Tropical tropopause layer Public Deposited

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  • Observations of temperature, winds, and atmospheric trace gases suggest that the transition from troposphere to stratosphere occurs in a layer, rather than at a sharp ‘‘tropopause.’’ In the tropics, this layer is often called the ‘‘tropical tropopause layer’’ (TTL). We present an overview of observations in the TTL and discuss the radiative, dynamical, and chemical processes that lead to its timevarying, three-dimensional structure. We present a synthesis definition with a bottom at 150 hPa, 355 K, 14 km (pressure, potential temperature, and altitude) and a top at 70 hPa, 425 K, 18.5 km. Laterally, the TTL is bounded by the position of the subtropical jets. We highlight recent progress in understanding of the TTL but emphasize that a number of processes, notably deep, possibly overshooting convection, remain not well understood. The TTL acts in many ways as a ‘‘gate’’ to the stratosphere, and understanding all relevant processes is of great importance for reliable predictions of future stratospheric ozone and climate.
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  • Fueglistaler, S., Dessler, A. E., Dunkerton, T. J., Folkins, I., Fu, Q., & Mote, P. W. (2009). Tropical tropopause layer. Reviews of Geophysics, 47. doi:10.1029/2008RG000267
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  • description.provenance : Made available in DSpace on 2010-10-05T22:12:37Z (GMT). No. of bitstreams: 1 Fueglistaler_et_al_Rev_Geophys_2009.pdf: 1560018 bytes, checksum: 183a205f9668bba30d2d5c90de09faf3 (MD5) Previous issue date: 2009-02-17
  • description.provenance : Submitted by Eric Vanderwall (ewscanner@gmail.com) on 2010-09-15T18:37:30Z No. of bitstreams: 1 Fueglistaler_et_al_Rev_Geophys_2009.pdf: 1560018 bytes, checksum: 183a205f9668bba30d2d5c90de09faf3 (MD5)
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