Land Breezes
At night, the land cools off faster than the ocean due to differences in their heat capacity, which forces the dying of the daytime sea breeze. If the land cools below that of the adjacent sea surface temperature, the pressure over the water will be lower than that of the land, setting up a land breeze as long as the environmental surface wind pattern is not strong enough to oppose it. If there is sufficient moisture and instability available, the land breeze can cause showers or even thunderstorms, over the water. Overnight thunderstorm development offshore due to the land breeze can be a good predictor for the activity on land the following day, as long as there are no expected changes to the weather pattern over the following 12–24 hours. This is mainly because the strength of the land breeze is weaker than the sea breeze. The land breeze will die once the land warms up again the next morning.
Read more about this topic: Sea Breeze
Famous quotes containing the words land and/or breezes:
“The great fact in life, the always possible escape from dullness, was the lake. The sun rose out of it, the day began there; it was like an open door that nobody could shut. The land and all its dreariness could never close in on you. You had only to look at the lake, and you knew you would soon be free.”
—Willa Cather (1873–1947)
“Willows whiten, aspens quiver,
Little breezes dusk and shiver.”
—Alfred Tennyson (1809–1892)