What coastal weather phenomenon explains a sea breeze?

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Sea breeze is produced by differential heating between land and sea, leading to onshore winds during the day. The land heats up faster than the adjacent sea, causing air over the land to rise and create lower pressure near the coast. Cooler air over the sea moves toward the land to replace the rising air, generating a steady breeze from sea to land along the coast. This daytime onshore flow is the essence of a sea breeze. The other scenarios describe different phenomena: offshore winds from cooler land temperatures occur mainly when the land is cooler than the sea, typically at night (land breeze); tidal currents and storm systems are unrelated to the everyday sea breeze.