JpGU-AGU Joint Meeting 2017

講演情報

[EE] 口頭発表

セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS09] [EE] 成層圏-対流圏相互作用 ―統一領域としての新しい視点―

2017年5月23日(火) 13:45 〜 15:15 A10 (東京ベイ幕張ホール)

コンビーナ:江口 菜穂(Kyushu University)、Rei Ueyama(NASA Ames Research Center)、Sean M Davis(NOAA Boulder)、Seok Woo Son(Seoul National University)、座長:江口 菜穂(九州大学)、座長:Ueyama Rei(NASA Ames Research Center)、座長:Son Seok-Woo(Seoul National University)

14:00 〜 14:15

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

★招待講演

*Aurelien Podglajen1Leonhard Pfister2Eric J Jensen2Thaopaul V Bui2Jonathan Dean-Day2Joan Alexander3Albert Hertzog1Bernd Karcher4Riwal Plougonven1William 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)

キーワード: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.