JpGU-AGU Joint Meeting 2017

Presentation information

[EE] Oral

A (Atmospheric and Hydrospheric Sciences) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS09] [EE] Stratosphere - Troposphere Interaction

Tue. May 23, 2017 1:45 PM - 3:15 PM A10 (Tokyo Bay Makuhari Hall)

convener:Nawo Eguchi(Kyushu University), Rei Ueyama(NASA Ames Research Center), Sean M Davis(NOAA Boulder), Seok Woo Son(Seoul National University), Chairperson:Nawo Eguchi(Kyushu University), Chairperson:Rei Ueyama(NASA Ames Research Center), Chairperson:Seok-Woo Son(Seoul National University)

2:00 PM - 2:15 PM

[AAS09-02] Small-scale wind fluctuations in the tropical tropopause layer from aircraft measurements : relationship with clouds and convection and impact on vertical mixing

★Invited papers

*Aurelien Podglajen1, Leonhard Pfister2, Eric J Jensen2, Thaopaul V Bui2, Jonathan Dean-Day2, Joan Alexander3, Albert Hertzog1, Bernd Karcher4, Riwal Plougonven1, William Randel5 (1.Laboratoire de Météorologie Dynamique, Ecole Polytechnique, 2.NASA Ames Research Center, 3.NorthWest Research Associates CoRA Office, 4.DLR, 5.National Center for Atmospheric Research)

Keywords:tropical tropopause layer, turbulent mixing, aircraft measurements

Turbulent vertical mixing in the tropical tropopause layer (TTL) is poorly known, although it could make a substantial contribution to the heat and tracer transport budgets in that part of the atmosphere. Past observations of small-scale turbulence in the TTL with Radar and radiosondes have been limited to a few tropical locations. Recently, during the ATTREX (Airborne Tropical TRopopause EXperiment) and POSIDON (Pacific Oxidants, Sulfur, Ice, Dehydration, and cONvection) campaigns, in situ measurements from scientific aircraft have provided extensive sampling of small-scale motions over the tropical Pacific, between 14 and 20 km.

In this presentation, high-frequency meteorological observations collected during those recent aircraft campaigns are used to characterize the occurrence of ‘‘clear air turbulence’’ in the TTL. Turbulent bursts are highly intermittent, and are more frequent and intense in the lower TTL and near deep convection. The relationship between turbulent bursts and cirrus clouds is quantified. Finally, the impact of "turbulent" bursts on vertical mixing is estimated and contrasted between convective and non convective regions. The estimated diffusivities are compared with those predicted by turbulent diffusion schemes used in operational analyses systems.