Because it is dependant on the temperature of the surrounding air.
There are two types of adiabatic lapse rates...wet and dry. (wet is also referred to as saturated or moist) To the extent that the cloudiness your question refers to represents saturated air, then no, the wet adiabatic lapse rate would be lower (approximately 1.5C/1000') than the dry adiabatic lapse rate (approximately 3C/1000').
the wet adiabatic rate of cooling involves condensation of water vapor, releasing latent heat which partially offsets the cooling from expansion. This latent heat addition makes the wet rate slower than the dry rate, where no condensation occurs.
If the wet adiabatic lapse rate is 6 degrees per kilometer, the temperature decreases by 6 degrees for every kilometer gained in altitude. To find the temperature at the top of the mountain, you need to know the initial temperature at the base of the mountain and the altitude gained to the top of the mountain. Start with the base temperature and subtract 6 degrees for every kilometer of altitude gained.
The rate of chemical weathering is generally higher in hot wet climates compared to cold dry climates. This is because higher temperatures and moisture levels accelerate chemical reactions that break down rocks and minerals. In contrast, cold and dry conditions slow down these reactions, leading to slower rates of chemical weathering.
Limestone would likely have the fastest rate of weathering in a warm wet climate. This is because limestone is more soluble in water compared to other rocks like granite or basalt, leading to quicker dissolution and weathering when exposed to moisture in a warm climate.
The rate at which adiabatic cooling occurs with increasing altitude for wet air (air containing clouds or other visible forms of moisture) is called the wet adiabatic lapse rate, the moist adiabatic lapse rate, or the saturated adiabatic lapse rate.
There are two types of adiabatic lapse rates...wet and dry. (wet is also referred to as saturated or moist) To the extent that the cloudiness your question refers to represents saturated air, then no, the wet adiabatic lapse rate would be lower (approximately 1.5C/1000') than the dry adiabatic lapse rate (approximately 3C/1000').
of the release of latent heat
the wet adiabatic rate of cooling involves condensation of water vapor, releasing latent heat which partially offsets the cooling from expansion. This latent heat addition makes the wet rate slower than the dry rate, where no condensation occurs.
of the release of latent heat
less than the wet adiabatic rate.
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 temperature of an air parcel increases during the wet adiabatic lapse rate because as the parcel rises and expands, it cools down. If the air is saturated with water vapor, latent heat is released as the water vapor condenses into water droplets. This latent heat warms the air parcel, causing the temperature to increase instead of decrease as it would in the dry adiabatic lapse rate.
Wet bulb temperature
If the wet adiabatic lapse rate is 6 degrees per kilometer, the temperature decreases by 6 degrees for every kilometer gained in altitude. To find the temperature at the top of the mountain, you need to know the initial temperature at the base of the mountain and the altitude gained to the top of the mountain. Start with the base temperature and subtract 6 degrees for every kilometer of altitude gained.
For airplane rentals, no. Since the wet rate includes fuel.
The forenvironments are dry, moist ,wet ,very wet.