Abstract
A new two-dimensional model with detailed photochemistry is presented. The model includes a detailed description of photochemical processes in the stratosphere and mesosphere. The downward transport of H2, H2O, and NOy from the mesosphere to the stratosphere is examined, and it is shown that mesospheric processes can influence the distributions of these chemical species in polar regions. For HNO3 we also find that small concentrations of liquid aerosols above 30 km could play a major role in determining the abundance in polar winter at high latitudes. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 12,937-12,951 |
| Journal | Journal of Geophysical Research |
| Volume | 99 |
| Issue number | D6 |
| DOIs | |
| State | Published - 1994 |