TY - JOUR
T1 - Measurement of Flare Size Distribution and Simulation of Seeding Effect with a Spectral Bin Parcel Model
AU - Konwar, Mahen
AU - Malap, Neelam
AU - Hazra, Anupam
AU - Axisa, Duncan
AU - Prabhakaran, Thara
AU - Khain, Alexander
N1 - Publisher Copyright:
© 2023, The Author(s), under exclusive licence to Springer Nature Switzerland AG.
PY - 2023/8
Y1 - 2023/8
N2 - Cloud seeding experiments were conducted during the Cloud Interaction and Precipitation Enhancement Experiment (CAIPEEX) near Hyderabad, India, in 2011. Here, we report both the background aerosol and hygroscopic flare size distributions measured during the airborne experiment. The size distributions were measured in the diameter (D) range of 0.02–50 µm; both ultra-fine (0.02 µm < D < 0.1 µm) and coarse mode (D > 0.5 µm) particles were in greater concentrations in flare than in the background aerosols. The sensitivity of cloud droplet growth to the flare particle size distribution is studied with the help of a 2000-spectral bin parcel model, where droplet growth, collisions, and formation of raindrops are represented. The simulation results indicate the rapid formation of warm rain in cloud due to the tail effect of activation of coarse mode aerosols into large size cloud droplets. At higher altitudes, in-cloud activation and a secondary mode in drop size distribution are noted. For a given cloud base updraft, the rain flux increases with the increase in the coarse mode aerosol concentrations. However, for a given coarse mode aerosol concentration, the rain flux decreases with increasing cloud base updrafts.
AB - Cloud seeding experiments were conducted during the Cloud Interaction and Precipitation Enhancement Experiment (CAIPEEX) near Hyderabad, India, in 2011. Here, we report both the background aerosol and hygroscopic flare size distributions measured during the airborne experiment. The size distributions were measured in the diameter (D) range of 0.02–50 µm; both ultra-fine (0.02 µm < D < 0.1 µm) and coarse mode (D > 0.5 µm) particles were in greater concentrations in flare than in the background aerosols. The sensitivity of cloud droplet growth to the flare particle size distribution is studied with the help of a 2000-spectral bin parcel model, where droplet growth, collisions, and formation of raindrops are represented. The simulation results indicate the rapid formation of warm rain in cloud due to the tail effect of activation of coarse mode aerosols into large size cloud droplets. At higher altitudes, in-cloud activation and a secondary mode in drop size distribution are noted. For a given cloud base updraft, the rain flux increases with the increase in the coarse mode aerosol concentrations. However, for a given coarse mode aerosol concentration, the rain flux decreases with increasing cloud base updrafts.
KW - CAIPEEX
KW - Cloud seeding
KW - Hygroscopic flare
KW - Spectral-bin parcel model
UR - http://www.scopus.com/inward/record.url?scp=85165884612&partnerID=8YFLogxK
U2 - 10.1007/s00024-023-03293-z
DO - 10.1007/s00024-023-03293-z
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AN - SCOPUS:85165884612
SN - 0033-4553
VL - 180
SP - 3019
EP - 3034
JO - Pure and Applied Geophysics
JF - Pure and Applied Geophysics
IS - 8
ER -