Using version 19 Halogen Occultation Experiment (HALOE) data, we estimate the abundance of water vapor entering the stratosphere [H 2 O] e is 3.80±0.49 ppmv averaged over 1993–1997. The average of all of the recently published estimates of [H 2 O] e is 3.85 ppmv, which we believe is the best estimate of [H 2 O] e .
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Dessler et al. (1999) studied this question.
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