This produces a sea breeze in late morning that abates in the afternoon or evening.
Generally the eastern side of the range has more vegetation than the eastern owing to the influence of the sea breeze.
If an offshore wind of 8 kn exists, the sea breeze is not likely to develop.
The strength of the sea breeze is directly proportional to the temperature difference between the land mass and the sea.
This energy comes from fronts, heating, moistening, or mesoscale convergence boundaries such as outflow and sea breeze boundaries, or orographic lift.
Due to the typical sea breeze, takeoffs and landings are typically done east-bound.
It was stirred by a sea breeze which began at about 10:00 from the west or northwest, which continued blowing until dark.
There is often a sea breeze on the coast, which combined with tides contributes to quick temperature changes over a single day.
