For airplane rentals, no. Since the wet rate includes fuel.
The saturated adiabatic lapse rate is lower than the dry adiabatic lapse rate because during the process of condensation, heat is released into the atmosphere, which partially offsets the cooling effect of rising air. This release of heat makes the cooling rate of saturated air less than that of dry air as it ascends through the atmosphere.
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').
No, the wet bulb is always lower. Evaporation from the wet bulb reduces its temperature.
No, the wet bulb is always lower. Evaporation from the wet bulb reduces its temperature.
No, the wet bulb is always lower. Evaporation from the wet bulb reduces its temperature.
No. The temperature of dry ice is far lower than that of ice water.
They dry at the same rate of speed.
The evaporation rate of a desert is much greater than the precipitation rate.
of the release of latent heat
Bulb temperature is typically lower than dry temperature because the bulb thermometer measures the temperature of the air without factoring in the effects of evaporation. The dry bulb temperature, on the other hand, accounts for the cooling effect of evaporation, giving a lower reading than the bulb temperature.
The wet adiabatic rate is lower than the dry adiabatic rate because, during the condensation of water vapor into liquid, latent heat is released. This release of heat warms the rising air parcel, which reduces the rate at which it cools as it ascends. In contrast, the dry adiabatic rate applies to unsaturated air, which cools more rapidly because there is no heat released from condensation. Thus, the presence of moisture and the associated latent heat release slow the cooling process in saturated air.
of the release of latent heat