Deep convective influence on the Asian summer monsoon anticyclone and associated tracer variability observed with Atmospheric Infrared Sounder (AIRS)

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CALIPSO detection of an Asian tropopause aerosol layer (2011, background): “…of mineral dust from Taklamakan and Gobi deserts in the middle troposphere [Liu et al., 2008], that could be subsequently transported over the Indian Sub‐continents or/and Tibetan Plateau by deep convection associated with the Asian Monsoon [Li et al., 2005; Randel and Park, 2006; Fu et al., 2006].”
Impact of the vertical velocity scheme on modeling transport in the tropical tropopause layer (2010, background): “Irrespective of the scenario, the hemispheric asymmetry of in-mixing is likely due to the strong Asian monsoon anticyclone [Dunkerton, 1995; Gettelman et al., 2004b; Randel and Park, 2006], as the main in-mixing (for boreal summer) occurs in regions of equatorward flow of the anticyclonic circulatio”
Observational characteristics of double tropopauses (2007, background): “The Asian monsoon circulation includes a strong anticyclonic flow in the UTLS region, with a relatively high (tropical) tropopause extending to 30 N [Highwood and Hoskins, 1998; Randel and Park, 2006].”
Tropical tropopause layer (2009, background): “, 2004b; Randel and Park, 2006] and Tibetan Plateau [Gettelman et al., 2004b; Randel and Park, 2006; Fu et al., 2006] also play an important role.”