The temperature at which condensation and evaporation are equal. The temperature at which dew will always form. The temperature to which air must be cooled to become saturated.

cool, dense air moving inland from over the water. warm, dense air moving inland from over the water. water absorbing and radiating heat faster than the land.

Cumulonimbus. Nimbostratus. Towering Cumulus.

heat exchange. movement of air. pressure differential.

59°C and 1013.2 millibars. 59°F and 29.92 millibars. 15°C and 29.92″ Hg.

High temperature, high relative humidity, and high density altitude. Low temperature, low relative humidity, and low density altitude. High temperature, low relative humidity, and low density altitude.

It increases performance. It has no effect on performance. It decreases performance.