Adiabatic Wind Descending Homework Problem

AI Thread Summary
The discussion revolves around a homework problem involving adiabatic wind descent affecting temperature in Denver. The scenario describes air descending from Grays Peak to Denver, with specific initial pressure and temperature values. The key equation mentioned is PV^gamma=constant, which relates pressure and volume in an adiabatic process. Participants are seeking guidance on how to derive a pressure-temperature relationship from this equation. The focus is on understanding the transformation needed to calculate the temperature rise in Denver due to the chinook wind.
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Hi everybody, this is my first post on your forum and i hope someone can help me :)

the problem is i can figure out how to approuch this problem :s i do know that the process of the air descending is adiabatic but still i can't get it :(

thanks for your help guys in advance.

Homework Statement



Suppose a strong wind is blowing toward Denver (elevation 1630 m) from Grays Peak (80 km) west of Denver, at an elevation of 4350 m), where the air pressure is 5.65×104 Pa and the air temperature is -16.0°C . The temperature and pressure in Denver before the wind arrives are 2.0 °C and 8.12×10^4 Pa. By how many Celsius degrees will the temperature in Denver rise when the chinook arrives?
 
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Yes, the descent of the air is adiabatic. There's an equation that describes what happens in an adiabatic process; it's PV^gamma=constant. Do you know how to transform this into a pressure-temperature relationship?
 
Hi ! thanks for your reply, as PV^gamma=constant i think we can say that p_1*v_1^gamma=p_2*v_2^gamma, but how to involve pressure in it ?

thanks :)
 
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