23.3°F
The Troposphere is 3.5 degrees f per thousand feet and 6.5 degrees s per kilometer.
Every 10 meters, the pressure will increase by one atmosphere. That is about 33 feet.
8,000 feet into the atmosphere
223mb. This is based on the assumption that every 5.6km is half the pressure of the original value. Keep in mind that below 16km is 90% of the atmosphere.
Alto
thousand standard cubic feet
On a standard day, the temperature at 40,000 feet is approximately -69.7F.
The formula is: Normal Cubic Feet = SCF * [T / (273 + 15.6)] * [ 14.73 / P] SCF = Standard Cubic Feet T = Temperature in kelvin P = Pressure in psi (absolute pressure, where 1 atmosphere = 14.73)
342,061 feet.
M stands for a thousand. and CF - cubic feet. MCF - thousand cubic feet, thus MMCF - thousand of thousand cubic feet which is just million cubic feet
As you gain altitude in the troposphere, the layer of atmosphere closest to the ground and extending about 8 miles up, the temperature will decrease by 1 degree Fahrenheit for every 200 feet.
The Troposphere is 3.5 degrees f per thousand feet and 6.5 degrees s per kilometer.
None. The milipede has a lot of feet, but not one thousand.
CO levels are not measured in feet and so you will not find such standard feet anywhere.CO levels are not measured in feet and so you will not find such standard feet anywhere.CO levels are not measured in feet and so you will not find such standard feet anywhere.CO levels are not measured in feet and so you will not find such standard feet anywhere.
scfh is "standard cubic feet per hour" and cfh doesn't neccessarily mean "standard". Standard conditions are stanard temperature (293 K), and standard pressure (1 atm, 101,300 Pa).
1 atmosphere is 33.9 feet of water.
The troposphere, the lowest layer of Earth's atmosphere, is heated from below. The troposphere is warmest at the bottom near Earth's surface. The troposphere is coldest at its top, where it meets up with the layer above (the stratosphere) at a boundary region called the tropopause. Temperatures drop as you move upward through the troposphere.Sunlight streams down from space through the atmosphere, striking the ground or ocean beneath. The sunlight heats the surface, and that surface radiates the heat into the adjacent atmosphere. Atmospheric scientists use a concept called a "standard atmosphere" to represent an average atmosphere with variations caused by weather, latitude, season, and so forth, removed. In the standard atmosphere model, the temperature at sea level at the bottom of the troposphere is 15° C (59° F). Higher up in the troposphere, where less heat from the surface warms the air, the temperature drops. Typically, the temperature drops about 6.5° C with each increase in altitude of 1 kilometer (about 3.6° F per 1,000 feet). The rate at which the temperature changes with altitude is called the "lapse rate". In the standard atmosphere, by the time you reach the top of the troposphere the temperature has fallen to a chilly -57° C (-70° F).Of course, the atmosphere is always changing and is never "standard". Temperatures in the troposphere, both at the surface and at various altitudes, do vary based on latitude, season, time of day or night, regional weather conditions, and so on. In some circumstances, the temperature at the top of the troposphere can be as low as -80° C (-110° F). When a weather phenomenon called at "temperature inversion" occurs, temperature in some part of the troposphere gets warmer with increasing altitude, contrary to the normal situation.In the layer above the troposphere, the stratosphere, temperature rises with increasing altitude. In the stratosphere, the air is heated from above by ultraviolet "light" which is absorbed by ozone molecules in the air. The tropopause is the boundary between the troposphere (below) and the stratosphere (above). The tropopause occurs where the temperature stops dropping with increasing altitude (in the troposphere) and begins climbing with increasing altitude (the stratosphere).