When temperatures rise, so does the air, pulling cool, moist
marine air inland onto the beaches like a foggy blanket.
Not exact matches
Frequently, particularly during the «May gray / June gloom» period, a thick «
marine layer» cloud cover keeps the
air cool and damp within a few miles of the coast, but yields to bright cloudless sunshine approximately 5 — 10 miles (8.0 — 16.1 km)
inland.
A sea breeze, which is caused by the temperature and pressure difference between warm areas
inland and the cool
air over the ocean, often develops on warm summer days as well, increasing the on - shore flow pattern and maintaining a constant flow of
marine stratus clouds onto the coastal areas.