Articles | Volume 12, issue 24
https://doi.org/10.5194/acp-12-12183-2012
https://doi.org/10.5194/acp-12-12183-2012
Research article
 | 
21 Dec 2012
Research article |  | 21 Dec 2012

Quantifying the deep convective temperature signal within the tropical tropopause layer (TTL)

L. C. Paulik and T. Birner

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Cited articles

Brewer, A. W.: Evidence for a world circulation provided by the measurements of helium and water vapor distribution in the stratosphere, Q. J. Roy. Meteor. Soc., 75, 351–363, 1949.
Chae, J. H., Wu, D. L., Read, W. G., and Sherwood, S. C.: The role of tropical deep convective clouds on temperature, water vapor, and dehydration in the tropical tropopause layer (TTL), Atmos. Chem. Phys., 11, 3811–3821, https://doi.org/10.5194/acp-11-3811-2011, 2011.
Fierro, A. O., Simpson, J., LeMone, M. A., Straka, J. M., and Smull, B. F.: On how hot towers fuel the Hadley cell: An observational and modeling study of line-organized convection in the equatorial trough from TOGA COARE, J. Atmos. Sci., 66, 2730–2746, 2009.
Folkins, I. and Martin, R. V.: The vertical structure of tropical convection and its impact on the budgets of water vapor and ozone, J. Atmos. Sci., 62, 1560–1573, 2005.
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