Abstract
A particular phenomenon observed on an acoustic sounder record is analyzed, and is interpreted as being associated with the passing of a land breeze front. A simple physical explanation of the frontal movements is suggested. The actual existence of the land breeze is demonstrated by examination of conventional meteorological observations.
| Original language | English |
|---|---|
| Journal | Journal of applied meteorology (1988) |
| Volume | 15 |
| Issue number | 6 |
| Pages (from-to) | 662-664 |
| ISSN | 0894-8763 |
| DOIs | |
| Publication status | Published - 1976 |