General Document on Common Questions and Answers on Cloud Seeding
The seasonal variability of VOCs along with meteorological parameters and associated sources over a high-altitude forested site in Western Ghats, India was investigated with a year-long dataset. The site receives predominately continental aged air masses except during monsoon. Biogenic emissions were dominant during pre-monsoon season. Isoprene was the largest emitted biogenic VOC in pre-monsoon (1.01 ppb). Observed monoterpene concentration had mixed biogenic and anthropogenic origin. Contribution of local traffic sources was evidenced at the SW of observation site. PMF analysis showed main contributions from biomass burning and aged air masses. The study revealed that VOCs over the high-altitude forested observation site is influenced by different types of anthropogenic and biogenic sources, which may further modulate the oxidative property of the atmosphere and may contribute largely to SOA formation.
Mukherjee S., Pandithurai G., Waghmare V., Mahajan A.S., Tinel L., Aslam M.Y., Meena G.S., Patil Sachin, Buchunde P., Kumar Anil, Atmospheric Environment, 331: 120598, August 2024, DOI:10.1016/j.atmosenv.2024.120598
Read MoreThis study aims to fix a problem in climate models where deep convection (intense storms) happens too often. Current models use traditional methods based on physics, like CAPE (a measure of storm potential), but these can be inaccurate. The study suggests using machine learning (ML) to parametrize occurrence of deep convection. Two ML methods, support vector machines and neural networks, are tested. The study also introduces a new way to determine which factors are most important for making these predictions. The ML methods are compared to the traditional CAPE-based approach and show better results. Additionally, a simple method based on the Mahalanobis distance is deployed as an easy-to-use alternative with similar accuracy with better interpretability. By improving deep convection trigger using ML, this study hopes to reduce the problem of excessive drizzle in climate models and improve rainfall prediction.
Kumar Siddharth, Mukhopadhyay P., Balaji C., Climate Dynamics, Online, July 2024, DOI:10.1007/s00382-024-07332-w, 1-18
Read MoreA decade long Black Carbon (BC) mass concentration, one of the highly absorbing species in the atmosphere was investigated over the central Indo-Gangetic Plain (IGP) during the period from 2009 to 2021. BC shows a significant decreasing trend over the central IGP since 2009, with a significant seasonal heterogeneity. The associated radiative forcing also shows a decreasing trend over the region on yearly scale since 2009. A decreasing trend in Black Carbon-Aerosol Radiative Forcing (BC-ARF) within the atmosphere relates to decrease in BC mass concentration and suggests reduced atmospheric warming.
Mehrotra B.J., Srivastava Atul K., Singh A., Parashar D., Majumder N., Singh R.S., Choudhary A., Srivastava M.K., Journal of Geophysical Research: Atmospheres, 129: e2024JD040754, July 2024, DOI:10.1029/2024JD040754, 1-19
Read MoreWith the changing climate, the study of fog formation is essential due to the impact of the complexity of natural and anthropogenic aerosols. The Eulerian–Lagrangian particle-based small-scale model for the diffusional growth of droplets is used to better understand the droplet activation and growth. The small-scale model simulations are performed using observed data from the Winter Fog Experiment study over Indira Gandhi International Airport, New Delhi. This study compared visibility from an existing parametrization with parcel–direct numerical simulation calculation. The hygroscopicity κ, which is highly related to the activation of aerosols to condensation nuclei, is taken into account to demonstrate the contribution of aerosol chemistry to fog droplet formation. The results highlight that hygroscopicity is essential in the numerical model for fog and visibility prediction as the microphysical properties of fog are regulated by aerosol species.
Bhowmik M., Hazra A., Ghude S.D., Wagh S., Chowdhury R., Parde A.N., Govardhan G., Gultepe I., Rajeevan M., Quarterly Journal of the Royal Meteorological Society, 150, July 2024, DOI:10.1002/qj.4729, 2690-2711
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