G Bronson Posted July 27, 2013 Posted July 27, 2013 Hey, So I'm doing this research/internship deal -- long story short I told the professor my knowlege of Atmospheric Science was very limited. I have to devise a study to test a hypothesis (or three), but am having a very hard time finding a testable hypothesis. I purchased an atmospheric science textbook (which I would need for next year), and all I have come up with is the following: ****** pressure= temperature X density X constantair pressure ~ temperature X densityThis expression says that the pressure of thegas is proportional to its density, as long as itstemperature does not change.This daily (diurnal)fluctuation of pressure appears to be due primarily tothe absorption of solar energy by ozone in the upper atmosphereand by water vapor in the lower atmosphere. Thewarming and cooling of the air creates density oscillationsknown as thermal (or atmospheric) tides that show upsmall pressure changes near the earth’s surface.usually indicates clearing weather or fairweather, whereas a steady drop in atmospheric pressure (afalling barometer) often signals the approach of a storm withinclement weather. **** I'm having a hard time turning anything into a testable hypothesis. The prof said I could use either a pressure sensor or a temperature gauge (thermal camera), though I haven't asked if I could use both or could use some other sort of input such as NOAA data. He gave me the example of a former student who was using a CO2 gauge, with the hypothesis that CO2 levels around leaves of trees would be lower during the day because of photosynthesis. If anyone can help me, or point me in the right direction I'd really appreciate it. Thanks.
vampares Posted August 11, 2013 Posted August 11, 2013 (edited) The pressure is also affected by changes in volume or vice versa. PV=nRT n is the molar amount of substance and R is the gas law constant, these might be ignored. The cause of atmospheric pressure is the force of gravity upon the the mass of air on earth. Being an open system, high pressure atmosphere will be inclined to move into the region of a lower pressure region until the pressure is equalized. Air will move more quickly at higher altitudes because it is less dense and experiences less friction. It is less dense because it occupies more volume because of the change in gravitational pressure. . . . Anyways, atmospheric pressure changes are usually a dynamic of precipitation. When water condenses to a liquid form it must release the thermal energy which allow it to become gaseous. This thermal energy will increase pressure and thereby the volume. The volumetric change will make the air less dense. It will rise. But looking at that gaseous water from the other direction you might think of it as being cold thereby dense. So it would have more pressure. It won't stay like that forever. Fast barometric changes are indications of convective storms. Hurricanes have low barometric pressure in the center. This sucks air inward. The atmosphere is also likely affected by the tidal forces of lunar gravity. I'm not sure how much difference this makes but I've had difficult time pinning down one barometric reading from another. There are many factors involved. Annotated are easier to read. Meteorologists use tools like hodographs. Edited August 11, 2013 by vampares
b1a2s3a4l5t6e7 Posted November 1, 2013 Posted November 1, 2013 It is very important to know our atmosphere, not only for weather, climate research and telecommunications , but also for geophysicist that study earthquake, by example, before a major earthquake the air becomes ionized, but storms and auroras also contributes to the ionized air and i hope that in the future wil be better understood and taught to the general public.
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