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Chemical Modeling of Stratospheric Chlorine Partitioning and Diurnal Variation ofNO2 and O3 for MAS and POAM

机译:平流层氯分配的化学模拟及mas和pOam中NO2和O3的日变化

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Using the JPL/CalTech O-D, time-dependent photochemical model, we compared theATLAS-3 MAS measurements to theoretical expectations. The latitudinal and altitudinal gradients are similar for latitudes south of 50 degrees North. Poleward of 50 degrees, unresolved differences remain. After using the model to identify potential problems, the altitude of the peak CIO volume mixing ratio agrees with theory.

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