The lapse rate is the rate of decrease of temperature with height. It is most commonly expressed in units of °C per kilometer (or 100 m). The lapse rate is an important aspect of atmospheric stability and weather forecasting.

There are a variety of ways to calculate the lapse rate. The most common is to use the difference in temperature between two levels in the atmosphere such as the temperature at the surface and the temperature at a higher altitude. This can be expressed as:

Lapse Rate (°C/km) = (Temperature at Higher Altitude – Temperature at Lower Altitude) / Height Difference

For example if the temperature at the surface is 20°C and the temperature at 3 km above the surface is 10°C the lapse rate would be:

Lapse Rate (°C/km) = (10°C – 20°C) / 3 km

= -6.67°C/km

Another way to calculate the lapse rate is to use the dew point temperature. The dew point is the temperature at which water vapor in the air condenses into liquid water. The dew point is a good indicator of atmospheric stability.

The lapse rate can be calculated using the dew point by:

Lapse Rate (°C/km) = (Dew Point Temperature – Surface Temperature) / Height Difference

For example if the dew point temperature is 10°C and the surface temperature is 20°C the lapse rate would be:

Lapse Rate (°C/km) = (10°C – 20°C) / 3 km

= -6.67°C/km

The rate of decrease of temperature with height is known as the lapse rate. The most commonly used unit is °C per kilometer (or 100 m). The lapse rate is an important factor in atmospheric stability and weather forecasting.

Lapse rates can either be moist or dry. A moist lapse rate occurs when the air is saturated with water vapor and the temperature decreases with height. This happens when the dew point is equal to or greater than the surface temperature. A dry lapse rate occurs when the air is not saturated with water vapor and the temperature decreases with height. This happens when the dew point is less than the surface temperature.

The lapse rate can also be expressed in terms of pressure. This is known as the pressure lapse rate and is given by:

Pressure Lapse Rate (hPa/km) = (Pressure at Higher Altitude – Pressure at Lower Altitude) / Height Difference

For example if the pressure at the surface is 1000 hPa and the pressure at 3 km above the surface is 950 hPa the pressure lapse rate would be:

Pressure Lapse Rate (hPa/km) = (1000 hPa – 950 hPa) / 3 km

= 50 hPa/km

The pressure lapse rate is generally used by meteorologists to calculate the altitude at which a given pressure will occur.

The lapse rate is a very important concept in meteorology and is used in a variety of weather forecasts and analyses.

## What is the definition for lapse rate?

Answer: The rate of decrease of temperature with height.

## What is the formula for calculating lapse rate?

Answer: The formula for calculating lapse rate is the difference in temperature divided by the difference in height.

## What are the units for measuring lapse rate?

Answer: The units for measuring lapse rate are degrees Celsius per meter.

## What is a dry adiabatic lapse rate?

Answer: A dry adiabatic lapse rate is the rate of decrease of temperature with height in the atmosphere in the absence of condensation.

## What is a wet adiabatic lapse rate?

Answer: A wet adiabatic lapse rate is the rate of decrease of temperature with height in the atmosphere in the presence of condensation.

## What is the formula for calculating dry adiabatic lapse rate?

Answer: The formula for calculating dry adiabatic lapse rate is the difference in temperature divided by the difference in height.

## What is the formula for calculating wet adiabatic lapse rate?

Answer: The formula for calculating wet adiabatic lapse rate is the difference in temperature divided by the difference in height.

## What is the dry adiabatic lapse rate in the troposphere?

Answer: The dry adiabatic lapse rate in the troposphere is 9.

8 degrees Celsius per kilometer.

## What is the wet adiabatic lapse rate in the troposphere?

Answer: The wet adiabatic lapse rate in the troposphere is 6 degrees Celsius per kilometer.

## What is the dry adiabatic lapse rate in the stratosphere?

Answer: The dry adiabatic lapse rate in the stratosphere is 2 degrees Celsius per kilometer.

## What is the wet adiabatic lapse rate in the stratosphere?

Answer: The wet adiabatic lapse rate in the stratosphere is 0.

5 degrees Celsius per kilometer.

## What factors affect lapse rate?

Answer: Factors that affect lapse rate include humidity pressure and temperature.

## How does humidity affect lapse rate?

Answer: Humidity affects lapse rate because it affects the rate of condensation.

## How does pressure affect lapse rate?

Answer: Pressure affects lapse rate because it affects the rate of decrease of temperature with height.

## How does temperature affect lapse rate?

Answer: Temperature affects lapse rate because it affects the rate of decrease of temperature with height.