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1. Global perturbation of stratospheric water and aerosol burden by Hunga eruption

5. A long pathway of high water vapor from the Asian summer monsoon into the stratosphere

6. A long pathway of high water vapor from the Asian summer monsoon into the stratosphere

9. Microphysical Modeling of Water Isotopic Composition in the Asian Summer Monsoon

10. A long way of water vapor from the Asian Summer Monsoon into the stratosphere

11. Global perturbation of stratospheric water and aerosol burden by the Hunga Tonga eruption: a 1-year aftermath

12. The dehydration carousel of stratospheric water vapor in the Asian summer monsoon anticyclone.

14. Intercomparison of upper tropospheric and lower stratospheric water vapor measurements over the Asian Summer Monsoon during the StratoClim campaign

15. Global perturbation of stratospheric water and aerosol burden by Hunga eruption

16. Persistence of moist plumes from overshooting convection in the Asian monsoon anticyclone

17. Supplementary material to "Intercomparison of upper tropospheric and lower stratospheric water vapor measurements over the Asian Summer Monsoon during the StratoClim Campaign"

18. Evolution of tracer and ice crystal distribution in the young plumes of overshooting turrets from the StratoClim golden flight

19. Persistence of moist plumes from overshooting convection in the Asian monsoon anticyclone

20. Supplementary material to "Persistence of moist plumes from overshooting convection in the Asian monsoon anticyclone"

21. Evolution of tracer and ice crystal distribution in the young plumes of overshooting turrets from the StratoClim golden flight 

22. In-situ measurements of the HDO/H2O Isotopic ratio in the Asian Summer Monsoon trace strong convective activity

28. Persistence of moist plumes from overshooting convection in the Asian monsoon anticyclone.

32. No anomalous supersaturation in ultracold cirrus laboratory experiments.

33. Laboratory measurements of HDO/H2O isotopic fractionation during ice deposition in simulated cirrus clouds.

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