Abstract. Measurements from HALOE indicate that there hasIn Plate 1 we show the a7 term calculated from fitting the been a significant decrease in CI-I• in the middle to upper HALOE CI-In measurements with (1). Since CH4 exhibits little stratosphere from 1991-1997. Two dimensional model diurnal variation, the result shown is calculated from a single calculations suggest that a decrease in the tropical upwelling is least-squares-fit to (1) after combining the sunrise and sunset the most plausible explanation f…
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