Convective injection into stratospheric intrusions alters the tropopause chemical structure.
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abstract
The tropopause chemical structure (TCS) is influenced by stratosphere-troposphere exchange (STE) and plays a role in the Earth's climate. However, this role is still not fully understood in East Asia, where active STE and high anthropogenic emissions coexist. Using airborne measurements of trace gases, including O3, CO, and H2O, we reveal the variations in TCS during two consecutive cut-off lows (COLs), an important trigger of STE. We demonstrate the important roles of two-way STE and long-range transport processes in delivering natural and anthropogenic signatures in the TCS. The former COL case shows a normal pattern of TCS, consisting of stratospheric and tropospheric air and a mixture of them. The latter, as a novel type of STE, exhibits an anomalous and complex structure due to deep convective injection into stratospheric intrusions and advection of remote marine air. The distinct mixture of stratospheric air and anthropogenic pollution alters the TCS, with horizontal and vertical scales estimated to be 200 and 1 km, respectively. Moreover, air of maritime origin, which is convectively transported and strongly dehydrated during long-range transport, is also identified. Such a complex TCS can produce unique chemical environments that modulate cloud physics and atmospheric radiation. From a climatological perspective, events of these anomalous airmasses are nonnegligible in terms of their frequency and chemical impact, as revealed by multiyear observations. These new insights advance our understanding of the mixing of natural and anthropogenic species that shape the TCS in East Asia and have implications for climate change.
