The short answer, is that it's complicated.
The humidity you see on the weather is what's called Relative Humidity, which means that it's already correlated with temperature. As the temperature rises, so does the maximum amount of water the air can hold before it starts precipitating back out. So 20% humidity at 60F will have a smaller volume of water in the air than 20% at 80F.
If you've reached a certain volume of water in the air, and the temperature falls, you can reach the dew point, which is when the air can't hold the same amount of water and deposits it as dew. This is typically when people water, as the air simply cannot absorb moisture until the temperature rises again and the dew starts to evaporate.
Air movement can exchange saturated air with dry air, or vice versa, so it varies as to how much it affects evaporation.
Soil temperature also plays a role, as warm soil will evaporate more than cool soil. This is part of what can make agrivoltaics so dang handy, the solar panel shade will keep soil temps down and increase water retention.