Preprints
https://doi.org/10.5194/acp-2020-1010
https://doi.org/10.5194/acp-2020-1010

  27 Oct 2020

27 Oct 2020

Review status: a revised version of this preprint was accepted for the journal ACP and is expected to appear here in due course.

Processes influencing lower stratospheric water vapour in monsoon anticyclones: insights from Lagrangian modeling

Nuria Pilar Plaza1, Aurélien Podglajen2, Cristina Peña-Ortiz1, and Felix Ploeger3,4 Nuria Pilar Plaza et al.
  • 1Área de Física de la Tierra. Departamento de Sistemas Físicos, Químicos y Naturales. Universidad Pablo de Olavide, Sevilla, Spain
  • 2Laboratoire de Météorologie Dynamique (LMD/IPSL), École polytechnique, Institut polytechnique de Paris, Sorbonne Université, École normale supérieure, PSL Research University, CNRS, Paris, France
  • 3Institute of Climate Research. Forschungszentrum Jülich, Jülich, Germany
  • 4Institute for Atmospheric and Environmental Research, University of Wuppertal, Wuppertal, Germany

Abstract. We investigate the influence of different chemical and physical processes on the water vapour distribution in the lower stratosphere (LS), in particular in the Asian and North-American monsoon anticyclones (AMA and NAMA, respectively). Specifically, we analyze effects of large-scale temperatures, methane oxidation, ice microphysics, and small-scale atmospheric mixing processes in model experiments with the chemistry transport model CLaMS. All these processes hydrate the LS, in particular over the Asian Monsoon. While ice microphysics has the largest global moistening impact, it is small-scale mixing which dominates the specific signature in the AMA. In particular, the small-scale mixing parameterization strongly contributes to the seasonal and intra-seasonal variability of water vapour in that region and including it in the model simulations results in a significantly improved agreement with observations. Although none of our experiments reproduces the spatial pattern of the NAMA seen in MLS observations, they all exhibit a realistic annual cycle and intra-seasonal variability, which are mainly controlled by temperatures. We further analyse the sensitivity of these results to the domain-filling trajectory set-up used in the five model experiments, here-called Lagrangian Trajectory Filling (LTF). Compared with MLS observations and with a multiyear reference simulation using the standard version of CLaMS, we find that LTF schemes result in a drier global LS and drier water vapour signal over the monsoon regions. Besides, the intra-seasonal variability of water vapour in the AMA is less correlated with MLS during June--August. We relate these results to the fact that the LTF schemes produce a low density of air parcels in the moistest areas of the AMA.

Nuria Pilar Plaza et al.

 
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Status: closed
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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Nuria Pilar Plaza et al.

Nuria Pilar Plaza et al.

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Short summary
We study the role of different processes in setting the lower stratospheric water vapour. We find that mechanisms involving ice microphysics and small-scale mixing produce the strongest increase of water vapour, in particular over the Asian Monsoon. Small-scale mixing has a especial relevance as it improves the agreement with observations at seasonal and intraseasonal timescales, in opposition with the North American Monsoon case, in which large-scale temperatures still dominate its variability.
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