Monsoon low pressure systems (LPS) are synoptic scale disturbances that form over South Asia during the summer monsoon season and often produce extreme precipitation events, causing disastrous floods. Numerous modelling and observational studies have confirmed the role of convection as a major energy provider for the p...
The Indian Summer Monsoon Rainfall (ISMR) is strongly influenced by large-scale climate variability associated with the El Niño–Southern Oscillation (ENSO), the Indian Ocean Dipole (IOD), and the Madden–Julian Oscillation (MJO). While the individual influences of these climate modes on the monsoon are well established,...
The spatiotemporal variability in annual rainfall and rainfall erosivity (R factor) is a crucial factor in assessing seasonal soil erosion dynamics and regional water resource management, since it has a substantial impact on complex interactions involving the water, soil, and surroundings under the variable climate reg...
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