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Modeling the TTL at Continental Scale for a Wet Season: An Evaluation of the BRAMS Mesoscale Model Using TRO-Pico Campaign, and Measurements From Airborne and Spaceborne Sensors

  • Abhinna K. Behera
  • , Emmanuel D. Rivière
  • , Virginie Marécal
  • , Jean François Rysman
  • , Claud Chantal
  • , Geneviève Sèze
  • , Nadir Amarouche
  • , Mélanie Ghysels
  • , Sergey M. Khaykin
  • , Jean Pierre Pommereau
  • , Gerhard Held
  • , Jérémie Burgalat
  • , Georges Durry
  • Centre national de la recherche scientifique
  • Météo-France/CNRS
  • Université Paris-Saclay
  • Division Technique
  • São Paulo State University

Research output: Contribution to journalArticlepeer-review

3 Citations (Scopus)

Abstract

In order to better understand the water vapor (WV) intrusion into the tropical stratosphere, a mesoscale simulation of the tropical tropopause layer using the BRAMS (Brazilian version of Regional Atmospheric Modeling System (RAMS)) model is evaluated for a wet season. This simulation with a horizontal grid point resolution of 20 km × 20 km cannot resolve the stratospheric overshooting convection (SOC). Its ability to reproduce other key parameters playing a role in the stratospheric WV abundance is investigated using the balloon-borne TRO-Pico campaign measurements, the upper-air soundings over Brazil, and the satellite observations by Aura Microwave Limb Sounder, Microwave Humidity Sounder, and Geostationary Operational Environmental Satellite 12. The BRAMS exhibits a good ability in simulating temperature, cold-point, WV variability around the tropopause. However, the simulation is typically observed to be warmer by ∼2.0°C and wetter by ∼0.4 ppmv at the hygropause, which can be partly affiliated with the grid boundary nudging of the model by European Centre for Medium-Range Weather Forecasts operational analyses. The modeled cloud tops show a good correlation (maximum cross-correlation of ∼0.7) with Geostationary Operational Environmental Satellite 12. Furthermore, the overshooting cells detected by Microwave Humidity Sounder are observed at the locations, where 75% of the modeled cloud tops are higher than 11 km. Finally, the modeled inertia-gravity wave periodicity and wavelength are comparable with those deduced from the radio sounding measurements during TRO-Pico campaign. The good behavior of BRAMS confirms the SOC contribution in the WV abundance, and variability is of lesser importance than the large-scale processes. This simulation can be used as a reference run for upscaling the impact of SOC at a continental scale for future studies.

Original languageEnglish
Pages (from-to)2491-2508
Number of pages18
JournalJournal of Geophysical Research: Atmospheres
Volume123
Issue number5
DOIs
Publication statusPublished - 16 Mar 2018
Externally publishedYes

Keywords

  • BRAMS
  • inertia-gravity waves
  • mesoscale modeling
  • stratospheric overshooting convection
  • tropical tropopause layer
  • water vapor budget

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