ACP Atmospheric Chemistry and Physics ACP 1680-7324 Copernicus GmbH Göttingen, Germany 10.5194/acp-6-2539-2006 The impact of cirrus clouds on tropical troposphere-to-stratosphere transport Corti T. 1 Luo B. P. 1 Fu Q. 2 Vömel H. 3 Peter T. 1 Institute for Atmospheric and Climate Science, ETH Zurich, Switzerland Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO, USA 03 07 2006 6 9 2539 2547 This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. This article is available from http://www.atmos-chem-phys.net/6/2539/2006/acp-6-2539-2006.html The full text article is available as a PDF file from http://www.atmos-chem-phys.net/6/2539/2006/acp-6-2539-2006.pdf

Although it is well known that air enters the stratosphere preferentially through upwelling in the tropics, the exact mechanisms of troposphere-to-stratosphere transport (TST) are still unknown. Previously proposed mechanisms have been found either to be too slow (e.g., clear sky upwelling) to provide agreement with in situ tracer measurements, or to be insufficient in mass flux to act as a major supply for the Brewer-Dobson circulation (e.g., convective overshooting). In this study we evaluate whether the lofting of air via cirrus cloud-radiation interaction might offer an alternative path for TST, which is responsible for a significant fraction of the observed air mass transport. We find that a combination of deep convection and subsequent upwelling associated with cirrus clouds and clear sky can explain the supply of air for the Brewer-Dobson circulation. Thus, upwelling associated with cirrus clouds offers a mechanism for the missing second stage, which links the first stage of TST, deep convection, to the third stage, the Brewer-Dobson circulation.

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