Abstract
The volume-weighted mean concentrations of most species were found to be about a factor of 5 lower during the wet season compared with previous results from the dry season. Only sodium, potassium, and chloride showed similar concentrations in both seasons. When the seasonal difference in rainfall amount is taken into consideration, the deposition fluxes are only slightly lower for most species during the wet season than during the dry season, again with the exception of chloride, potassium, and sodium. Sodium and chloride are present in the same ratio as in sea salt; rapid advection of air masses of marine origin to the central Amazon Basin during the wet season may be responsible for the observed higher deposition flux of these species. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 16,987-16,999 |
| Journal | Journal of Geophysical Research |
| Volume | 95 |
| Issue number | D10 |
| DOIs | |
| Publication status | Published - 1990 |
| Externally published | Yes |