Calculating Water Level Rise in Low Pressure Zone | Atmospheric Pressure Effect

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SUMMARY

The discussion focuses on calculating the water level rise in a low atmospheric pressure zone, specifically where the pressure is 64 mm-Hg less than the surrounding area. The conversion of this pressure difference to Pascals results in 8505.27 Pa. Using the hydrostatic pressure equation, the calculated water height is 9.47 m; however, the correct answer is 0.85 m, indicating a misunderstanding of the pressure difference application. The key takeaway is that the pressure difference alone determines the water level rise without needing to reference atmospheric pressure.

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Homework Statement



Suppose that a zone of low atmospheric pressure (a "low") is at some place on the surface of the sea. The pressure at the center of the "low" is 64 mm-Hg less than the pressure at a large distance from the center. By how much will this cause the water level to rise at the center?



Homework Equations


p-p0= -p(density)gy



The Attempt at a Solution



First I converted 64 mm-Hg to Pa using 1.01X10^5 Pa/760 mm-Hg and I got 8505.27 Pa

p-p0=-p(density)gy
101325 Pa-8505.27 Pa=1000X9.8Xh
h=92819.73/9800=9.47 m

According to the book, the answer is 0.85 m
 
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qspartan570 said:

Homework Statement



Suppose that a zone of low atmospheric pressure (a "low") is at some place on the surface of the sea. The pressure at the center of the "low" is 64 mm-Hg less than the pressure at a large distance from the center. By how much will this cause the water level to rise at the center?



Homework Equations


p-p0= -p(density)gy



The Attempt at a Solution



First I converted 64 mm-Hg to Pa using 1.01X10^5 Pa/760 mm-Hg and I got 8505.27 Pa

p-p0=-p(density)gy
101325 Pa-8505.27 Pa=1000X9.8Xh
h=92819.73/9800=9.47 m

According to the book, the answer is 0.85 m

The pressure value that you've been given is already a pressure difference, so there's no need to invoke atmospheric pressure. All you need is the height of a column of water (seawater, which has a slightly different density than pure water!) that will produce that pressure at its base.
 

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