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Jutro sa maglom na obali reke.


Pogled na obalu reke u jutru sa maglom.
Jutros sam sa mojim unukom presao preko mosta i sisao na drugu obalu Morave, gde je zavladala magla.
Magla predstavlja kondenzovanu vodenu paru u atmosferi pri povrsini troposfere. Po svom sastavu se ne razlikuje od oblaka, jedina razlika izmedju oblaka i magle je po mestu gde se javljaju.
Rano jutros temperatura je bila 0 C stepen.
Na drugoj obali reke nije bilo ljudi, vladala je tisina.


Morning with fog on the river bank.


View of the river bank in the morning with fog.
This morning, I crossed the bridge with my grandson and went to the other bank of the Morava, where the fog prevailed.
Fog is condensed water vapor in the atmosphere at the surface of the troposphere. It does not differ from clouds in its composition, the only difference between clouds and fog is where they appear.
Early this morning the temperature was 0 C degree.
There were no people on the other side of the river, there was silence.

ikeharel, NickVu, jemaflor, Fis2, jhm, PaulVDV, ChrisJ, mcmtanyel has marked this note useful

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Additional Photos by Pavle Randjelovic (pajaran) Gold Star Critiquer/Gold Star Workshop Editor/Gold Note Writer [C: 13107 W: 2912 N: 26815] (110797)
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