![]() Many of the meteorological phenomena that are associated with the coast are a consequence of synoptic-scale forcing. Interactions with large scale meteorological systems A similar structure can occur when the incident flow is not uniform, such as in the vicinity of a storm. The best examples of the phenomenon are found associated with cold air damming between a coastal front and mountain ridges. The topographically induced pressure fields produce along-ridge pressure gradients that can result in alongshore barrier jets. The steady-state response is a pressure ridge, a phenomenon referred to as damming.
0 Comments
Leave a Reply. |
Details
AuthorWrite something about yourself. No need to be fancy, just an overview. ArchivesCategories |