10 p of 3.6 degrees F per 1000 ft. QUESTION 7 The temperature of the atmosphere at different altitudes can be described using the O environmental lapse rate b.saturated adiabatic lapse rate dry adiabatic lapse rate diting condensation level
The lapse rate is the rate at which the atmospheric variable like the temperature in the earth's surface and these changes with altitude. It corresponds to the vertical pressure gradients.
These temperature profiles are an interaction of radiation convection of sunlight's ground heats the surface from below. As however, the air is hot it expands it then has low densities.
Thus the temperature found at various altitudes is a direct result of the normal lapse rate of the earth that is 6.5 degrees C per kilometer, hence the attitude increases the temperature decreases in relation to the air molecules the inversion of temperature generally occurs in the troposphere.
