Abstract
Sensitivities are presented as gradient fields. Some characteristics of the sensitivity fields have simple dynamical explanations, such as their strong dependence on winds, and do not require an adjoint model to reveal them. Other characteristics would be difficult to ascertain without an adjoint model, although they, too, in retrospect, have simple dynamical explanations. Still others, although equally important and undoubtedly dependent on the dynamics, would be practically impossible to determine without an adjoint. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 539-557 |
| Number of pages | 19 |
| Journal | Tellus, Series A: Dynamic Meteorology and Oceanography |
| Volume | 45 A |
| Issue number | 5 |
| State | Published - 1993 |
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