It is a measure of the change in temperature (in degrees Celsius) per kilometre.
Not quite sure where it could be used: temperature gradients are too variable going up into the atmosphere or down ocean depths. Things like inversion layers would play havoc with any such measure.
On the other hand, it could not be used for distance from the equator because there will be too many local factors in play.
Multiply litres per km by 2.35 to get miles per gallon.
You are traveling at 1,280 km per hour.
7.4 km per hour equates to 4.6 miles per hour.
Speed is NOT measured in km but km PER HOUR. The average speed was 88.88 (repeating) km per hour.
41 km per hour = 25.47 mph
You would be in the troposphere, the lowest layer of the Earth's atmosphere where temperature decreases with altitude at an average rate of 6.5 degrees Celsius per kilometer.
The temperature decreases by about 6.5 degrees Celsius per kilometer in the troposphere, so the total temperature change between 3 km and 7 km above the Earth's surface would be approximately 26 degrees Celsius.
The temperature at 3.4 km below the Earth's surface generally increases with depth due to geothermal heating. On average, the geothermal gradient is about 25-30 degrees Celsius per kilometer, so at 3.4 km below the surface, the temperature could be around 85-102 degrees Celsius.
Distance is measured in linear units like kilometers, while temperature is measured in degrees Celsius. Therefore, 10 km does not equate to a temperature in degrees Celsius.
below the surface of the earth, as we move deeper towards the core (HEAT's CAUSE) the temperature rises. this rise of temperature with depth is referred to as the geothermal gradient. in most parts of the world that are away from the plate boundaries, with every km depth an increase of 22 degrees Celsius in temperature is observed. Different areas show different geothermal gradients. in many parts of the world its as high as 30 degrees Celsius per Km and in some its as low as 15 degrees Celsius per Km.
below the surface of the earth, as we move deeper towards the core (HEAT's CAUSE) the temperature rises. this rise of temperature with depth is referred to as the geothermal gradient. in most parts of the world that are away from the plate boundaries, with every km depth an increase of 22 degrees Celsius in temperature is observed. Different areas show different geothermal gradients. in many parts of the world its as high as 30 degrees Celsius per Km and in some its as low as 15 degrees Celsius per Km.
142 (km per minute) = 8,520 km/h142 (km per minute) = 5,294.08 mph
Assuming temperature decreases at a standard lapse rate of about 6.5°C per kilometer, the temperature of the air at 500 meters would be approximately 23 degrees Celsius - (0.5 km * 6.5°C/km) = 20.25 degrees Celsius.
1.5km per seconds
5 km per second is equivalent to 18,000 km per hour. This is very fast, nearly 11,185 miles per hour. For context, the speed of sound is around 1,225 km per hour.
there is 3280.8399 ft per km
1000 meters per km