Articles | Volume 25, issue 16
https://doi.org/10.5194/acp-25-9295-2025
https://doi.org/10.5194/acp-25-9295-2025
Research article
 | 
26 Aug 2025
Research article |  | 26 Aug 2025

Aerosol impacts on isolated deep convection: findings from TRACER

Dié Wang, Roni Kobrosly, Tao Zhang, Tamanna Subba, Susan van den Heever, Siddhant Gupta, and Michael Jensen

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Cited articles

Abbott, T. H. and Cronin, T. W.: Aerosol invigoration of atmospheric convection through increases in humidity, Science, 371, 83–85, https://doi.org/10.1126/science.abc5181, 2021. a, b, c
Anagnostou, E. N.: A convective/stratiform precipitation classification algorithm for volume scanning weather radar observations, Meteorol. Appl., 11, 291–300, https://doi.org/10.1017/S1350482704001409, 2004. a
Andreae, M. O., Rosenfeld, D., Artaxo, P., Costa, A. A., Frank, G., Longo, K. M., and Silva-Dias, M. A. F. d.: Smoking rain clouds over the Amazon, Science, 303, 1337–1342, 2004. a
Baidu, M., Schwendike, J., Marsham, J. H., and Bain, C.: Effects of vertical wind shear on intensities of mesoscale convective systems over West and Central Africa, Atmos. Sci. Lett., 23, e1094, https://doi.org/10.1002/asl.1094, 2022. a, b
Barth, M. C., Cantrell, C. A., Brune, W. H., Rutledge, S. A., Crawford, J. H., Huntrieser, H., Carey, L. D., MacGorman, D., Weisman, M., Pickering, K. E., Bruning, E., Anderson, B., Apel, E., Biggerstaff, M., Campos, T., Campuzano-Jost, P., Cohen, R., Crounse, J., Day, D. A., Diskin, G., Flocke, F., Fried, A., Garland, C., Heikes, B., Honomichl, S., Hornbrook, R., Huey, L. G., Jimenez, J. L., Lang, T., Lichtenstern, M., Mikoviny, T., Nault, B., O’Sullivan, D., Pan, L. L., Peischl, J., Pollack, I., Richter, D., Riemer, D., Ryerson, T., Schlager, H., Clair, J. S., Walega, J., Weibring, P., Weinheimer, A., Wennberg, P., Wisthaler, A., Wooldridge, P. J., and Ziegler, C.: The Deep Convective Clouds and Chemistry (DC3) Field Campaign, B. Am. Meteoro. Soc., 96, 1281–1309, https://doi.org/10.1175/BAMS-D-13-00290.1, 2015. a
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We aim to understand how tiny particles in the air, called aerosols, affect rain clouds in the Houston–Galveston area. More aerosols generally do not make these clouds grow much taller, with an average height increase of about 1 km. However, their effects on rainfall strength and cloud expansion are less certain. Clouds influenced by sea breezes show a stronger aerosol impact, possibly due to factors that are unaccounted for like vertical winds in near-surface layers.
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