how doI calculate temperature change of a rising air mass?
554161
As answer 4 implies, it defies simple description and modeling, since the lapse rate (rate of change of temperature with altitude) depends on air humidity, and of course that can vary. Up to about 11 KM altitude you can approximate the lapse rate as 6.5 C per km (ref. 1), but that applies to an "international standard atmosphere" which may not exist in your application.\nLooking at the diagrams at the bottom of the page in ref. 2, you can see how a typical real-world weather situation (warm water-laden air blowing onto the shore and passing over a mountain) has a more complex temperature profile.
501191
There is a formula...but this is much easier\n\nhttp://www.onlineconversion.com/temperature.htm
1136431
Should be simple.  Warm air rises because it is less dense than cool air.  Cool air rushes in to replace the rising warm air.\n\nPlug this simple formula into the complex real world of spinning globe, equitorial heat and polar regions & you get weather.
956325
false - temperature is a measure of heat
576652
I hope this would help you:\n\nLow Temperature:     -270° F (-170° C)\nAverage Temperature: -185° C \nHigh Temperature: 700°F (350°C)
782736
If ideal gas law is obeyed...\n\ndensity = mass/V == n/V\n\nPV = nRT\nP = (n/V)RT\n\nIf temp is held constant then increasing density increases pressure.
769934
It's the actual temperature with humidity, wind chill factor (if applicable), dew point and other conditions taken into consideration. There's actually a mathematical equation to figure it out but it may be hard to find since the calculations are done by computers these days.
264700
There are many properties but the two most important are:\n\n1. Temperature (cold or warm air mass) - this affects the density of the air mass as well as it's relative humidity, dew point, how it interacts with other air masses of different temperatures, etc. Temperature is the main driver for what types of weather systems will be generated within an air mass.\n\n2. Absolute humidity - the actual water content of the air mass all attributes to the types of weather systems it will generate, and where highs and lows will form.\n\nAlso, air masses can be moving or stagnant, stable or unstable, constant or dynamic, and I'm probably forgetting others.
266705
for every 167 meter increase in the first layer of the atmosphere there is one degree Celsius decrease in temperature.If you get the temperature of the gas,in this case atmosphere, you can calculate the pressure by using the ideal gas law equation.
921703
Just let the units tell you what to do.  H=mass* T*sp heat.  with T in K
149054
In air, higher temperatures result in faster sound waves.  The formula is \n\nV = Vo SQRT( 1 + T/273) , where V = speed of sound in the air, T = temperature in degrees Celsius, and Vo= speed of sound at 0 degrees Celsius = 331 m/s.
471029
They know where air masses originate & how cold those air masses are when they start at their source region.\n\nAs the air mass moves across the continent, it changes in temp to that closer in temp to the air mass already in place.\n\nFor instance, if an air mass orginates over nothern Canada, it will be dry & cold. As it moves south, it will start taking on characteristics of the areas that it moves over. It will get warmer. By the time it reaches say, Mexico, it will have warmed up tremendously.\n\nThey can predict how much kinetic energy will be gained or lost by that.\n\nI don't think there is an exact formula for this kind of science. Most of predicting the weather is actually "predicting"!\n\n;)
100101
Use a calculator, add all three together (be sure to include the negatives) and then multiply by the number of temperatures.
722101
Surface Temperature = 5500ºC\n\nCore Temperature = about 15,000,000ºC
1098555
As the temperature rises, the any object dilates, increases its volume. Gases dilates the more for a certain temperature variation. As volume of a certain mass of gas increases, the density decreases. The different temperature and density air masses can move and change their position (= convection), hot and less dense air is rising, while cold and dense air is coming down, forming streams of air (or water). As long as the difference in the temperature / density between the two regions exist, the convection remains. All the winds, seaside breezes, streams in the oceans are streams of air / water formed by convection, where the different temperature and density air  / water moves. Ex. seaside breeze: because the sea water heats up slower than the ground, the warmer air above the ground rises during the day and in its place comes a cooler air from above the sea. In the evening, when the ground starts to cool down, the breeze changes its direction towards the sea. The same for the Golf stream, which is a warm water stream towards the north coming from the warm tropical region, and heating up the cooler region of north - western Europe.
856026
Use the gas law\nPV=nRT
1008978
well this is really a chemistry problem but the formula is q=mC(delta) T, meaning heat= mass times the specific heat capacity times the change in temperature, so to set this up we use, 1.68^10 j = m (4.18 j/g) (80 degrees) becuase 4.18 is C and 80 degrees is the amount u wish to raise it, so then u get 1.68^10 j = 334.4m, divide both sides by 334.4 and you get .53558=m so your mass is .536g of water