period (June–September 2022). Cells are categorized by lifetime into short-lived (<40 min), intermediate-lived (40–80 min), and long-lived (80+ min) groups. Long-lived cells were broader (~13.2 km at 2–4-km height) and deeper (~11.4 km) than short-lived cells (~6.4-km width, ~7.31-km height). Using random forest (RF) modeling and correlation analyses, precipitable water vapor (PWV), 2–6-km lapse rate, 0–8-km bulk shear, and fine aerosol mass concentration (Mass_f) are identified as key predictors of cell lifetime. Higher PWV is associated with significantly longer convective cell lifetimes compared to the low-PWV group, particularly within low 2–6-km temperature lapse rate (LR_26km), moderate-to-higher 0–8-km bulk shear (BS_08km), and low-to-moderate Mass_f environments. RF analysis also identifies low-level (0–2 km) equivalent potential temperature, PWV, Mass_f, and surface latent heat flux as key predictors for cell width and height. Short-lived cells have higher aerosol number concentrations (500–1000-nm size range), linked to onshore wind conditions and marine aerosols; however, their low concentration suggests the sensitivity may reflect associated meteorological regimes rather than a direct aerosol effect. Long-lived cells have higher concentrations of organic and sulfate aerosols, while short-lived cells exhibit higher black carbon concentrations. These results highlight the intricate dependence of convective cell lifetimes and structure on environmental moisture, thermodynamics, wind shear, and aerosol characteristics.

Original languageEnglish
Pages (from-to)1291-1317
Number of pages27
JournalJournal of the Atmospheric Sciences
Volume83
Issue number7
DOIs
StatePublished - Jul 2026
Externally publishedYes

Keywords

  • Aerosol-cloud interaction
  • Clustering
  • Coastal meteorology
  • Convective storms
  • Radars/radar observations
  • Surface observations

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