monsoonsubtropikon
Monsoonsubtropikon is a climatological term used to describe a secondary monsoon-like circulation that develops in subtropical latitude zones during late summer and early autumn. Unlike the primary monsoon, which results from the differential heating of continental landmasses and adjacent oceans, the monsoonsubtropikon is driven by interactions between land‑sea breezes, upper atmospheric troughs, and the monsoon trough itself.
The phenomenon is first noted in the central Asian steppes, where warm air from the interior is
Typical precipitation associated with monsoonsubtropikon events is moderate, with rainfall totals between 25 and 50 millimeters
From a meteorological perspective, monsoonsubtropikon acts as a subtle bridge between the dry post‑monsoon period and
Because of its relatively small scale, monsoonsubtropikon is often underrepresented in global climate models. However, emerging