maylisbethsgeografi blogspot.com

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Mandag 20. desember 2010. Når varmluftsballongen inneholder kald luft, har molekylene veldig lite energi. Dette gjør at ballonger ikke stiger og har veldig liten bevegelse. Når luften inne i ballongen blir varm får molekylene mye mer energi, og de beveger seg fra side til side. Dette gjør at den. Utvider seg, og stiger. Lavtrykk er der luften stiger pga at bakkenvannet er varm, Dette danner skyer og kan også danne regn pga fuktighet i. Send dette via e-post. Mandag 6. desember 2010. Vis RAS I NORGE.
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Mandag 20. desember 2010. Når varmluftsballongen inneholder kald luft, har molekylene veldig lite energi. Dette gjør at ballonger ikke stiger og har veldig liten bevegelse. Når luften inne i ballongen blir varm får molekylene mye mer energi, og de beveger seg fra side til side. Dette gjør at den. Utvider seg, og stiger. Lavtrykk er der luften stiger pga at bakkenvannet er varm, Dette danner skyer og kan også danne regn pga fuktighet i. Send dette via e-post. Mandag 6. desember 2010. Vis RAS I NORGE.

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This web page maylisbethsgeografi.blogspot.com states the following, "Når varmluftsballongen inneholder kald luft, har molekylene veldig lite energi." We saw that the webpage said " Dette gjør at ballonger ikke stiger og har veldig liten bevegelse." It also said " Når luften inne i ballongen blir varm får molekylene mye mer energi, og de beveger seg fra side til side. Utvider seg, og stiger. Lavtrykk er der luften stiger pga at bakkenvannet er varm, Dette danner skyer og kan også danne regn pga fuktighet i."

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