Abstract
Two primary characteristics of the precipitation have been found. First, the major rainfall events were linked components. Deep convection was primarily prefrontal or frontal, while the stratiform precipitation was postfrontal, presumably in association with overrunning and orographic lifting. Second, there was a pronounced diurnal variability in the rainfall. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 2540-2557 |
| Number of pages | 18 |
| Journal | Monthly Weather Review |
| Volume | 119 |
| Issue number | 11 |
| DOIs | |
| State | Published - 1991 |