On a warm summer day, a large mass of air (atmospheric pressure 1.01*10^5 Pa) is

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On a warm summer day, a large mass of air (atmospheric pressure 1.01*10^5 Pa) is heated by the ground to a temperature of 25.0 C and then begins to rise through the cooler surrounding air. Part A Calculate the temperature of the air mass when it has risen to a level at which atmospheric pressure is only 8.2010^4 Pa . Assume that air is an ideal gas, 1.40 with . (This rate of cooling for dry, rising air, corresponding to roughly 1 C per 100m of altitude, is called the dry adiabatic lapse rate.) please help, WILL RATE On a warm summer day, a large mass of air (atmospheric pressure 1.01*10^5 Pa) is heated by the ground to a temperature of 25.0 C and then begins to rise through the cooler surrounding air. Part A Calculate the temperature of the air mass when it has risen to a level at which atmospheric pressure is only 8.2010^4 Pa . Assume that air is an ideal gas, 1.40 with . (This rate of cooling for dry, rising air, corresponding to roughly 1 C per 100m of altitude, is called the dry adiabatic lapse rate.) please help, WILL RATE Part A Calculate the temperature of the air mass when it has risen to a level at which atmospheric pressure is only 8.2010^4 Pa . Assume that air is an ideal gas, 1.40 with . (This rate of cooling for dry, rising air, corresponding to roughly 1 C per 100m of altitude, is called the dry adiabatic lapse rate.) please help, WILL RATE

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