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I remember studying that air pressure and temperature are inversely proportional. Now I saw in book that "Atmospheric pressure decreases as we go higher and higher." But in height the temperature is less, and so the air pressure is high. But it is given atmospheric pressure increases with altitude. I googled and understood that air pressure and atmospheric pressure are different. But I can't understand how each is different from the other in properties.``

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"Atmospheric pressure increases as we go higher and higher." Uh oh . –  Dimensio1n0 Aug 14 '13 at 12:40
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Atmospheric pressure decreases, not increases, with altitude –  John Rennie Aug 14 '13 at 13:20
    
hang on everyone, why are we not commenting on the "inversely proportional" part? PV=nRT, all other things the same, air pressure and temperature are proportional, not inversely. –  Jim Aug 20 '13 at 18:47
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closed as unclear what you're asking by Dilaton, akhmeteli, Waffle's Crazy Peanut, Jim, BebopButUnsteady Aug 20 '13 at 22:22

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Air pressure is the intrinsic pressure in a quantity of air. It can come from any number of sources. Perhaps there is a closed cylinder of air with a piston compressing it isothermally. Or perhaps the air in the tire in your car is under pressure due to the weight of the car and the surface tension of the tire.

Atmospheric pressure is air pressure due solely to the weight of the air above you in the atmosphere. It is typically around $10^5\ \mathrm{N/m^2}$ on Earth, but can vary with altitude and weather. It is just a "natural," ubiquitous special case of air pressure in physical situations taking place inside an atmosphere.

Note that this is a very subtle distinction, and interchanging the terms "air pressure" and "atmospheric pressure" should cause absolutely no confusion in practice.

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If you simply go outside and hold in your hand something of standard area, like a coin, atmospheric pressure is nothing but the weight of all the air above that coin, in a very slender cylinder, going from the coin up to outer space. Of course, since some of the air can sneak in under it and push up, you don't feel that weight.

Temperature of air is like temperature of anything. If you heat it, it gets hotter, and if you cool it, it gets colder. Air gets heated because the sun shines on the ground, making it hot, which raises the temperature of the air.

Another way to make air hot is to squeeze it. Like if you take a bicycle tire pump and squeeze some air with it (increasing its pressure), you should notice the pump gets warm. The opposite happens too. If you let it expand, it gets cooler, but those only happen because the air in the pump is sort of insulated from the outside air. (There's a big word for that - "adiabatic".)

Now in real outside air, the air doesn't stay still. Some of it moves up, and some moves down. The air that moves up goes to a place of lower pressure because there's less air above it, so it expands and gets cooler. Likewise descending air gets warmer, for the same adiabatic reason. So, for example, the air is much warmer at the bottom of the Grand Canyon than at the top.

Put all these together and you'll start to understand how weather works.

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Your answer explains about atmospheric pressure, but it doesn't tell me anything about air pressure. Please make some edits and let me be out of misery –  Govind Balaji Aug 15 '13 at 10:02
    
@govindo: You don't need to make that distinction, between air and atmospheric pressure. Air, like any fluid, has pressure. –  Mike Dunlavey Aug 15 '13 at 10:51
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