1.
As more moisture is added to this air, the rate at which water will evaporate will probably decrease
Explanation:
As long as the air above the lake remains at a constant temperature, the relative humidity of the air will rise with increased evaporation of the water from the lake.
This will continue to increase until the relative humidity reaches approximately 50% and then the evaporation decreases until the saturation point of the air mass is reached where evaporation virtually stops because the air cannot take up more moisture. At saturation point, the rate at which the air mass loses moisture back to the lake (as dew) becomes equal to the rate at which the lake loses water to the air.
Learn More:
For more on relative humidity check out;
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