It is known that density p of air decreases with height y as rho=rho₀e-y/y₀, where rho₀ = 1.25 kg³ is the density at sea level, and go is a constant. This density variation is called the law of atmospheres. Obtain this law assuming that the temperature of atmosphere remains a constant (isothermal conditions). Also assume that the value of g remains constant.
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yu077gt676is56cy
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8t yr bifms lgtjt yhg
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