The specific heat capacity of air is approximately 1.01 kJ/kg°C. The density of air at room temperature is around 1.225 kg/m³. Assuming the same temperature and pressure, 1 cubic foot of air would weigh approximately 0.0413 kg. Therefore, it would require around 0.0413 kJ to heat up 1 cubic foot of air by 1 degree Celsius.
As a digital assistant, I do not have a physical form or the ability to measure temperature at my "feet." My purpose is to provide information and assistance to the best of my abilities.
At the top of Mount Everest, where the atmospheric pressure is lower, water boils at around 160 degrees Fahrenheit (71 degrees Celsius) instead of the standard 212 degrees Fahrenheit (100 degrees Celsius) at sea level.
This depends on the air temperature (since Air is a gas). You can dynamically find the results, though, by using this online calculator; http://hyperphysics.phy-astr.gsu.edu/hbase/sound/souspe.html
The cost of one degree change in heat can vary widely depending on factors like the size of the space being heated, the type of heating system, and energy prices. It is best to consult with a heating professional or energy provider to get an accurate estimate for your specific situation.
-4.83 Celsius
The temperature typically decreases by about 2 degrees Fahrenheit for every 1,000 feet in altitude gained in the troposphere (the lowest atmospheric layer where weather occurs). So, at 26,000 feet, the temperature could be around 52 degrees Fahrenheit colder than at ground level.
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.
degree is the unit of either temperature or angle. But feet is the unit of length. So no relation between these two
On a standard day, the temperature at 40,000 feet is approximately -69.7F.
Water typically freezes at 32 degrees Fahrenheit (0 degrees Celsius) at sea level. As altitude increases, the boiling point of water decreases by about 1 degree Fahrenheit for every 500 feet gain in altitude. Therefore, at 2500 feet, water is likely to freeze at a slightly lower temperature than 32 degrees Fahrenheit.
The standard atmosphere temperature at 10,000 feet altitude is approximately 23.4 degrees Fahrenheit or -4.8 degrees Celsius.
On average, the temperature decreases by about 3.5°F for every 1,000 feet increase in elevation. This concept is known as the environmental lapse rate. However, the actual rate at which temperature decreases with elevation can vary based on local conditions and geographic location.
There is no way to measure the temperature at the Earth's core directly. We know from mines and drill holes that, near the surface of the Earth, the temperature increases by about 1 degree Fahrenheit for every 60 feet in depth. If this temperature increase continued to the center of the Earth, the Earth's core would be 100,000 degrees Celsius! But nobody believes the Earth is that hot; the temperature increase must slow down with depth and the core is probably about 3000 to 5000 degrees Celsius.
Water boils at a lower temperature on a hill due to decreased atmospheric pressure at higher altitudes. For every 500 feet increase in elevation, the boiling point of water decreases by about 1 degree Fahrenheit.
Air pressure and temperature do not change in the same way with altitude. As altitude increases, air pressure decreases because there is less air mass above pushing down. This leads to a decrease in temperature with altitude at a rate of about 2 degrees Celsius per 1,000 feet due to the decrease in pressure causing the air to expand and cool.
At 90,000 feet in altitude, the temperature is approximately -94 degrees Fahrenheit (-70 degrees Celsius). This high up in the atmosphere, temperatures are extremely cold due to the thin air and lack of insulation.