To What Extent Does High-Latitude Wave Forcing Drive Tropical Upwelling in the Brewer–Dobson Circulation?

Reply to comment by John R. Lanzante on “Trends in the temperature and water vapor content of the tropical lower stratosphere: Sea surface connection”

(2009) Karen H. Rosenlof et al.   JOURNAL OF GEOPHYSICAL RESEARCH

Comment on “Trends in the temperature and water vapor content of the tropical lower stratosphere: Sea surface connection” by Karen H. Rosenlof and George C. Reid

(2009) John R. Lanzante   JOURNAL OF GEOPHYSICAL RESEARCH

Higher tropical SSTs strengthen the tropical upwelling via deep convection

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The Strength of the Brewer–Dobson Circulation in a Changing Climate: Coupled Chemistry–Climate Model Simulations

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Improvements to NOAA’s Historical Merged Land–Ocean Surface Temperature Analysis (1880–2006)

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Trends in the temperature and water vapor content of the tropical lower stratosphere: Sea surface connection

(2008) Karen H. Rosenlof et al.   JOURNAL OF GEOPHYSICAL RESEARCH

QBO and annual cycle variations in tropical lower stratosphere trace gases from HALOE and Aura MLS observations

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Dynamical Balances and Tropical Stratospheric Upwelling

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Morphology of Tropical Upwelling in the Lower Stratosphere

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Acceleration of the Brewer–Dobson Circulation due to Increases in Greenhouse Gases

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