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A simple explanation for the increase in relative humidity between 11 and 14 km in the tropicsFOLKINS, Ian; KELLY, K. K; WEINSTOCK, E. M et al.Journal of geophysical research. 2002, Vol 107, Num D23, pp ACL26.1-ACL26.7, issn 0148-0227Article

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Closure of the total hydrogen budget of the northern extratropical lower stratosphereHURST, D. F; DUTTON, G. S; SCOTT, D. C et al.Journal of geophysical research. 1999, Vol 104, Num D7, pp 8191-8200, issn 0148-0227Article

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Validation and determination of ice water content-radar reflectivity relationships during CRYSTAL-FACE : Flight requirements for future comparisonsSAYRES, D. S; SMITH, J. B; PITTMAN, J. V et al.Journal of geophysical research. 2008, Vol 113, Num D5, issn 0148-0227, D05208.1-D05208.10Article

Comment on: Balloon-borne observations of water vapor and ozone in the tropical upper troposphere and lower stratosphere. Authors' replyDESSLER, A. E; WEINSTOCK, E. M; CORNEJO, J et al.Journal of geophysical research. 2003, Vol 108, Num D4, pp ACL3.1-ACL4.3, issn 0148-0227Article

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