Coupled aerosol-chemical modeling of UARS HNO3 and N2O5 measurements in the arctic upper stratosphere
Gas-phase photochemical models do not account for the formation of a secondary altitude HNO3 maximum in the upper stratosphere at high latitudes during winter, suggesting that some processes are missing in the currently accepted chemistry of reactive nitrogen species [Kawa et al., 1995]. Heterogeneo...
Main Authors: | , , , , , , , , |
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Format: | Journal article |
Published: |
1997
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