Formulas for atmospheric pressure variation with altitude. Scroll down to related links and look at "Atmospheric pressure - Wikipedia".
320,000 ft above sea leavel
Because of the pressure in the higher atmosphere is much lower than the pressure where it was filled. This causes the pressure inside to expand the balloon up to and past the bursting point. Most likely the tip of the troposphere.
Pressure decreases as height increases and vice-versa.
describe how the height of the tides changes from monday to thursday
The Earth's atmosphere declines with altitude.
Formulas for atmospheric pressure variation with altitude. Scroll down to related links and look at "Atmospheric pressure - Wikipedia".
The standard sea level pressure of Earth's atmosphere - a pressure of 1 Bar or one "atmosphere".
Generally, atmospheric pressure is greatest at ground level, because you are at the bottom of the 25 mile thick atmosphere of earth. Greatest water pressure in a swimming pool is at the bottom, too. As you go up into the atmosphere, the pressure tends to decrease.
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Force over Area= Pressure
For the same reason. The liquid above the location considered, or the atmosphere above the position considered, helps contribute to the pressure; if there is more liquid or atmosphere above, there is more pressure.
Pressure is given by the formula -pgh , where p= desity of water , g gravity ,and h height . So pressure at the depth 3.5m =1*9.8*3.5 pa =34.3 pa. (Assuming density of water to be 1).
the shape and height causes it to vary with temperature,pressure,and the amount of water vapor in the atmosphere
320,000 ft above sea leavel
Pressure always decreases with height. This is because atmospheric pressure is just a measure of how much air is weighing down. So the higher you go in the atmosphere, the less air is above you (more of it is below you) and the lower the pressure will be.
Because of the pressure in the higher atmosphere is much lower than the pressure where it was filled. This causes the pressure inside to expand the balloon up to and past the bursting point. Most likely the tip of the troposphere.
The formula relating the pressure in a liquid to the depth of the liquid is P = P0 + dgh. P is the pressure, P0 is atmospheric pressure, d is the density of the fluid, g is the acceleration of gravity, and h is height below the surface of the water.