Lapse rate is the speed at which the lapse of conduction or convection occurs, many lapsings have been submitted by african scientists because they are near the equator where mitosis occurs and the mitochondria of the feline cells are at there most sensitive state of equality. the equation is 7*lapse&temp(deg K)*potate
Temperature lapse rate is the rate at which air temperature decreases with an increase in altitude. The standard lapse rate is around 6.5°C per kilometer, meaning that for every kilometer you ascend in the atmosphere, the temperature decreases by 6.5°C on average. The lapse rate can vary depending on atmospheric conditions, such as humidity and atmospheric stability.
two seconds on Google revealed this: http://www.iupac.org/goldbook/T06266.pdf an extract from this document: "temperature lapse rate (in atmospheric chemistry)The rate of change of temperature with altitude (dT/dz)."
The standard temperature lapse rate is the rate at which we expect air to be colder, the higher we go.
The rate is about 2 Fahrenheit degrees per 1000 feet of altitude, which coincidentally happens to be about 1 Celsius degree per 100 meters.
NOT 2 Fahrenheit degrees per 1000 feet!
2 CENTIGRADE degrees per 1000 feet.
No, in the troposphere, the temperature generally decreases as altitude increases at a rate of about 6.5 degrees Celsius per kilometer. This relationship is known as the environmental lapse rate.
The temperature at 20,000 feet above sea level can vary depending on the specific conditions, but on average, it is around -40°F to -50°F (-40°C to -45°C). This temperature tends to decrease as altitude increases due to the lapse rate, which is the rate at which atmospheric temperature decreases with an increase in altitude.
The temperature typically decreases as you go up through the troposphere. This decrease in temperature with altitude is known as the lapse rate, and is usually around 6.5°C per kilometer of altitude.
It decreases because as you move up in altitude the air becomes thinner making it colder.
On average, the temperature decreases by around 3.5°F for every 1,000 feet increase in elevation, known as the lapse rate. At 8,000 feet altitude, you can expect the temperature to be around 28°F cooler than at ground level, so it would be approximately 42°F at that height if the ground temperature is 70°F.
The rate at which temperature decreases with increasing altitude is known as the lapse rate.
Lapse rate is the rate at which air temperature decreases with existing altitude
The environmental lapse rate (ELR), is the rate of decrease of temperature with altitude in the stationary atmosphere at a given time and location.While Normal Lapse Rate is average concept for temperature decline with height in the troposphere.
The standard temperature lapse rate in the troposphere is approximately 6.5°C per kilometer, or 3.5°F per 1,000 feet. This means that the temperature decreases by this rate as altitude increases within the troposphere.
It doesnt
The moist adiabatic lapse rate is usually lower than the dry adiabatic lapse rate because the presence of water vapor in the air allows for some heat to be released during condensation. The moist adiabatic lapse rate varies depending on the amount of water vapor in the air, while the dry adiabatic lapse rate remains constant at around 9.8°C per kilometer.
Stability prevails when the environmental lapse rate is less than the adiabatic lapse rate. This means that the temperature of the surrounding air decreases at a slower rate with altitude compared to the dry or moist adiabatic lapse rates, resulting in a more stable atmosphere.
The lapse rate is defined as the rate at which atmospheric temperature decreases with increase in altitude. It is strongly influenced by both the heating and cooling of the ground.
Environmental lapse rate
The adiabatic lapse rate refers to the rate at which temperature changes with altitude in a parcel of dry or moist air when there is no exchange of heat with the surroundings. The dry adiabatic lapse rate is approximately 10°C per 1000 meters for dry air, while the moist adiabatic lapse rate varies with humidity but is generally lower due to the release of latent heat during condensation.
As a mass of air rises in the troposphere, its temperature will usually decrease due to adiabatic expansion. This is known as the lapse rate. The rate at which the temperature decreases with height is known as the environmental lapse rate, which is typically around 6.5°C per kilometer.
That statement describes the environmental lapse rate of saturated air, also known as the moist adiabatic lapse rate. This rate signifies how quickly the temperature of saturated air changes as it ascends or descends through the atmosphere under adiabatic conditions. The specific value of 0.6 degrees Celsius per 100 meters is a typical approximation for the moist adiabatic lapse rate.