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In rising from the bottom of a lake - to the top - thetemperature of an air bubble remains unchanged - but itsdiameter gets doubledIf h is the barometric height(expressed in m of mercury of relative density ρ) at thesurface of the lake - the depth of the lake is [1994]

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In rising from the bottom of a lake - to the top - thetemperature of an air bubble remains unchanged - but itsdiameter gets doubledIf h is the barometric height(expressed in m of mercury of relative density ρ) at thesurface of the lake - the depth of the lake is [1994]






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