Calculate the magnitude of the net force

AI Thread Summary
To calculate the net force on an air parcel of mass 1.0x10-3kg at 4.0km altitude with a temperature of 250K, one must first understand the lapse rate, which is the decrease in temperature with altitude, set at 6.5K/km. The atmospheric pressure at this altitude can be determined using the standard atmospheric model, starting from the surface pressure of 1 atm. By calculating the density of the surrounding air at 4 km and comparing it to the density of the air parcel, the net buoyant force can be derived. This buoyant force is the key to determining the net force acting on the air parcel. Understanding these concepts is essential for solving the problem accurately.
ninaw21
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Homework Statement


Calculate the magnitude of the net force on an air parcel of mass 1.0x10-3kg which is at a temperature 250K and which is in the US standard atmosphere at an altitude of 4.0km. Take the lapse rate as 6.5K/km and the surface temperature as 288K

Homework Equations


Force = Mass x Acceleration
Acceleration = Speed / Time


The Attempt at a Solution


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ninaw21 said:

Homework Statement


Calculate the magnitude of the net force on an air parcel of mass 1.0x10-3kg which is at a temperature 250K and which is in the US standard atmosphere at an altitude of 4.0km. Take the lapse rate as 6.5K/km and the surface temperature as 288K

Homework Equations


Force = Mass x Acceleration
Acceleration = Speed / Time


The Attempt at a Solution


?

Can you say more about this problem? What is a "lapse rate"? The net force on the package from what?
 
berkeman said:
Can you say more about this problem? What is a "lapse rate"? The net force on the package from what?
The lapse rate is the rate of decrease of atmospheric temperature with altitude. In this problem, the temperature of the air parcel is different from the temperature of the surrounding atmospheric air, since the parcel has not yet equilibrated. First, you calculate the pressure of the atmospheric air at 4 km, knowing that the pressure at the surface is 1 atm., and assuming that the atmospheric air column is in static equilibrium (and knowing how the temperature, and thus the density, vary with altitude). Once you know the atmospheric pressure, you can get the density at 4 km, and compare it with the density of the air parcel at the same ambient pressure, and at the temperature of the parcel. From this, you can get the net buoyant force on the parcel.
 
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