The homework problem to end all homework problems.
Physics Stack Exchange is a question and answer site for active researchers, academics and students of physics.. standard temperature, temperature lapse rate and height, and I know the values on earth are as. using the barometric equation is a good start after assumptions. The barometric equation and its thermodynamic variables are.
The assumption of constant gravity is not crucial in solving Equation (3), that is, the variation of gravity with altitude and latitude can be safely ignored for short-distance trips ().Moreover, it is known that temperature tends to change with altitude. The lapse rate is defined as the rate of temperature increase in the atmosphere with the altitude: a constant lapse rate L can be assumed.
See also: Barometric formula There are two different equations for computing pressure at various height regimes below 86 km (or 278,400 ft). Equation 1 is used when the value of standard temperature lapse rate is not equal to zero and equation 2 is used when standard temperature lapse rate equals zero.
For these equations, , and correspond to the altitude, pressure, and temperature at the bottom of the stratosphere. The pressure at the bottom of the layer is determined from the user provided inputs of the pressure and temperature at sea level knowing that the altitude at the bottom of the layer is 11 km; assuming the default pressure was used at sea level, the pressure at the bottom of the.
Keywords: Action, adiabatic lapse rate, entropy, barometric formula, climate change Introduction The main hypothesis advanced in this paper is that algorithms developed from the physical property of action with Clausius’ virial theorem can enable plots of the atmosphere’s dynamic morphology.
Atmospheric pressure is defined as the force per unit area exerted against a surface by the weight of air above that surface at any given point in the Earth's atmosphere.In most circumstances atmospheric pressure is closely approximated by the hydrostatic pressure caused by the weight of air above the measurement point. Low pressure areas have less atmospheric mass above their location.
The discrimination is due to the problematic assumptions (assuming a standard lapse rate) associated with reduction of sea level from high elevations. (7) The Dead Sea, the lowest place on Earth at 430 metres (1,410 ft) below sea level, has a correspondingly high typical atmospheric pressure of 1065 hPa.