Preprints
https://doi.org/10.5194/egusphere-2026-2688
https://doi.org/10.5194/egusphere-2026-2688
11 Jun 2026
 | 11 Jun 2026
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

A Triple-Structured Mesospheric Climate Pattern Driven by a Double-Celled Meridional Circulation during the Equinox-Solstice Transition Months of November and May

Liang Zhang and Zhongfang Liu

Abstract. The upper mesosphere is a dynamically and chemically complex region where interannual climate variability remains incompletely understood, particularly during the transition months between the equinox and solstice circulation regimes. Using multi-satellite observations from MLS and SABER, we investigate the coupled dynamical-microphysical-chemical-thermal structures during November and May, building on the bottom-up mechanism of “upwelling—water vapor (H2O)—ozone (O3)—temperature”. We employ temperature near 80 km (the T80 index) as a proxy for upwelling intensity and identify two distinct centers: a summer polar upwelling and a tropical upwelling. Together they drive a double-celled anomalous meridional circulation that organizes the global climate into a novel triple-structured pattern, with coherent signatures in the summer high-latitude, equatorial, and winter high-latitude regions. A key finding is that hydration occurs below polar mesospheric clouds (PMCs) without pronounced dehydration above them. This “hydration-without-dehydration” configuration, made possible by the weak PMCs typical of November and May, indicates the dominance of the cold-trap effect over the conventional freeze-drying effect. The absence of dehydration further isolates the temperature-dependent ozone kinetic pathway for polar ozone enhancement, a pathway that is otherwise convolved with dehydration effects in stronger PMC seasons. Ozone and atomic oxygen (O) respond to the combined influences of meridional H2O transport and local thermal forcing, and the resulting radiative and chemical heating governs temperatures near 90 km (T90). These results establish the structure of the transitional climate regime, demonstrating that the shift from symmetric (equinox) to antisymmetric (solstice) variability is mediated by a well-organized, upwelling-driven double-celled circulation.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
Share
Liang Zhang and Zhongfang Liu

Status: open (until 23 Jul 2026)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
Liang Zhang and Zhongfang Liu
Liang Zhang and Zhongfang Liu
Metrics will be available soon.
Latest update: 11 Jun 2026
Download
Short summary
For transition months of November/May between equinox and solstice, satellite observations identify a double-celled anomalous meridional circulation driven by coexisting summer polar and tropical upwellings, which organizes a triple-structured mesospheric climate pattern across summer hemisphere, equator, and winter hemisphere. The “hydration-without-dehydration” signature under weak polar mesospheric clouds supports the cold-trap effect and clarifies the thermal pathway for ozone enhancement.
Share