This is the view looking northeasterly across Little Clear Lake, Limberlost. The water surface was like a plate glass mirror. It was only rippled when a family of geese swam in front of me on their way to the far shore. Later in the morning the northwesterly wind rippled the surface. Daytime heating is responsible for eroding the radiational inversion and making the atmospheric boundary layer unstable. This allows the air mass circulations from aloft to penetrate to the ground. This cycle happens nearly every day...
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