Abstract
The results of two simple multilevel numerical experiments for the deep ocean circulation are decomposed into vertical modes, and a comparison is made between the decomposed flow fields and the results of corresponding reduced-gravity models. -from Authors
| Original language | English |
|---|---|
| Journal | Journal of Geophysical Research |
| Volume | 100 |
| Issue number | C6 |
| Publication status | Published - 1995 |
All Science Journal Classification (ASJC) codes
- Geophysics
- Oceanography
- Forestry
- Ecology
- Aquatic Science
- Water Science and Technology
- Soil Science
- Geochemistry and Petrology
- Earth-Surface Processes
- Atmospheric Science
- Earth and Planetary Sciences (miscellaneous)
- Space and Planetary Science
- Palaeontology