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Discussion papers
https://doi.org/10.5194/acp-2018-707
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-2018-707
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 23 Jul 2018

Research article | 23 Jul 2018

Review status
This discussion paper is a preprint. A revision of the manuscript is under review for the journal Atmospheric Chemistry and Physics (ACP).

Impact of upstream moisture structure on a back-building convective precipitation system in south-eastern France during HyMeX IOP13

Keun-Ok Lee1, Cyrille Flamant2, Fanny Duffourg3, Véronique Ducrocq3, and Jean-Pierre Chaboureau1 Keun-Ok Lee et al.
  • 1Laboratoire d’Aérologie, Université de Toulouse, CNRS, UPS, Toulouse, France
  • 2LATMOS/IPSL, CNRS, Sorbonne Université and Université Paris-Saclay, Paris, France
  • 3CNRM, UMR 3589, Université de Toulouse, Météo-France & CNRS, Toulouse, France

Abstract. The present study examines the impact of the environmental moisture structure in the lower troposphere (below 2km above sea level, ASL) on the precipitation development, observed in southern France during intensive observation period 13 of the first Special Observation Period of the Hydrological cycle in the Mediterranean Experiment (HyMeX SOP-1), through a series of sensitivity experiments using the non-hydrostatic numerical model Meso-NH. The control simulation (CNTL) and all the other 12 sensitivity experiments examined in this study succeed in reproducing a heavy precipitation event (HPE) in the coastal mountainous region of Var in south-eastern France as observed. The sensitivity experiments are designed to investigate the response of the variability of the water vapour content upstream in the moist marine atmospheric boundary layer (MABL) and the drier air above on the HPE. The comparisons between CNTL and the 12 sensitivity experiments show how the life cycle of precipitation associated with the HPE, but also the upstream flow (over the sea), is modified, even for moisture contents changes of only 1gkg−1 below 2km ASL. Within the low-level wind convergence between southerlies and south-westerlies, a small increase of moisture content in the MABL prolongs moderate precipitation (≥5mm in 15min) and enlarges the area of weak precipitation (≥1mm in 15min). The moistening in the 1–2km ASL layer, just above the MABL, prolongs the duration of moderate precipitation, for a similar total precipitation amount as in CNTL. The drier MABL and 1–2km ASL layer shorten both the life-time of precipitation and the total precipitation amount with respect to CNTL. We also found that the moisture in the MABL has a stronger impact on producing enhanced precipitation (both in terms of amount and intensity) than the moisture just above (1–2km ASL). Also it is worth noting that adding moisture in the MABL does not necessarily lead to enhanced precipitation amount. At the same time, the duration of moderate precipitation increases with increasing moisture as does the area covered by weak precipitations, while the area covered by the intense precipitation (≥30mm) decreases. Despite a simplified moisture-profile modification approach, this study suggests that moisture structure in lower troposphere is a key for accurate prediction at short-term range of the timing and location of precipitation in the coastal mountainous region in southern France.

Keun-Ok Lee et al.
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Status: final response (author comments only)
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Keun-Ok Lee et al.
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